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LCL RESOURCES LIMITED — Capital/Financing Update 2022
Nov 24, 2022
65217_rns_2022-11-24_2d4504a2-78dd-405e-bca3-923d54ad13a4.pdf
Capital/Financing Update
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25 November 2022 ASX Announcement ASX: LCL
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Company to acquire multiple copper, nickel and gold targets in PNG
HIGHLIGHTS
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The acquisition of private company, Footprint Resources Pty Ltd, includes multiple copper, gold and nickel targets in Papua New Guinea proximal to existing Tier-1 deposits
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The acquisition extends the Company’s exposure to nickel and copper (as well as gold), both critical metals in the EV battery sector
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Creates new exploration focusses for the Company, on top of the ongoing development of the Colombian Quinchia Project
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Footprint principals to join Los Cerros to drive PNG projects - ensures continuity of project and country knowledge
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Exploration programs commencing on two of the five Footprint projects with new geological models as targets
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Preparation for a 3,000m diamond drilling program at Kusi, where recent work has reinterpreted the economic potential for a gold-copper oxide skarn with historical drill intersections including 35m @ 3.04g/t Au from 136m in KSDD007 and trench sampling including 8m @ 11.5g/t Au, 2.6% Cu, 24g/t Ag
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Applying modern geophysical techniques in conjunction with field work to locate the source of massive nickel sulphide boulder float assaying up to 45.8% Ni at Veri Veri
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PNG exploration to focus on high grade discovery and aim to attract JV partners to advance multiple gold-copper porphyry targets in PNG and Colombia
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Colombian work continues on high-level investigations of potential production scenarios ahead of a Preliminary Economic Assessment of the 2.6Moz Quinchia Project
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The Company held over $11M cash at 30 September 2022
Los Cerros Limited (ASX: LCL) (Los Cerros or the Company) is pleased to advise it has acquired 100% of Papua New Guinea ( PNG ) focussed private exploration company Footprint Resources Pty Ltd ( Footprint ), exposing the Company to multiple high grade exploration targets within five large project areas prospective for copper-gold and nickel.
The acquisition provides high-impact, new discovery potential to Los Cerros’ shareholders, in a region that is proven to host a large number of major mineral deposits. Importantly, the acquisition of Footprint increases the Company’s exposure to nickel and copper, both critical metals for the electric vehicle market, in addition to its existing gold portfolio.
Details of the material terms of the acquisition are outlined below.
The Company also welcomes Footprint principals and only shareholders, geologists Glenn Twomey and John Dobe, as Los Cerros’ employees. They bring with them Footprint’s PNG exploration team, logistical support and in-country relationships. Inheriting continuity of project knowledge and incountry experience to ensure Los Cerros can hit the ground running and commence its exploration program immediately.
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Mr Twomey and Mr Dobe bring nearly 60 years of combined global ‘boots on the ground’ mineral exploration expertise including a combined sixteen years in PNG in senior roles (Exploration Manager PNG and Principal Geologist-Project Generation, respectively) for Barrick Gold, the world’s largest gold producer. In addition, Mr Twomey has held Board positions and performed material roles in resource expansions including at Porgera (in PNG). Mr Dobe brings world class experience in project generation with extensive expertise in porphyry, epithermal, IOCG, sediment hosted copper and orogenic gold systems. Mr Twomey and Mr Dobe formed Footprint eight years ago to leverage their combined experience and understanding of PNG geology.
The Footprint acquisition includes a total of 3,867km[2] of exploration titles in central and southern areas of PNG (Figure 1). The titles cover deep-seated, northeast trending, arc normal structures, widely regarded as key controls to large PNG copper-gold deposits such as the Wafi-Golpu deposit.
Following completion of the acquisition, Los Cerros will focus initially on a 3,000m diamond drilling program at the Kusi target within the Ono Project. Footprint have re-interpreted historical diamond drilling results at Kusi, including 35m @ 3.04g/t Au from 136m in KSDD007, as representing significant potential for a near surface, high grade gold-copper oxide skarn deposit.
At the Veri Veri prospect, within the Liamu licence, exploration will focus on the source of creek float boulders of massive nickel sulphides assaying up to 45.8% Ni with some samples also reporting high gold grades such as 23.37% Ni plus 10.6g/t Au.
Additional significant copper/gold targets occur across the Liamu, Imou and Tauya projects. The Company is eager to see advances across all targets concurrently and as such is open to JV farm-ins and strategic alliances that fast-track realisation of the potential of the Company’s PNG and Colombian multi-commodity portfolio and optimises the project generation capacity of the Footprint team.
The Company continues towards a PEA[1] on the Quinchia Project in Colombia which de-risks the project through building confidence in the current 2.6Moz[2] Resource and simultaneously dials down Colombian expenditure pending greater clarity on new government mine development policies.
Los Cerros Managing Director, Jason Stirbinskis added
“This transformational addition to the Los Cerros mineral portfolio offers immediate and material exploration upside as well as jurisdictional and metal diversity, in particular the addition of critical metals to the electric vehicle sector. It also ensures we play to our strengths as successful explorers while our Quinchia Project migrates to engineering/development studies.
I have walked the ground over the key projects and the near term prospectivity of our new PNG portfolio is compelling. We are particularly excited to welcome Glenn and John to the Company as they bring extensive PNG geological experience, are aligned to our ESG priorities and equip Los Cerros with a unique strategic and technical advantage in both PNG and Colombia across various mineralisation styles.”
1 See announcement 29 August 2022 for further detail.
2 Contains a mix of Inferred, Indicated and Measured Resources. Using Tesorito MRE of 1.3Moz @ 0.81 g/t Au. The Miraflores Reserve is included in the Miraflores Resource. Refer ASX announcement dated 14 March 2017 (Miraflores Resource) and 27 November 2017 (Miraflores Reserve) and 25 February 2020 (Dosquebradas Resource) and 22 March 2022 (Tesorito Resource). The Company confirms that it is not aware of any new information or data that materially affects the information included in the market announcements, and that all material assumptions and technical parameters underpinning the estimates continue to apply.
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Figure 1 : The acquired licences are located within central and southern Papua New Guinea within mineralised belts. Most are proximal to arc normal structures (faults) which are often associated with regional scale mineralisation, as evidenced by established discoveries.
The Footprint Portfolio Acquired
1. Ono Project – Gold/Copper target
The Ono Project consists of 1,630km[2] of granted contiguous exploration licenses over an intrusive complex considered prospective for high grade oxide gold in skarns along with epithermal and porphyry style mineralisation. Ono is situated ~150km from the industrial port of Lae and within the same structural belt as the Hidden Valley gold mine and the Wafi-Golpu copper/gold project (Figure 2).
Kusi , is the most advanced target. Best drill results were recorded from the southern boundary of the area of interest where three diamond holes (Table 10) were drilled to test for a buried porphyry, predicted to exist based on surface data. The holes intersected an upper limestone skarn unit above the porphyry target and reported:
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KSDD003 10.1m @ 2.39g/t Au from 0m
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KSDD004 20m @ 2.89g/t Au from 107m
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KSDD007 35m @ 3.04g/t Au from 136m
Historical trenching of a lower limestone skarn unit, some 500m below the upper limestone skarn, assayed:
- 28m @ 0.90g/t Au, 21.6g/t Ag, 1.9% Pb and 1.9% Zn
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In 2021-2022 Footprint consolidated tenement ownership and concluded that high grade historical drill intersections in KSDD003, ‘04 & ‘07 represent oxide skarn mineralisation in a sub-horizontal upper limestone unit cut by thin diorite dykes related to an underlying copper-gold porphyry hydrothermal system. None of the historical drill holes have tested a known lower limestone skarn unit or, in the opinion of both Footprint and Los Cerros, have adequately tested the buried copper-gold porphyry theory.
As an initial test of this new model, Footprint trenched the projected outcrop of the upper limestone unit intersected in KSDD004 and KSDD007 recording 20m @ 3.84g/t Au (Table 1) and establishing continuity of the high-grade oxide skarn mineralisation from hillside outcrop to intercepts in KSDD004 and to KSDD007 over a distance of nearly 300m into the mountain.
To further test the copper-gold skarn concept, Footprint prospected, sampled and trenched the steeply dissected and poorly exposed eastern portion of the gold in soil anomaly which led to the 2022 discovery of Leah’s Lode (Figure 3), 1km east of the KSDD004 drill pad, where sampling of skarn (Table 2) in trench FPTR4 (Photos 1a, b & c) assayed:
- 8m @ 11.5g/t Au, 2.6% Cu, 24g/t Ag including visible gold, primary chalcopyrite and secondary copper minerals
The gold-copper mineralisation within the upper limestone unit is believed to be derived from a buried causative porphyry (Figure 3). This is a well understood model, with high grade skarn gold/polymetallic deposits mined at Grasberg/Ertsberg in Irian Jaya and Ok Tedi in PNG.
The upper limestone is modelled to occur over a total area of approximately 3km x 1.5km (Figure 3). A proposed 3,000m diamond drilling program will initially focus in the areas with historical drilling and trenching, targeting a high-grade oxide resource, whilst prospecting will continue to define the exposed upper limestone perimeter which has potential to be a laterally extensive gold-copper mineralised unit.
Previous explorers discovered gold mineralisation at Garawaria and Dui Creek, 3km south of Kusi and at Kau Creek 10km south of Kusi (Figure 2). These prospects are yet to be field checked by Footprint or Los Cerros. Beyond these areas, there has been limited exploration within the remainder of the 32km x 10km Ono intrusive complex.
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Figure 2: The Ono Project sits with the same belt as the multi-million-ounce Wafi-Golpu and Hidden Valley projects. The established exploration targets at Ono conform to a regional arc normal NE trend as evidenced in regional magnetics, there is considered to be significant potential for further success along this trend within the Ono licences.
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Figure 3: Plan view of Kusi showing gold in soils geochemical anomaly, 3D magnetic inversion shell and historical drill collars over modelled upper limestone skarn and interpreted intrusive (porphyry) centre. See Figure 4 for cross section A-A’.
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Figure 4: Kusi stylised cross section showing assay results over modelled relationship between mapped skarns and potential central porphyry. Note 71m trench (KSTC45A) intercept is interpreted to be along strike and thus not representative of true thickness.
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Photos 1a, b & c . Photo 1a: Leah’s Lode is a 2022 discovery. Trenching (FPRTR4) has delivered 8m @ 11.5g/t Au, 2.6% Cu, 24g/t Ag. Photo 1b: Clearly visible copper oxides exposed within the trench. Photo 1c: High grade chalcopyrite-garnetmagnetite polished rock sample from Leah’s Lode outcrop, 2m from trench - 61.3g/t Au, 18% Cu, 135g/t Ag (Table 3).
2. Veri Veri Prospect - Nickel
The Veri Veri prospect (Figures 1 & 5), located ~100km ESE of Port Moresby and 50km NE of Kupiano port, covers mafic and ultramafic complexes within the Papuan Ultramafic Belt and is considered prospective for high grade nickel sulphide mineralisation (Photo 2). The prospect occurs within the Company’s larger Liamu Project (Figure 5).
Early regional surveys by A.O.G. Minerals’ (1971) geologists located massive nickel sulphide boulders in Veri Veri Creek. This discovery prompted historical exploration programs, initially tracing boulders upstream. Follow-up trenching exposed an east-west trending nickel sulphide vein up to 0.3m thick. However, additional massive nickel sulphide float was subsequently discovered further upstream from the trench. Float samples from within or near the Veri Veri Creek include (Table 6):
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15.66% Ni and 9.1g/t Au
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45.8% Ni (no Au value)
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23.37% Ni and 10.6g/t Au
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32.7% Ni and 3.2g/t Au
Where exposed, primary mineralisation is hosted in narrow shear zones, normally 2-4m wide, comprising massive, vein and veinlet nickel sulphide minerals millerite, heazlewoodite and pentlandite plus fracture coated nickel silicate mineral garnierite.
The high sulphide content indicates the potential for modern geophysical surveys as a cost effective exploration tool to locate any substantial zones of massive sulphides in this poorly exposed and steeply dissected topography. There has been no drilling for nickel sulphides within the Veri Veri Project area.
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Photo 2: Veri Veri creek float samples include massive nickel sulphide minerals (heazlewoodite, millerite, pentlandite) and nickel-bearing silicates including serpentinite and garnierite. Photo Right: boulder with nickel sulphides in creek. Samples taken by Footprint, see Table 4 and JORC tables in this announcement.
3. Liamu Project – copper/gold epithermals and porphyries
Multiple untested copper-gold epithermal and porphyry targets
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Ubei a 4km x 4km surface geochemical anomaly defined by rock chip samples with individual samples frequently grading >2% Cu and 2g/t Au (Table 8). An undrilled central EM geophysical anomaly is thought to be mapping a porphyry intrusive centre at depth. Peripheral epithermal Cu/Au vein corridors include Puma with undrilled underlying IP geophysical anomaly.
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Dada Trenching has revealed intense 40 veins/m porphyry quartz veining assaying 96m @ 0.41g/t Au (Table 7) open in all directions. Not drilled.
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Figure 5 : Location of Liamu and Veri Veri Projects over gold rock chip geochemistry.
4. Imou Project – skarn and epithermal and porphyry copper/gold potential in world class district
The Imou Project is within a world class district hosting the multi-million-ounce Ok Tedi, Porgera and Frieda River projects (Figures 1 & 6). Targets:
- Imou Porphyry Target Limited historical drilling has identified a large, shallow, low-grade CuAu porphyry with an associated higher-grade Cu-Au breccia zone. Mineralisation remains open in all directions including the possibility of higher-grade porphyry pulses/events. Best intersection:
o IM19DD001, 305m @ 0.37% Cu, 0.37g/t Au from 5m, including 14m at 2.43% Cu, 2.78g/t Au from 186m
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Michael’s Creek, an epithermal target with surface rock chip samples including 58.5g/t Au in quartz veining
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High Creek , a Cu-Au skarn
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Bikaru , an epithermal gold target
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Figure 6 : The Imou Project is prospective for Cu/Au and is near globally significant projects..
5. Tauya Project – Copper. Along strike from Yandera Cu-Mo porphyry
The Tauya Project is within the Bismark Intrusive Complex, 6km along strike from the giant Yandera Cu-Mo porphyry (Figure 7), one of the largest undeveloped projects in the SW Pacific. Tauya is an early-stage target which has been recently granted. Historical surface exploration has been undertaken by numerous companies, including CRA, Kennecott, Highlands Gold and Marengo Mining. Footprint is currently compiling the historical data.
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Target 1. Numerous copper geochemical anomalies in streams, rock chips and soils within an interpreted alteration corridor that extends from Yandera to the southeast
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Target 2. High grade gold in quartz/sulphide vein float samples over 500m strike coincidental with artisanal mining.
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25 November 2022 ASX Announcement ASX: LCL
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Figure 7: The Tauya Project area includes a porphyry target along strike from the Yandera Porphyry .
Why PNG
PNG is ‘elephant country’, historically the domain of major mining companies focussing on the exploration for Tier-1 gold-copper porphyry deposits. Junior explorers have recently been attracted by high grade gold-copper epithermal potential overlooked by the majors. One such example is K92 Mining Inc (TSX:KNT) who acquired the Kainantu gold-copper deposit (located between Los Cerros’ Ono and Tauya Projects – Figure 1) from Barrick in 2014.
Los Cerros believes it has potential for near term success at the Kusi Project, where Footprint have developed a new oxide skarn gold-copper geological model in multiple, near surface limestone units. Previous Kusi explorers focussed exclusively on porphyry style mineralisation. Additional high grade
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vein ‘K92 targets’ within the Ono Project and other Footprint projects will be Los Cerros’s gold-copper exploration priority in conjunction with exploration for high grade nickel sulphides.
Footprint principals’ combined 16 years of cost effective PNG exploration management experience has previously attracted a significant PNG joint venture agreement with a major international miner. These skill sets will be an advantage to Los Cerros in attracting joint venture partners particularly in the search for copper-gold porphyries over the Company’s extensive holdings in PNG and Colombia.
Footprint transaction details
Los Cerros has acquired 100% of Footprint’s shares through the payment of $350,000 cash and the issue of 65,064,886 fully paid ordinary shares of Los Cerros, representing 10% of the Company’s current issued capital. 80% of the new shares have been escrowed for 12 months (until 22 November 2023).
Messrs Twomey and Dobe have joined the Company as executives. Both have Executive Service Agreements which contemplate full time employment with Los Cerros inclusive of non-competition clauses; obligations concerning discoveries and new information; and performance-based bonuses/incentives issued under the Company’s Performance Rights and Options Plan linked to meeting targets associated with Company’s new PNG assets.
The Footprint purchase includes all assets, net working capital, granted titles, title applications and employees of Footprint and incorporates the usual caveats and warranties for a transaction of this nature.
For the purpose of ASX Listing Rule 15.5, the Board has authorised this announcement to be released.
For further enquiries contact:
Jason Stirbinskis
Managing Director - Los Cerros Limited 3/35 Outram Street WEST PERTH WA 6005 [email protected]
FORWARD LOOKING STATEMENTS This document contains forward looking statements concerning Los Cerros. Forward-looking statements are not statements of historical fact and actual events and results may differ materially from those described in the forward-looking statements as a result of a variety of risks, uncertainties and other factors. Forward-looking statements are inherently subject to business, economic, competitive, political and social uncertainties and contingencies. Many factors could cause the Company’s actual results to differ materially from those expressed or implied in any forward-looking information provided by the Company, or on behalf of the Company. Such factors include, among other things, risks relating to additional funding requirements, metal prices, exploration, development and operating risks, competition, production risks, regulatory restrictions, including environmental regulation and liability and potential title disputes. Forward looking statements in this document are based on Los Cerros’ beliefs, opinions and estimates of Los Cerros as of the dates the forward-looking statements are made, and no obligation is assumed to update forward looking statements if these beliefs, opinions and estimates should change or to reflect other future developments. Although management believes that the assumptions made by the Company and the expectations represented by such information are reasonable, there can be no assurance that the forward-looking information will prove to be accurate. Forward-looking information involves known and unknown risks, uncertainties, and other factors which may cause the actual results, performance or achievements of the Company to be materially different from any anticipated future results, performance or achievements expressed or implied by such forward-looking information. Such factors include, among others, the actual market price of gold, the actual results of future exploration, changes in project parameters as plans continue to be evaluated, as well as those factors disclosed in the Company's publicly filed documents. Readers should not place undue reliance on forward-looking information. The Company does not undertake to update any forward-looking information, except in accordance with applicable securities laws. No representation, warranty or undertaking, express or implied, is given or made by the Company that the occurrence of the events expressed or implied in any forward-looking statements in this presentation will actually occur.
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JORC STATEMENTS - COMPETENT PERSONS STATEMENTS
The technical information related to Los Cerros assets contained in this report that relates to Exploration Results (excluding those pertaining to Mineral Resources and Reserves) is based on information compiled by Mr Cesar Garcia, who is a Member of the Australasian Institute of Mining and Metallurgy and who is a Geologist employed by Los Cerros on a full-time basis. Mr Garcia has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration, and to the activity which he is undertaking, to qualify as a Competent Person as defined in the 2012 Edition of the ‘Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves’. Mr Garcia consents to the inclusion in the release of the matters based on the information he has compiled in the form and context in which it appears.
The information presented here that relates to Mineral Resources of the Tesorito Project, Quinchia District, Republic of Colombia is based on and fairly represents information and supporting documentation compiled by Mr. Michael Andrew of Snowden Optiro. Mr Andrew takes overall responsibility for the Resource Estimate. Mr. Andrew is a Fellow of the Australasian Institute of Mining and Metallurgy (AusIMM). Mr Andrew is not an employee or related party of the Company. Mr. Andrew has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration and to the activity he is undertaking to qualify as Competent Persons as defined in the 2012 Edition of the ‘Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (JORC Code 2012)’. Mr. Andrew consents to the inclusion in the news release of the information in the form and context in which it appears.
The information presented here that relates to Mineral Resources of the Dosquebradas Project, Quinchia District, Republic of Colombia is based on and fairly represents information and supporting documentation compiled by Mr. Scott E. Wilson of Resource Development Associates Inc, of Highlands Ranch Colorado, USA. Mr Wilson takes overall responsibility for the Resource Estimate. Mr. Wilson is Member of the American Institute of Professional Geologists, a “Recognised Professional Organisation” as defined by the Australasian Institute of Mining and Metallurgy (AusIMM). Mr Wilson is not an employee or related party of the Company. Mr. Wilson has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration and to the activity he is undertaking to qualify as Competent Persons as defined in the 2012 Edition of the ‘Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (JORC Code 2012)’. Mr. Wilson consents to the inclusion in the news release of the information in the form and context in which it appears
Mineral Resources and Reserves Statement
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QUINCHIA PROJECT - MINERAL RESOURCE ESTIMATE (MRE)
Quinchia subzone Resource Category CUT-OFF TONNES (Mt) Au (g/t) Au (koz)
Tesorito Inferred 0.5g/t Au 50.0 0.81 1,298
Dosquebradas Inferred 0.5g/t Au 20.2 0.71 459
Miraflores - U.Ground Measured + Indicated 1.2g/t Au 9.3 2.82 840
Miraflores - U.Ground Inferred 1.2g/t Au 0.5 2.36 37
QUINCHIA RESOURCE 80.0 1.02 2,634
Note: Miraflores Resource includes Miraflores Reserve
MIRAFLORES RESERVE
CATEGORY TONNES (Mt) Au (g/t) Ag (g/t) Au (koz) Ag (koz)
Proved 1.70 2.75 2.20 150 120
Probable 2.62 3.64 3.13 307 264
Total 4.32 3.29 2.77 457 385
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The information in this section is drawn from the following ASX releases:
| Deposit | Release Date |
|---|---|
| Miraflores Mineral Resource Estimate and explanatorynotes | 14 March 2017 |
| Miraflores Ore Reserve Estimate and explanatorynotes | 17 November 2017 |
| Dosquebradas Mineral Resource Estimate and explanatorynotes | 25 February2020 |
| Tesorito Resource Mineral Resource Estimate and explanatorynotes | 22 March 2022 |
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| From (m) | To (m) | Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
|---|---|---|---|---|---|
| 0 | 2 | 493524.3 | 9134241.5 | Oxidised skarn | 3 |
| 2 | 4 | 493523.6 | 9134239.6 | Oxidised skarn | 2.39 |
| 4 | 6 | 493522.9 | 9134237.7 | Oxidised skarn | 1.55 |
| 6 | 8 | 493522.2 | 9134235.8 | Oxidised skarn | 4.4 |
| 8 | 10 | 493521.5 | 9134234.0 | Oxidised skarn | 16 |
| 10 | 12 | 493520.8 | 9134232.1 | Oxidised skarn | 6.3 |
| 12 | 14 | 493520.2 | 9134230.2 | Oxidised skarn | 1.27 |
| 14 | 16 | 493519.8 | 9134228.2 | Oxidised skarn | 0.9 |
| 16 | 18 | 493519.5 | 9134226.3 | Oxidised skarn | 2.27 |
| 18 | 20 | 493519.1 | 9134224.3 | Oxidised skarn | 1.63 |
| 20 | 22 | 493518.8 | 9134222.3 | Oxidised skarn | 2.56 |
Table 1 : Material Intercepts of Kusi trench 1 sampling by Footprint.
| From (m) | To (m) | Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) | Cu ppm | Ag g/t | Mo **ppm ** |
Zn **ppm ** |
|---|---|---|---|---|---|---|---|---|---|
| 0 | 1 | 494319.1 | 9134920 | Phyllite | 2.697 | 6792 | 3.4 | 48.9 | 2739 |
| 1 | 2 | 494319.1 | 9134921 | Phyllite | 1.027 | 1525 | 3.2 | 9.7 | 1233 |
| 2 | 3 | 494319.1 | 9134922 | Skarn | 8.196 | 15809 | 17.7 | 68 | 5283 |
| 3 | 4 | 494319.2 | 9134923 | Skarn | 3.142 | 17909 | 9.9 | 542 | 4957 |
| 4 | 5 | 494319.2 | 9134924 | Skarn | 27.74 | 36073 | 55.9 | 492 | 1286 |
| 5 | 6 | 494319.2 | 9134925 | Skarn | 43.298 | 121586 | 93.7 | 45.2 | 1525 |
| 6 | 7 | 494319.3 | 9134926 | Phyllite | 4.702 | 7702 | 7.5 | 47.7 | 207 |
| 7 | 8 | 494319.3 | 9134927 | Phyllite | 1.186 | 2410 | 2.4 | 26.8 | 215 |
Table 2 : Material Intercepts of Kusi trench (Leah’s Lode) FTPR4. Sampling by Footprint.
| Easting WGS84Z55S |
Northing WGS84Z55S |
Au (g/t) | Ag (g/t) | Pb (ppm) |
Zn (ppm) |
|---|---|---|---|---|---|
| 492655 | 9134037 | 0.25 | 3.00 | 290 | 21200 |
| 492656 | 9134037 | 0.25 | 3.00 | 290 | 21200 |
| 492657 | 9134037 | 0.35 | 7.00 | 20500 | 1390 |
| 492658 | 9134037 | 0.35 | 7.00 | 20500 | 1390 |
| 492659 | 9134037 | 0.18 | 13.00 | 12600 | 6200 |
| 492660 | 9134037 | 0.18 | 13.00 | 12600 | 6200 |
| 492661 | 9134037 | 0.40 | 3.00 | 820 | 5000 |
| 492662 | 9134037 | 0.40 | 3.00 | 820 | 5000 |
| 492663 | 9134037 | 1.19 | 9.00 | 6420 | 7800 |
| 492664 | 9134037 | 1.19 | 9.00 | 6420 | 7800 |
| 492665 | 9134037 | 0.43 | 43.00 | 23500 | 17300 |
| 492666 | 9134037 | 0.43 | 43.00 | 23500 | 17300 |
| 492667 | 9134037 | 2.01 | 7.00 | 2320 | 9900 |
| 492668 | 9134037 | 2.01 | 7.00 | 2320 | 9900 |
| 492669 | 9134037 | 1.56 | 14.00 | 11000 | 17300 |
| 492670 | 9134037 | 1.56 | 14.00 | 11000 | 17300 |
| 492671 | 9134037 | 0.54 | 28.00 | 29500 | 41000 |
| 492672 | 9134037 | 0.54 | 28.00 | 29500 | 41000 |
| 492673 | 9134037 | 0.79 | 36.00 | 34000 | 35800 |
| 492674 | 9134037 | 0.79 | 36.00 | 34000 | 35800 |
| 492675 | 9134037 | 1.95 | 36.00 | 20400 | 28800 |
| 492676 | 9134037 | 1.95 | 36.00 | 20400 | 28800 |
| 492677 | 9134037 | 2.01 | 45.00 | 24300 | 61000 |
| 492678 | 9134037 | 2.01 | 45.00 | 24300 | 61000 |
| 492679 | 9134037 | 0.60 | 39.00 | 48500 | 11000 |
| 492680 | 9134037 | 0.60 | 39.00 | 48500 | 11000 |
| 492681 | 9134037 | 0.51 | 16.00 | 16500 | 6900 |
| 492682 | 9134037 | 0.51 | 16.00 | 16500 | 6900 |
Table 3 : Material Intercepts of Kusi lower limestone trench. Sampling by CRA (Rio Tinto)
| Easting WGS84Z55S |
Northing WGS84Z55S |
Au (g/t) | Ag (g/t) | Pb (ppm) |
Zn (ppm) |
|---|---|---|---|---|---|
| 493995 | 9134401 | 0.17 | 0.20 | 144 | 29 |
| 493996.5 | 9134404 | 0.10 | 0.10 | 262 | 18 |
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25 November 2022 ASX Announcement ASX: LCL
==> picture [102 x 68] intentionally omitted <==
| 493998.4 | 9134404 | 0.13 | 0.20 | 177 | 19 |
|---|---|---|---|---|---|
| 493999.3 | 9134404 | 0.11 | 0.10 | 164 | 52 |
| 494000.3 | 9134404 | 0.08 | NA | 299 | 117 |
| 494001.2 | 9134404 | 0.05 | 0.20 | 221 | 34 |
| 494001.7 | 9134405 | 0.08 | 0.20 | 253 | 30 |
| 494002.2 | 9134406 | 0.46 | 0.70 | 877 | 355 |
| 494002.6 | 9134407 | 4.94 | 8.30 | 8800 | 3780 |
| 494003.1 | 9134408 | 1.65 | 2.10 | 398 | 470 |
| 494003.6 | 9134408 | 0.69 | 4.00 | 1400 | 679 |
| 494004.1 | 9134409 | 4.87 | 3.00 | 4940 | 976 |
| 494005.1 | 9134409 | 4.36 | 5.00 | 4180 | 1280 |
| 494006 | 9134409 | 2.36 | 2.70 | 3490 | 371 |
| 494007 | 9134409 | 15.40 | 9.30 | 3890 | 3030 |
| 494008 | 9134408 | 24.60 | 11.00 | 5500 | 6370 |
| 494008.9 | 9134408 | 0.83 | 1.00 | 667 | 1560 |
| 494009.9 | 9134408 | 4.53 | 3.30 | 364 | 616 |
| 494010.8 | 9134409 | 8.72 | 9.30 | 2160 | 1170 |
| 494011.7 | 9134409 | 21.80 | 6.50 | 2250 | 1660 |
| 494012.7 | 9134409 | 17.50 | 4.50 | 4190 | 11000 |
| 494013.6 | 9134410 | 3.88 | 7.40 | 3860 | 17200 |
| 494014.5 | 9134410 | 4.02 | 9.60 | 2320 | 2290 |
| 494015.5 | 9134411 | 2.93 | 3.10 | 2810 | 2540 |
| 494016.2 | 9134411 | 5.33 | 8.00 | 4160 | 5500 |
| 494017 | 9134412 | 8.95 | 9.50 | 3630 | 7950 |
| 494017.7 | 9134413 | 13.30 | 3.20 | 3040 | 12700 |
| 494018.5 | 9134413 | 6.75 | 3.10 | 2850 | 20600 |
| 494019.2 | 9134414 | 3.19 | 2.00 | 3100 | 5390 |
| 494020 | 9134415 | 1.15 | 1.70 | 1580 | 1350 |
| 494020.7 | 9134415 | 4.12 | 2.70 | 2780 | 4080 |
| 494021.5 | 9134416 | 8.76 | 6.20 | 7570 | 7500 |
| 494022.2 | 9134417 | 15.60 | 8.00 | 4460 | 14700 |
| 494023 | 9134417 | 32.90 | 14.80 | 16000 | 34700 |
| 494023.7 | 9134418 | 10.90 | 6.10 | 5180 | 30900 |
| 494024.5 | 9134418 | 0.60 | 2.20 | 1550 | 3600 |
| 494025.4 | 9134419 | 6.93 | 5.20 | 3510 | 5820 |
| 494026.3 | 9134419 | 4.80 | 11.80 | 10900 | 26400 |
| 494027.2 | 9134420 | 9.88 | 9.70 | 6710 | 20300 |
| 494028.1 | 9134420 | 5.52 | 11.90 | 22300 | 25300 |
| 494029 | 9134421 | 10.20 | 20.10 | 18000 | 14900 |
| 494029.7 | 9134421 | 1.32 | 7.70 | 3300 | 29800 |
| 494030.4 | 9134422 | 0.37 | 1.80 | 2140 | 28000 |
| 494031.2 | 9134423 | 0.38 | 1.60 | 1030 | 4480 |
| 494032.6 | 9134424 | 0.76 | 2.30 | 1570 | 5060 |
| 494034.8 | 9134425 | 0.43 | 1.30 | 605 | 4430 |
| 494037.1 | 9134426 | 0.73 | 1.30 | 2280 | 5740 |
| 494040 | 9134428 | 4.83 | 2.10 | 4190 | 19300 |
| 494042.1 | 9134430 | 5.09 | 2.70 | 6070 | 30400 |
| 494043.7 | 9134432 | 0.36 | 1.10 | 454 | 314 |
| 494044.2 | 9134433 | 3.79 | 2.80 | 3970 | 8470 |
| 494044.7 | 9134434 | 3.71 | 8.80 | 10300 | 28500 |
| 494045.2 | 9134434 | 0.30 | 1.80 | 3130 | 4990 |
| 494045.7 | 9134435 | 0.40 | 3.60 | 2130 | 3220 |
| 494045.9 | 9134436 | 1.99 | 8.30 | 3540 | 4480 |
| 494046.1 | 9134436 | 1.97 | 8.10 | 3070 | 7590 |
| 494046.2 | 9134437 | 5.42 | 17.20 | 1450 | 4820 |
| 494046.4 | 9134438 | 3.26 | 10.90 | 645 | 1550 |
| 494046.5 | 9134439 | 4.25 | 2.10 | 1730 | 2150 |
| 494046.7 | 9134440 | 1.53 | 2.40 | 2580 | 3750 |
| 494046.9 | 9134440 | 0.59 | 0.70 | 370 | 505 |
| 494047 | 9134441 | 0.51 | 0.70 | 1250 | 1000 |
| 494047.2 | 9134442 | 0.18 | 0.70 | 567 | 1760 |
| 494047.3 | 9134443 | 3.31 | 3.70 | 1450 | 458 |
| 494047.5 | 9134443 | 4.54 | 3.30 | 1500 | 390 |
Table 4 : Material Intercepts of Kusi Trench KSTC45A. Sampling by Pacific Niugini Limited (ASX:PNR)
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25 November 2022 ASX Announcement ASX: LCL
==> picture [102 x 68] intentionally omitted <==
| Sample_ID | Easting | Northing | Lithology | Au_g/t | Ag g/t | Cu % | Pb % | Zn % |
|---|---|---|---|---|---|---|---|---|
| 171408 | 492742 | 9133713 | Skarn | 3.35 | 170 | 0.15 | 6.3 | 13.9 |
| 207300 | 494319 | 9134925 | Skarn | 61.3 | 135 | 18 | 0.0007 | 0.19 |
| 171434 | 494016 | 9134422 | Skarn | 40.4 | 116 | 11.65 | 0.0019 | 0.1 |
| 633359 | 494899.1 | 9135128 | Skarn | 1.24 | 47.9 | 0.06 | 2.5 | 2.15 |
Table 5 : Material outcrop rock chip samples at Kusi.
| Sample ID | Easting WGS | Northing WGS | Ni % | Au g/t | Mo ppm | Co ppm |
|---|---|---|---|---|---|---|
| FT5780 | 680804 | 8912033 | 15.59 | 6.6 | 20.6 | 785 |
| FT5781 | 681311 | 8912228 | 11.76 | 1.4 | 386 | 597 |
| FT5783 | 681482 | 8912399 | 4.63 | 1.4 | 457 | 317 |
| FT5784 | 681545 | 8912434 | 10.98 | 3.0 | 124 | 1139 |
| FT5785 | 681649 | 8912476 | 19.26 | 0.8 | 9.4 | 1127 |
| FT5786 | 681702 | 8912460 | 15.66 | 9.1 | 940 | 1112 |
| FT5787 | 682059 | 8913363 | 23.37 | 10.6 | 66.4 | 942 |
| FT57878 | 681311 | 8912228 | 6.79 | 0.6 | 96.3 | 765 |
| FT57879 | 682059 | 8913363 | 26.13 | 0.3 | 79.9 | 3931 |
| FT5780 | 680804 | 8912033 | 15.59 | 6.6 | 20.6 | 785 |
| 611751 | 687237 | 8912054 | 45.8 | NA | NA | NA |
| GMXR901 | 681939 | 8914116 | 32.7 | 3.2 | NA | NA |
Table 6 : Rock chip float samples. Veri Veri Project.
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25 November 2022 ASX Announcement
ASX: LCL
==> picture [103 x 68] intentionally omitted <==
Table 7 : Material trench samples of Dada trench (Liamu Project).
| From (m) |
To (m) |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
|---|---|---|---|---|---|
| 0 | 2 | 647005 | 8941244 | Feldspar Porphyry | 0.20 |
| 2 | 4 | 647006 | 8941242 | Feldspar Porphyry | 0.24 |
| 4 | 6 | 647008 | 8941241 | Feldspar Porphyry | 0.32 |
| 6 | 8 | 647009 | 8941239 | Feldspar Porphyry | 0.28 |
| 8 | 10 | 647010 | 8941238 | Feldspar Porphyry | 0.29 |
| 10 | 12 | 647012 | 8941237 | Feldspar Porphyry | 0.29 |
| 12 | 14 | 647013 | 8941236 | Feldspar Porphyry | 0.26 |
| 14 | 16 | 647015 | 8941235 | Feldspar Porphyry | 0.20 |
| 16 | 18 | 647016 | 8941233 | Feldspar Porphyry | 0.26 |
| 18 | 20 | 647018 | 8941232 | Feldspar Porphyry | 0.20 |
| 20 | 22 | 647019 | 8941231 | Feldspar Porphyry | 0.27 |
| 22 | 24 | 647020 | 8941229 | Feldspar Porphyry | 0.43 |
| 24 | 26 | 647021 | 8941228 | Feldspar Porphyry | 1.22 |
| 26 | 28 | 647022 | 8941226 | Feldspar Porphyry | 0.59 |
| 28 | 30 | 647023 | 8941225 | Feldspar Porphyry | 0.41 |
| 30 | 32 | 647024 | 8941223 | Feldspar Porphyry | 0.48 |
| 32 | 34 | 647026 | 8941222 | Feldspar Porphyry | 0.42 |
| 34 | 36 | 647028 | 8941221 | Feldspar Porphyry | 0.38 |
| 36 | 38 | 647030 | 8941221 | Feldspar Porphyry | 0.45 |
| 38 | 40 | 647032 | 8941221 | Feldspar Porphyry | 0.52 |
| 40 | 42 | 647034 | 8941221 | Feldspar Porphyry | 0.40 |
| 42 | 44 | 647036 | 8941221 | Feldspar Porphyry | 0.49 |
| 44 | 46 | 647038 | 8941221 | Feldspar Porphyry | 0.81 |
| 46 | 48 | 647039 | 8941221 | Feldspar Porphyry | 1.06 |
| 48 | 50 | 647041 | 8941221 | Feldspar Porphyry | 0.72 |
| 50 | 52 | 647043 | 8941221 | Feldspar Porphyry | 0.19 |
| 52 | 54 | 647044 | 8941221 | Feldspar Porphyry | 0.28 |
| 54 | 56 | 647045 | 8941221 | Feldspar Porphyry | 0.19 |
| 56 | 58 | 647044 | 8941218 | Feldspar Porphyry | 0.32 |
| 58 | 60 | 647046 | 8941217 | Feldspar Porphyry | 0.26 |
| 60 | 62 | 647047 | 8941216 | Feldspar Porphyry | 0.44 |
| 62 | 64 | 647049 | 8941215 | Feldspar Porphyry | 0.31 |
| 64 | 66 | 647051 | 8941215 | Feldspar Porphyry | 0.19 |
| From (m) |
To (m) |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|
| 66 | 68 | 647052 | 8941214 | Feldspar Porphyry | 0.32 | |
| 68 | 70 | 647054 | 8941213 | Feldspar Porphyry | 0.47 | |
| 70 | 72 | 647056 | 8941213 | Feldspar Porphyry | 0.28 | |
| 72 | 74 | 647058 | 8941212 | Feldspar Porphyry | 0.40 | |
| 74 | 76 | 647059 | 8941212 | Feldspar Porphyry | 0.87 | |
| 76 | 78 | 647061 | 8941211 | Feldspar Porphyry | 0.75 | |
| 78 | 80 | 647063 | 8941211 | Feldspar Porphyry | 0.43 | |
| 80 | 82 | 647065 | 8941211 | Feldspar Porphyry | 0.34 | |
| 82 | 84 | 647067 | 8941210 | Feldspar Porphyry | 0.67 | |
| 84 | 86 | 647069 | 8941210 | Feldspar Porphyry | 0.30 | |
| 86 | 88 | 647070 | 8941210 | Feldspar Porphyry | 0.48 | |
| 88 | 90 | 647072 | 8941209 | Diorite | 0.24 | |
| 90 | 92 | 647074 | 8941209 | Diorite | 0.16 | |
| 92 | 94 | 647076 | 8941208 | Diorite | 0.20 | |
| 94 | 96 | 647078 | 8941208 | Diorite | 0.25 |
Table 8: Ubei rock chip samples Liamu Project,-999 = not assayed
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
|---|---|---|---|---|---|
| FT5095 | 667336 | 8923650 | Basalt | 367.7 | 4899 |
| FT0065 | 667002 | 8921976 | Qtz-sulphide vein | 312.0 | 79504 |
| FT009007 | 666941 | 8921890 | Qtz-sulphide vein | 209.7 | 108949 |
| FT0047 | 667007 | 8922034 | Breccia | 156.0 | 94971 |
| FT5233 | 667009 | 8922008 | Andesite | 153.3 | 69042 |
| FT009006 | 667013 | 8921986 | Qtz-sulphide vein | 141.0 | 69975 |
| FT5229 | 667011 | 8922011 | Andesite | 133.9 | 95102 |
| FT5232 | 667009 | 8922009 | Andesite | 129.1 | 102764 |
| FT3009 | 667547 | 8921901 | Qtz-sulphide vein | 113.0 | 3648 |
| FT009004 | 667012 | 8921984 | Qtz-sulphide vein | 106.3 | 46712 |
| FT009057 | 667009 | 8921984 | Qtz-sulphide vein | 102.5 | 81990 |
| FT0061 | 666769 | 8921533 | not logged | 100.0 | 92680 |
| FT5230 | 667010 | 8922011 | Andesite | 89.5 | 46433 |
| FT5275 | 668030 | 8921949 | Basalt | 70.0 | 59878 |
| FT5280 | 666645 | 8924159 | Basalt | 66.6 | 210662 |
| FT009002 | 667010 | 8921984 | Qtz-sulphide vein | 47.2 | 5451 |
| FT3067 | 668991 | 8923288 | Qtz-sulphide vein | 42.5 | 16455 |
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25 November 2022 ASX Announcement
==> picture [103 x 68] intentionally omitted <==
ASX: LCL
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT009003 | 667011 | 8921984 | Qtz-sulphide vein | 32.8 | 7902 | FT00989 | 667416 | 8921999 | Qtz-sulphide vein | 7.0 | 2107 | ||
| FT5225 | 667014 | 8922014 | Andesite | 27.3 | 38935 | FT3070 | 668792 | 8923356 | Qtz-sulphide vein | 6.9 | 285 | ||
| FT5228 | 667012 | 8922012 | Andesite | 23.8 | 24233 | FT008547 | 666991 | 8921977 | Breccia | 6.9 | 83171 | ||
| FT5224 | 667015 | 8922015 | Andesite | 22.0 | 17580 | FT5292 | 667435 | 8921834 | Basalt | 6.7 | 8412 | ||
| FT5220 | 667014 | 8922013 | Andesite | 20.6 | 40296 | FT5290 | 667436 | 8921836 | Basalt | 6.6 | 11689 | ||
| FT5226 | 667014 | 8922013 | Andesite | 20.2 | 26151 | FT008552 | 667317 | 8921895 | Breccia | 6.4 | 16564 | ||
| FT008792 | 666958 | 8922000 | Qtz-sulphide vein | 20.1 | 18157 | FT5069 | 667489 | 8923809 | Andesite | 6.2 | 64 | ||
| FT5223 | 667016 | 8922015 | Andesite | 19.9 | 23889 | FT3008 | 667525 | 8921925 | Gossan | 6.1 | 6567 | ||
| FT008794 | 667035 | 8922123 | Qtz-sulphide vein | 19.3 | 39703 | FT5291 | 667435 | 8921835 | Basalt | 6.0 | 8791 | ||
| FT5303 | 667426 | 8921803 | Basalt | 18.3 | 6826 | FT008716 | 666925 | 8922061 | Andesite | 5.8 | 321 | ||
| FT008707 | 666893 | 8922200 | Qtz-sulphide vein | 16.7 | 2847 | FT3071 | 668787 | 8923347 | Andesite | 5.7 | 255 | ||
| FT00888 | 667011 | 8921989 | Qtz-sulphide vein | 16.0 | 15977 | FT008556 | 667884 | 8921938 | Qtz-sulphide vein | 5.6 | 107806 | ||
| FT3076 | 669002 | 8923319 | Andesite | 15.4 | 1678 | FT5814 | 667307 | 8923651 | Basalt | 5.4 | 857 | ||
| FT5512 | 668987 | 8923312 | not logged | 15.0 | 2291 | FT5352 | 667960 | 8922063 | not logged | 4.8 | 29110 | ||
| FT5222 | 667016 | 8922016 | Andesite | 15.0 | 14610 | FT5341 | 666922 | 8921967 | Andesite | 4.4 | 2096 | ||
| FT5218 | 666939 | 8921969 | Andesite | 14.8 | 11499 | FT5115 | 666957 | 8923622 | Gossan | 4.2 | 38020 | ||
| FT00809 | 667058 | 8922863 | Qtz-sulphide vein | 14.5 | 17634 | FT3060 | 667656 | 8922123 | Qtz-sulphide vein | 4.0 | 1052 | ||
| FT5097 | 667368 | 8923635 | Basalt | 14.4 | 27707 | FT00967 | 667427 | 8922012 | Qtz-sulphide vein | 3.8 | 32512 | ||
| FT008795 | 667035 | 8922123 | Qtz-sulphide vein | 14.2 | 14941 | FT5284 | 666917 | 8924501 | Basalt | 3.5 | 105011 | ||
| FT00801 | 666487 | 8922470 | Qtz-sulphide vein | 13.6 | 2309 | FT5094 | 667331 | 8923653 | Basalt | 3.4 | 7800 | ||
| FT5216 | 666963 | 8921954 | Gossan | 13.4 | 4829 | FT00819 | 667579 | 8923639 | Qtz-sulphide vein | 3.4 | 476 | ||
| FT5287 | 667437 | 8921839 | Basalt | 12.2 | 46414 | FT5107 | 667068 | 8923476 | Andesite | 3.4 | 9987 | ||
| FT5289 | 667436 | 8921837 | Basalt | 12.1 | 15683 | FT5192 | 666963 | 8921867 | Gossan | 3.4 | 612 | ||
| FT3005 | 667367 | 8921902 | Qtz-sulphide vein | 11.0 | 14006 | FT009031 | 667485 | 8921913 | Qtz-sulphide vein | 3.3 | 7595 | ||
| FT009056 | 667427 | 8922012 | Qtz-sulphide vein | 11.0 | 103609 | FT5175 | 666961 | 8921868 | Andesite | 3.2 | 368 | ||
| FT5815 | 667305 | 8923652 | Basalt | 9.2 | 2973 | FT008714 | 666864 | 8922196 | Qtz-sulphide vein | 3.1 | 1127 | ||
| FT008605 | 667882 | 8921953 | Qtz-sulphide vein | 9.1 | 110757 | FT3007 | 667481 | 8921883 | Qtz-sulphide vein | 3.1 | 210115 | ||
| FT5332 | 666972 | 8921993 | Andesite | 8.9 | 3858 | FT3063 | 669170 | 8923375 | Qtz-sulphide vein | 3.0 | 17803 | ||
| FT5277 | 666634 | 8924044 | Basalt | 8.8 | 30050 | FT5108 | 667049 | 8923472 | Gossan | 2.8 | 9255 | ||
| FT00897 | 666838 | 8922400 | Gossan | 8.5 | 1794 | FT3006 | 667433 | 8921839 | Qtz-sulphide vein | 2.8 | 4767 | ||
| FT5792 | 667331 | 8923652 | Basalt | 8.4 | 11245 | FT3002 | 667475 | 8922106 | Gossan | 2.7 | 9374 | ||
| FT5215 | 666962 | 8921954 | Gossan | 8.3 | 8077 | FT5172 | 667034 | 8922001 | Gossan | 2.7 | 149 | ||
| FT00845 | 666481 | 8922466 | Qtz-sulphide vein | 7.9 | 11966 | FT5795 | 667333 | 8923650 | Basalt | 2.5 | 2067 | ||
| FT5302 | 667424 | 8921803 | Basalt | 7.4 | 3145 | FT5190 | 666964 | 8921869 | Gossan | 2.4 | 1196 | ||
| FT5219 | 667011 | 8922011 | Andesite | 7.3 | 33647 | FT5191 | 666964 | 8921868 | Gossan | 2.2 | 363 |
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25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT5790 | 667327 | 8923653 | Basalt | 2.2 | 2476 | FT5552 | 667404 | 8924646 | IAG | 1.2 | 180 | ||
| FT5106 | 667283 | 8923278 | Basalt | 2.1 | 43371 | FT5331 | 666971 | 8921992 | Andesite | 1.2 | 853 | ||
| FT008559 | 667793 | 8922020 | Qtz-sulphide vein | 2.1 | 1273 | FT5308 | 667045 | 8922045 | Basalt | 1.2 | 490 | ||
| FT5167 | 667287 | 8923060 | Basalt | 2.0 | 426 | FT5237 | 667651 | 8923140 | Qtz-sulphide vein | 1.2 | 4997 | ||
| FT5212 | 666937 | 8921940 | Andesite | 1.9 | 510 | FT5187 | 667378 | 8922022 | Basalt | 1.1 | 156 | ||
| FT009058 | 667404 | 8921976 | Qtz-sulphide vein | 1.9 | 65005 | FT0057 | 667413 | 8921044 | not logged | 1.1 | 64115 | ||
| FT5102 | 667200 | 8923513 | Basalt | 1.8 | 8522 | FT0064 | 666924 | 8921898 | not logged | 1.1 | 1574 | ||
| FT00826 | 667172 | 8923390 | Qtz-sulphide vein | 1.8 | 1874 | FT5066 | 667488 | 8923807 | Andesite | 1.1 | 149 | ||
| FT008778 | 666972 | 8922013 | Qtz-sulphide vein | 1.8 | 233 | FT008785 | 666887 | 8923792 | Qtz-sulphide vein | 1.1 | 11190 | ||
| FT3064 | 669178 | 8923303 | Andesite | 1.8 | 549 | FT5188 | 667378 | 8922023 | Qtz-sulphide vein | 1.1 | 352 | ||
| FT5818 | 667373 | 8923635 | Basalt | 1.8 | 3553 | FT3073 | 668865 | 8923307 | Andesite | 1.1 | 139 | ||
| FT009030 | 667486 | 8921914 | Basalt | 1.8 | 3084 | FT00807 | 666654 | 8922525 | IAG | 1.1 | 6110 | ||
| FT5169 | 667212 | 8922957 | IAG | 1.7 | 6067 | FT00818 | 667024 | 8923520 | Qtz-sulphide vein | 1.1 | 1906 | ||
| FT00854 | 666483 | 8922474 | Basalt | 1.7 | 5408 | FT5236 | 667653 | 8923140 | Qtz-sulphide vein | 1.0 | 2687 | ||
| FT009014 | 667983 | 8921850 | Qtz-sulphide vein | 1.7 | 7867 | FT0053 | 667343 | 8921911 | not logged | 1.0 | 10707 | ||
| FT5801 | 667336 | 8923645 | Basalt | 1.7 | 1169 | FT00805 | 667256 | 8923429 | Qtz-sulphide vein | 1.0 | 9347 | ||
| FT3020 | 667836 | 8924177 | Basalt | 1.6 | 433 | FT5264 | 668058 | 8921950 | Basalt | 1.0 | 12780 | ||
| FT5118 | 666901 | 8923444 | Basalt | 1.6 | 34572 | FT5813 | 667365 | 8923681 | Basalt | 1.0 | 701 | ||
| FT5300 | 667434 | 8921825 | Basalt | 1.6 | 769 | FT00981 | 667414 | 8922008 | Qtz-sulphide vein | 1.0 | 4855 | ||
| FT5088 | 667777 | 8924036 | Basalt | 1.5 | 19 | FT3030 | 667033 | 8924560 | Basalt | 1.0 | 24 | ||
| FT5793 | 667332 | 8923651 | Basalt | 1.5 | 1349 | FT3053 | 667808 | 8924015 | Andesite | 1.0 | 19 | ||
| FT5235 | 667646 | 8923140 | Qtz-sulphide vein | 1.4 | 7080 | FT5820 | 667373 | 8923639 | Basalt | 1.0 | 63 | ||
| FT5796 | 667334 | 8923649 | Basalt | 1.4 | 3118 | FT5361 | 667555 | 8923840 | Basalt | 1.0 | 167 | ||
| FT3045 | 666901 | 8923832 | Breccia | 1.4 | 5931 | FT5539 | 668377 | 8923322 | Basalt | 1.0 | 15937 | ||
| FT5278 | 666691 | 8923992 | not logged | 1.3 | 3923 | FT00846 | 666481 | 8922467 | Qtz-sulphide vein | 1.0 | 1358 | ||
| FT008554 | 667395 | 8921910 | Qtz-sulphide vein | 1.3 | 3822 | FT3057 | 667682 | 8923972 | Qtz-sulphide vein | 1.0 | 56 | ||
| FT5211 | 666937 | 8921939 | Andesite | 1.3 | 623 | FT5103 | 667197 | 8923515 | Basalt | 1.0 | 943 | ||
| FT5092 | 667647 | 8923918 | Basalt | 1.3 | 103 | FT5096 | 667347 | 8923635 | Basalt | 1.0 | 42868 | ||
| FT00961 | 666935 | 8921904 | Qtz-sulphide vein | 1.3 | 496 | FT3024 | 667706 | 8924317 | Gossan | 0.9 | 144 | ||
| FT00962 | 666934 | 8921903 | Qtz-sulphide vein | 1.3 | 238 | FT00979 | 667416 | 8922009 | Qtz-sulphide vein | 0.9 | 8516 | ||
| FT3059 | 667662 | 8922115 | Gossan | 1.3 | 605 | FT5234 | 667647 | 8923140 | Qtz-sulphide vein | 0.9 | 57896 | ||
| FT008787 | 666954 | 8921882 | Qtz-sulphide vein | 1.2 | 738 | FT5296 | 667434 | 8921830 | Basalt | 0.9 | 263 | ||
| FT5501 | 668809 | 8923863 | Andesite | 1.2 | 2871 | FT5099 | 667290 | 8923483 | Basalt | 0.9 | 5723 | ||
| FT008549 | 666998 | 8922022 | Basalt | 1.2 | 780 | FT5282 | 666773 | 8924227 | Basalt | 0.9 | 1679 | ||
| FT5174 | 666965 | 8921878 | Andesite | 1.2 | 9579 | FT5380 | 667515 | 8923840 | IMD | 0.8 | 460 |
19
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT00825 | 666890 | 8923635 | IAG | 0.8 | 10061 | FT008782 | 667374 | 8924166 | Andesite | 0.6 | 1126 | ||
| FT009029 | 667486 | 8921915 | Basalt | 0.8 | 1166 | FT3025 | 667626 | 8924383 | Gossan | 0.6 | 9555 | ||
| FT5213 | 666937 | 8921941 | Andesite | 0.8 | 751 | FT5193 | 666963 | 8921866 | Gossan | 0.6 | 178 | ||
| FT00980 | 667415 | 8922009 | Qtz-sulphide vein | 0.8 | 9093 | FT5549 | 669887 | 8922781 | Basalt | 0.6 | 128478 | ||
| FT00820 | 667586 | 8923665 | Andesite | 0.8 | 209 | FT5375 | 667526 | 8923840 | IMD | 0.5 | 608 | ||
| FT5044 | 667472 | 8923794 | Andesite | 0.8 | 36 | FT008548 | 666958 | 8921882 | Qtz-sulphide vein | 0.5 | 931 | ||
| FT3015 | 668564 | 8922782 | Qtz-sulphide vein | 0.8 | 86268 | FT5168 | 667233 | 8922876 | Andesite | 0.5 | 2247 | ||
| FT5285 | 666984 | 8924556 | Basalt | 0.8 | 724 | FT5141 | 667028 | 8922123 | Basalt | 0.5 | 1426 | ||
| FT5500 | 668778 | 8923849 | not logged | 0.8 | 84 | FT5231 | 667010 | 8922010 | Andesite | 0.5 | 2665 | ||
| FT00824 | 667368 | 8923635 | Andesite | 0.8 | 3444 | FT5288 | 667436 | 8921838 | Basalt | 0.5 | 10129 | ||
| FT3062 | 669193 | 8923291 | Qtz-sulphide vein | 0.7 | 9974 | FT0063 | 666934 | 8921896 | not logged | 0.5 | 9024 | ||
| FT0048 | 666764 | 8920450 | BHO | 0.7 | 1355 | FT5061 | 667484 | 8923805 | Andesite | 0.5 | 11164 | ||
| FT3004 | 667429 | 8921919 | Qtz-sulphide vein | 0.7 | 3290 | FT008709 | 666894 | 8922196 | Andesite | 0.5 | 293 | ||
| FT009032 | 667485 | 8921913 | Basalt | 0.7 | 562 | FT3050 | 667648 | 8923965 | Andesite | 0.5 | 203 | ||
| FT00972 | 667423 | 8922010 | Gossan | 0.7 | 4477 | FT5078 | 667470 | 8923804 | Andesite | 0.5 | 56 | ||
| FT008799 | 666958 | 8921953 | Basalt | 0.7 | 99 | FT5531 | 667407 | 8924629 | Basalt | 0.5 | 14519 | ||
| FT00823 | 667588 | 8923695 | Andesite | 0.7 | 39 | FT5043 | 667472 | 8923792 | Andesite | 0.5 | 37 | ||
| FT008700 | 666901 | 8922083 | Andesite | 0.7 | 639 | FT008784 | 667418 | 8924189 | Andesite | 0.5 | 11 | ||
| FT008551 | 666755 | 8921463 | Basalt | 0.7 | 1906 | FT008800 | 666959 | 8921955 | Basalt | 0.5 | 344 | ||
| FT5090 | 667692 | 8923936 | Basalt | 0.7 | 90 | FT00811 | 667173 | 8923385 | Qtz-sulphide vein | 0.5 | 1427 | ||
| FT3074 | 668877 | 8923295 | Qtz-sulphide vein | 0.7 | 19858 | FT5799 | 667336 | 8923647 | Basalt | 0.5 | 10837 | ||
| FT5086 | 667674 | 8923977 | Basalt | 0.7 | 59 | FT009010 | 667985 | 8921851 | Basalt | 0.5 | 1180 | ||
| FT0067 | 648523 | 8945471 | PFH | 0.6 | 17008 | FT008788 | 666955 | 8921882 | Qtz-sulphide vein | 0.5 | 788 | ||
| FT5339 | 666981 | 8921995 | Andesite | 0.6 | 647 | FT00804 | 667224 | 8923485 | Gossan | 0.5 | 10475 | ||
| FT00969 | 667426 | 8922011 | Gossan | 0.6 | 3141 | FT5142 | 667027 | 8922122 | Basalt | 0.4 | 720 | ||
| FT0066 | 648524 | 8945472 | PFH | 0.6 | 12999 | FT008725 | 666920 | 8922071 | Qtz-sulphide vein | 0.4 | 1131 | ||
| FT008596 | 667799 | 8921978 | Andesite | 0.6 | 292 | FT008796 | 666979 | 8921941 | Qtz-sulphide vein | 0.4 | 7142 | ||
| FT009005 | 667012 | 8921985 | Qtz-sulphide vein | 0.6 | 1485 | FT5165 | 667000 | 8923215 | Basalt | 0.4 | 1988 | ||
| FT5511 | 669077 | 8923216 | not logged | 0.6 | 236 | FT5077 | 667472 | 8923804 | Andesite | 0.4 | 48 | ||
| FT008721 | 666923 | 8922069 | Andesite | 0.6 | 126 | FT5084 | 667459 | 8923710 | Gossan | 0.4 | 99 | ||
| FT5333 | 666973 | 8921993 | Andesite | 0.6 | 1781 | FT5238 | 667670 | 8923143 | Qtz-sulphide vein | 0.4 | 2126 | ||
| FT5079 | 667468 | 8923804 | Andesite | 0.6 | 88 | FT008779 | 666972 | 8922018 | Qtz-sulphide vein | 0.4 | 1167 | ||
| FT5364 | 667552 | 8923840 | Basalt | 0.6 | 501 | FT00984 | 667412 | 8922007 | Gossan | 0.4 | 4039 | ||
| FT3032 | 667072 | 8924601 | Breccia | 0.6 | 108681 | FT008733 | 666932 | 8922030 | BHO | 0.4 | 721 | ||
| FT5279 | 666691 | 8923992 | not logged | 0.6 | 256 | FT009009 | 667058 | 8922038 | Qtz-sulphide vein | 0.4 | 1151 |
20
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT5059 | 667482 | 8923804 | Andesite | 0.4 | 1684 | FT5513 | 669275 | 8922537 | VOO | 0.3 | 4114 | ||
| FT3069 | 668778 | 8923363 | Qtz-sulphide vein | 0.4 | 7947 | FT008699 | 666943 | 8921976 | Andesite | 0.3 | 1197 | ||
| FT008555 | 667917 | 8921973 | Qtz-sulphide vein | 0.4 | 96540 | FT5082 | 667473 | 8923790 | Basalt | 0.3 | 65 | ||
| FT00976 | 667419 | 8922010 | Gossan | 0.4 | 100074 | FT008726 | 666920 | 8922072 | Qtz-sulphide vein | 0.3 | 990 | ||
| FT5824 | 667306 | 8923648 | Basalt | 0.4 | 22 | FT3078 | 668914 | 8923470 | IAG | 0.3 | 592 | ||
| FT008598 | 667895 | 8921910 | Qtz-sulphide vein | 0.4 | 17934 | FT5502 | 668863 | 8923798 | not logged | 0.3 | 52 | ||
| FT008790 | 666971 | 8921932 | Qtz-sulphide vein | 0.4 | 556 | FT00817 | 667089 | 8923436 | Andesite | 0.3 | 773 | ||
| FT3033 | 667834 | 8924613 | Qtz-sulphide vein | 0.4 | 90772 | FT5798 | 667336 | 8923648 | Basalt | 0.3 | 453 | ||
| FT5797 | 667335 | 8923649 | Basalt | 0.4 | 2008 | FT3072 | 668790 | 8923347 | Andesite | 0.3 | 53 | ||
| FT3021 | 667809 | 8924189 | Basalt | 0.4 | 24 | FT3010 | 668021 | 8921934 | Gossan | 0.3 | 17422 | ||
| FT00983 | 667412 | 8922007 | Gossan | 0.4 | 3030 | FT5270 | 668029 | 8921950 | Basalt | 0.3 | 21048 | ||
| FT5330 | 666997 | 8922003 | Andesite | 0.3 | 1546 | FT5537 | 667044 | 8923688 | not logged | 0.3 | 1847 | ||
| FT008783 | 667374 | 8924166 | Andesite | 0.3 | 38 | FT008597 | 667809 | 8921971 | Qtz-sulphide vein | 0.3 | 28392 | ||
| FT00960 | 666935 | 8921904 | Gossan | 0.3 | 204 | FT5311 | 667046 | 8922081 | Basalt | 0.3 | 8784 | ||
| FT5105 | 667349 | 8923220 | Andesite | 0.3 | 4265 | FT5120 | 666881 | 8923366 | Basalt | 0.3 | 14559 | ||
| FT00892 | 666843 | 8922400 | Basalt | 0.3 | 316 | FT5164 | 666989 | 8923222 | Basalt | 0.3 | 1132 | ||
| FT008734 | 666931 | 8922030 | Qtz-sulphide vein | 0.3 | 373 | FT00821 | 667592 | 8923666 | Andesite | 0.3 | 57 | ||
| FT5067 | 667489 | 8923808 | Andesite | 0.3 | 60 | FT5053 | 667476 | 8923804 | Basalt | 0.3 | 11 | ||
| FT5214 | 666954 | 8921917 | Andesite | 0.3 | 2132 | FT5104 | 667194 | 8923518 | Basalt | 0.3 | 490 | ||
| FT5227 | 667013 | 8922012 | Andesite | 0.3 | 1778 | FT5379 | 667516 | 8923840 | IMD | 0.3 | 594 | ||
| FT3075 | 668913 | 8923306 | Qtz-sulphide vein | 0.3 | 36 | FT5307 | 667624 | 8922232 | Andesite | 0.3 | 1062 | ||
| FT008557 | 667962 | 8921820 | Breccia | 0.3 | 16211 | FT5546 | 667925 | 8923519 | Andesite | 0.3 | 7382 | ||
| FT008553 | 667404 | 8921880 | Qtz-sulphide vein | 0.3 | 907 | FT5354 | 667956 | 8922065 | not logged | 0.3 | 26955 | ||
| FT0056 | 667401 | 8921998 | not logged | 0.3 | 12263 | FT5286 | 668041 | 8922052 | Andesite | 0.3 | 33347 | ||
| FT5098 | 667363 | 8923636 | Basalt | 0.3 | 14102 | FT5338 | 666980 | 8921995 | Andesite | 0.3 | 722 | ||
| FT008715 | 666926 | 8922062 | Andesite | 0.3 | 68 | FT00812 | 667157 | 8923042 | IAG | 0.2 | 12292 | ||
| FT5062 | 667485 | 8923805 | Basalt | 0.3 | 356 | FT5081 | 667447 | 8923802 | Andesite | 0.2 | 561 | ||
| FT3058 | 667652 | 8923992 | Qtz-sulphide vein | 0.3 | 49 | FT00828 | 667462 | 8923645 | Basalt | 0.2 | 15008 | ||
| FT5063 | 667486 | 8923805 | Basalt | 0.3 | 83 | FT00968 | 667427 | 8922011 | Gossan | 0.2 | 10018 | ||
| FT5116 | 666949 | 8923650 | Gossan | 0.3 | 8453 | FT5089 | 667475 | 8923790 | Andesite | 0.2 | 84 | ||
| FT3023 | 667786 | 8924309 | Basalt | 0.3 | 204 | FT5822 | 667373 | 8923643 | Basalt | 0.2 | 25 | ||
| FT5083 | 667624 | 8923724 | Basalt | 0.3 | 35429 | FT00985 | 667411 | 8922006 | Gossan | 0.2 | 1863 | ||
| FT008550 | 666779 | 8921589 | Qtz-sulphide vein | 0.3 | 253 | FT5070 | 667490 | 8923811 | Andesite | 0.2 | 27 | ||
| FT008724 | 666921 | 8922070 | Andesite | 0.3 | 343 | FT5173 | 667027 | 8921976 | Andesite | 0.2 | 916 | ||
| FT3011 | 667991 | 8922002 | Qtz-sulphide vein | 0.3 | 35373 | FT5347 | 666970 | 8921992 | Andesite | 0.2 | 998 |
21
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT3017 | 668390 | 8922772 | Qtz-sulphide vein | 0.2 | 6011 | FT5538 | 668400 | 8923436 | Basalt | 0.2 | 0 | ||
| FT3036 | 667938 | 8924479 | Breccia | 0.2 | 26760 | FT5251 | 668045 | 8921950 | Basalt | 0.2 | 3792 | ||
| FT5065 | 667488 | 8923806 | Andesite | 0.2 | 149 | FT0046 | 648551 | 8941396 | SSC | 0.2 | 923 | ||
| FT0054 | 667339 | 8921891 | not logged | 0.2 | 3327 | FT009008 | 667087 | 8922048 | Basalt | 0.2 | 934 | ||
| FT3052 | 667682 | 8923972 | Andesite | 0.2 | 830 | FT5052 | 667476 | 8923803 | Basalt | 0.2 | 11 | ||
| FT5060 | 667483 | 8923805 | Andesite | 0.2 | 468 | FT5281 | 666769 | 8924194 | Basalt | 0.2 | 813 | ||
| FT00978 | 667417 | 8922009 | Qtz-sulphide vein | 0.2 | 17278 | FT5504 | 668854 | 8923765 | Andesite | 0.2 | 72 | ||
| FT5791 | 667330 | 8923652 | Basalt | 0.2 | 374 | FT00950 | 666941 | 8922019 | Basalt | 0.2 | 1062 | ||
| FT5221 | 667017 | 8922016 | Andesite | 0.2 | 1155 | FT008558 | 667808 | 8921983 | Gossan | 0.2 | 8660 | ||
| FT00982 | 667413 | 8922008 | Gossan | 0.2 | 4501 | FT008797 | 666957 | 8921952 | Basalt | 0.2 | 309 | ||
| FT5055 | 667478 | 8923804 | Basalt | 0.2 | 10 | FT5377 | 667518 | 8923840 | IMD | 0.2 | 241 | ||
| FT008711 | 666867 | 8922196 | Andesite | 0.2 | 156 | FT5802 | 667336 | 8923644 | Basalt | 0.2 | 6018 | ||
| FT5051 | 667475 | 8923802 | Basalt | 0.2 | 12 | FT5826 | 667306 | 8923644 | Basalt | 0.2 | 64 | ||
| FT5309 | 667041 | 8922049 | Basalt | 0.2 | 9213 | FT00895 | 666840 | 8922400 | Basalt | 0.2 | 449 | ||
| FT5507 | 669278 | 8923107 | not logged | 0.2 | 5281 | FT5350 | 667963 | 8922062 | not logged | 0.2 | 28998 | ||
| FT5071 | 667491 | 8923813 | Andesite | 0.2 | 27 | FT00963 | 667431 | 8922013 | Gossan | 0.2 | 23276 | ||
| FT5143 | 667025 | 8922121 | Basalt | 0.2 | 920 | FT3012 | 667873 | 8922030 | Qtz-sulphide vein | 0.2 | 1887 | ||
| FT3048 | 667066 | 8923918 | Andesite | 0.2 | 61 | FT5204 | 666969 | 8921916 | Qtz-sulphide vein | 0.2 | 389 | ||
| FT5144 | 667023 | 8922120 | Basalt | 0.2 | 868 | FT5064 | 667487 | 8923805 | Basalt | 0.2 | 24 | ||
| FT5068 | 667489 | 8923808 | Andesite | 0.2 | 21 | FT5342 | 666919 | 8921977 | Andesite | 0.2 | 1753 | ||
| FT5087 | 667760 | 8924025 | Basalt | 0.2 | 13 | FT5353 | 667958 | 8922064 | Basalt | 0.1 | 15809 | ||
| FT5310 | 667046 | 8922084 | Basalt | 0.2 | 4262 | FT5505 | 668832 | 8923635 | not logged | 0.1 | 20759 | ||
| FT5075 | 667475 | 8923801 | Andesite | 0.2 | 12 | FT3022 | 667839 | 8924212 | Basalt | 0.1 | 246 | ||
| FT008777 | 666945 | 8921982 | IDM | 0.2 | 482 | FT5305 | 668175 | 8922476 | Andesite | 0.1 | 525 | ||
| FT5056 | 667479 | 8923804 | Basalt | 0.2 | 107 | FT5180 | 667378 | 8922010 | Basalt | 0.1 | 88 | ||
| FT5267 | 668061 | 8921950 | Basalt | 0.2 | 2326 | FT5830 | 667373 | 8923651 | Basalt | 0.1 | 65 | ||
| FT0055 | 667342 | 8921882 | not logged | 0.2 | 2757 | FT5258 | 668052 | 8921950 | Basalt | 0.1 | 6312 | ||
| FT5259 | 668053 | 8921950 | Basalt | 0.2 | 3026 | FT008729 | 666918 | 8922074 | Andesite | 0.1 | 320 | ||
| FT5058 | 667481 | 8923804 | Basalt | 0.2 | 23 | FT5057 | 667480 | 8923804 | Basalt | 0.1 | 20 | ||
| FT00893 | 666842 | 8922400 | Basalt | 0.2 | 412 | FT5346 | 666970 | 8921991 | Andesite | 0.1 | 382 | ||
| FT5276 | 666850 | 8923911 | Basalt | 0.2 | 2098 | FT00810 | 666783 | 8923039 | Basalt | 0.1 | 243 | ||
| FT00852 | 666482 | 8922472 | Basalt | 0.2 | 2803 | FT5112 | 667048 | 8923501 | IAG | 0.1 | 15021 | ||
| FT5186 | 667378 | 8922021 | Basalt | 0.2 | 165 | FT5085 | 667450 | 8923725 | Basalt | 0.1 | 23 | ||
| FT3001 | 667459 | 8922090 | Gossan | 0.2 | 18614 | FT5111 | 667052 | 8923497 | BHO | 0.1 | 22347 | ||
| FT5054 | 667477 | 8923804 | Basalt | 0.2 | 8 | FT5260 | 668054 | 8921950 | Basalt | 0.1 | 7501 |
22
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT5253 | 668047 | 8921950 | Basalt | 0.1 | 3713 | FT5355 | 667954 | 8922065 | not | logged | 0.1 | 10332 | |
| FT5515 | 669325 | 8922575 | not logged | 0.1 | 14893 | FT00987 | 667409 | 8922005 | Gossan | 0.1 | 1407 | ||
| FT00860 | 666852 | 8922400 | Andesite | 0.1 | 201 | FT5170 | 667050 | 8922878 | IAG | 0.1 | 50 | ||
| FT3037 | 667937 | 8924479 | Qtz-sulphide vein | 0.1 | 13721 | FT5362 | 667554 | 8923840 | Basalt | 0.1 | 963 | ||
| FT5046 | 667474 | 8923797 | Andesite | 0.1 | 12 | FT00827 | 667621 | 8923733 | Basalt | 0.1 | 3127 | ||
| FT0058 | 666778 | 8920451 | not logged | 0.1 | 2354 | FT5072 | 667492 | 8923814 | Andesite | 0.1 | 21 | ||
| FT009034 | 667961 | 8921894 | Basalt | 0.1 | 3204 | FT5073 | 667494 | 8923816 | Andesite | 0.1 | 45 | ||
| FT00840 | 666481 | 8922461 | Basalt | 0.1 | 556 | FT008710 | 666868 | 8922196 | Andesite | 0.1 | 351 | ||
| FT3003 | 667454 | 8921943 | Basalt | 0.1 | 599 | FT5217 | 667028 | 8922027 | Andesite | 0.1 | 643 | ||
| FT5373 | 667528 | 8923840 | IMD | 0.1 | 303 | FT5294 | 667434 | 8921832 | Basalt | 0.1 | 487 | ||
| FT008717 | 666924 | 8922063 | Andesite | 0.1 | 88 | FT00850 | 666482 | 8922471 | Basalt | 0.1 | 782 | ||
| FT009037 | 667963 | 8921896 | Qtz-sulphide vein | 0.1 | 18437 | FT5295 | 667434 | 8921831 | Basalt | 0.1 | 149 | ||
| FT008602 | 667949 | 8921967 | Andesite | 0.1 | 16787 | FT5335 | 666975 | 8921994 | Andesite | 0.1 | 573 | ||
| FT009050 | 667975 | 8921898 | Qtz-sulphide vein | 0.1 | 1886 | FT00896 | 666839 | 8922400 | Basalt | 0.1 | 464 | ||
| FT00965 | 667429 | 8922013 | Gossan | 0.1 | 2910 | FT00993 | 668633 | 8924764 | Gossan | 0.1 | 16823 | ||
| FT3014 | 668251 | 8922556 | Gossan | 0.1 | 42950 | FT00894 | 666841 | 8922400 | Basalt | 0.1 | 382 | ||
| FT5050 | 667475 | 8923801 | Andesite | 0.1 | 35 | FT5366 | 667550 | 8923840 | Basalt | 0.1 | 1445 | ||
| FT5242 | 667484 | 8923805 | Basalt | 0.1 | 19640 | FT3061 | 667518 | 8922136 | Basalt | 0.1 | 494 | ||
| FT5376 | 667519 | 8923840 | IMD | 0.1 | 117 | FT008723 | 666921 | 8922069 | Andesite | 0.1 | 166 | ||
| FT5516 | 669366 | 8922721 | VOO | 0.1 | 5787 | FT009039 | 667965 | 8921897 | Qtz-sulphide vein | 0.1 | 5441 | ||
| FT5794 | 667333 | 8923650 | Basalt | 0.1 | 2195 | FT5283 | 666891 | 8924484 | Basalt | 0.1 | 26379 | ||
| FT008720 | 666924 | 8922069 | Andesite | 0.1 | 182 | FT5266 | 668060 | 8921950 | Basalt | 0.1 | 1827 | ||
| FT009038 | 667964 | 8921896 | Qtz-sulphide vein | 0.1 | 21094 | FT00887 | 666915 | 8922000 | Basalt | 0.1 | 439 | ||
| FT00853 | 666483 | 8922473 | Basalt | 0.1 | 2026 | FT5550 | 667807 | 8921742 | Andesite | 0.1 | 229 | ||
| FT008746 | 666949 | 8921979 | Andesite | 0.1 | 408 | FT5816 | 667303 | 8923651 | Basalt | 0.1 | 482 | ||
| FT3040 | 667936 | 8924482 | Qtz-sulphide vein | 0.1 | 11679 | FT5042 | 667471 | 8923790 | Andesite | 0.1 | 60 | ||
| FT5545 | 668060 | 8923371 | Andesite | 0.1 | 124 | FT5047 | 667474 | 8923798 | Andesite | 0.1 | 27 | ||
| FT5378 | 667517 | 8923840 | IMD | 0.1 | 190 | FT5360 | 667556 | 8923840 | IAG | 0.1 | 116 | ||
| FT3027 | 667550 | 8924440 | Andesite | 0.1 | 46 | FT00970 | 667425 | 8922011 | Gossan | 0.1 | 1707 | ||
| FT5171 | 667046 | 8922801 | Basalt | 0.1 | 1971 | FT3054 | 668055 | 8924750 | Qtz-sulphide vein | 0.1 | 12512 | ||
| FT5336 | 666978 | 8921994 | Andesite | 0.1 | 642 | FT009044 | 667969 | 8921899 | Qtz-sulphide vein | 0.1 | 7438 | ||
| FT5312 | 667046 | 8922078 | Basalt | 0.1 | 1123 | FT3013 | 668097 | 8922301 | Qtz-sulphide vein | 0.1 | 13092 | ||
| FT009041 | 667967 | 8921898 | Basalt | 0.1 | 8992 | FT5045 | 667473 | 8923796 | Andesite | 0.1 | 23 | ||
| FT00966 | 667428 | 8922012 | Gossan | 0.1 | 11246 | FT008601 | 667903 | 8921944 | Andesite | 0.1 | 250 | ||
| FT00822 | 667598 | 8923665 | Andesite | 0.1 | 459 | FT5337 | 666979 | 8921994 | Andesite | 0.1 | 296 |
23
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT5372 | 667529 | 8923840 | IMD | 0.1 | 539 | FT009046 | 667971 | 8921899 | Basalt | 0.1 | 4012 | ||
| FT00803 | 667204 | 8923520 | MSP | 0.1 | 3656 | FT3066 | 669164 | 8923225 | Andesite | 0.1 | 5264 | ||
| FT008727 | 666919 | 8922073 | Andesite | 0.1 | 78 | FT5508 | 669278 | 8923107 | not logged | 0.1 | 4843 | ||
| FT008798 | 666958 | 8921953 | Basalt | 0.1 | 148 | FT00833 | 666483 | 8922454 | Basalt | 0.1 | 260 | ||
| FT5349 | 667965 | 8922061 | not logged | 0.1 | 3223 | FT008786 | 666798 | 8923981 | Basalt | 0.1 | 4222 | ||
| FT5357 | 668000 | 8922009 | Basalt | 0.1 | 20341 | FT009052 | 667977 | 8921898 | Basalt | 0.1 | 1371 | ||
| FT5529 | 667890 | 8924547 | IDM | 0.1 | 1023 | FT3016 | 668487 | 8922830 | Qtz-sulphide vein | 0.1 | 838 | ||
| FT5252 | 668046 | 8921950 | Basalt | 0.1 | 1409 | FT3018 | 667904 | 8922561 | Qtz-sulphide vein | 0.1 | 4224 | ||
| FT5367 | 667549 | 8923840 | Basalt | 0.1 | 193 | FT00814 | 667141 | 8922881 | IAG | 0.1 | 1351 | ||
| FT00841 | 666481 | 8922462 | Basalt | 0.1 | 439 | FT5114 | 667030 | 8923530 | IAG | 0.1 | 7886 | ||
| FT3031 | 667030 | 8924555 | Basalt | 0.1 | 94 | FT5832 | 667373 | 8923655 | Basalt | 0.1 | 63 | ||
| FT5509 | 669299 | 8923054 | not logged | 0.1 | 14578 | FT008722 | 666922 | 8922069 | Andesite | 0.1 | 63 | ||
| FT00891 | 666844 | 8922400 | Basalt | 0.1 | 351 | FT00988 | 667408 | 8922005 | Gossan | 0.1 | 3197 | ||
| FT5334 | 666974 | 8921994 | Andesite | 0.1 | 844 | FT3041 | 667935 | 8924483 | Qtz-sulphide vein | 0.1 | 5203 | ||
| FT00977 | 667418 | 8922010 | Qtz-sulphide vein | 0.1 | 16422 | FT5261 | 668055 | 8921950 | Basalt | 0.1 | 3484 | ||
| FT5117 | 666929 | 8923543 | IAG | 0.1 | 14905 | FT5340 | 666982 | 8921995 | Basalt | 0.1 | 287 | ||
| FT5274 | 668025 | 8921950 | Basalt | 0.1 | 7226 | FT5363 | 667553 | 8923840 | Basalt | 0.1 | 1109 | ||
| FT5514 | 669325 | 8922575 | not logged | 0.1 | 28 | FT5521 | 668462 | 8924327 | IDM | 0.1 | 700 | ||
| FT00990 | 666946 | 8921890 | Qtz-sulphide vein | 0.1 | 497 | FT5828 | 667373 | 8923647 | Basalt | 0.1 | 836 | ||
| FT00974 | 667421 | 8922010 | Gossan | 0.1 | 6600 | FT008793 | 666960 | 8921958 | Basalt | 0.1 | 174 | ||
| FT3056 | 667456 | 8924551 | Gossan | 0.1 | 29 | FT00998 | 668141 | 8924364 | Basalt | 0.1 | 2304 | ||
| FT3077 | 668928 | 8923464 | IAG | 0.1 | 539 | FT5370 | 667546 | 8923840 | IDD | 0.1 | 1730 | ||
| FT5532 | 667594 | 8924767 | IDD | 0.1 | 26988 | FT5179 | 667378 | 8922008 | Basalt | 0.0 | 82 | ||
| FT00975 | 667420 | 8922010 | Gossan | 0.1 | 6341 | FT00849 | 666482 | 8922470 | Basalt | 0.0 | 510 | ||
| FT5048 | 667474 | 8923799 | Andesite | 0.1 | 18 | FT5306 | 668269 | 8922872 | Andesite | 0.0 | 1094 | ||
| FT5271 | 668028 | 8921950 | Basalt | 0.1 | 6671 | FT5348 | 667967 | 8922061 | not logged | 0.0 | 6599 | ||
| FT5324 | 667963 | 8921949 | Basalt | 0.1 | 6743 | FT00973 | 667422 | 8922010 | Gossan | 0.0 | 4145 | ||
| FT008743 | 666925 | 8922037 | Andesite | 0.1 | 2466 | FT00991 | 667266 | 8922077 | Qtz-sulphide vein | 0.0 | 24 | ||
| FT3026 | 667563 | 8924453 | Andesite | 0.1 | 36 | FT3019 | 667890 | 8924146 | Basalt | 0.0 | 2450 | ||
| FT3044 | 667956 | 8924516 | IAG | 0.1 | 3713 | FT5119 | 666886 | 8923417 | Basalt | 0.0 | 1154 | ||
| FT5076 | 667474 | 8923804 | Andesite | 0.1 | 35 | FT5297 | 667434 | 8921829 | Basalt | 0.0 | 132 | ||
| FT5255 | 668049 | 8921950 | Basalt | 0.1 | 1324 | FT5329 | 667987 | 8921952 | not logged | 0.0 | 211 | ||
| FT00986 | 667410 | 8922006 | Gossan | 0.1 | 2220 | FT00995 | 668627 | 8924772 | Qtz-sulphide vein | 0.0 | 3840 | ||
| FT5343 | 666944 | 8921989 | Andesite | 0.1 | 128 | FT00800 | 666828 | 8922395 | Basalt | 0.0 | 371 | ||
| FT00867 | 666865 | 8922300 | Andesite | 0.1 | 92 | FT008606 | 667882 | 8921954 | Andesite | 0.0 | 476 |
24
25 November 2022 ASX Announcement
==> picture [103 x 68] intentionally omitted <==
ASX: LCL
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT009048 | 667973 | 8921899 | Basalt | 0.0 | 2719 | FT009012 | 667983 | 8921850 | Basalt | 0.0 | 288 | ||
| FT5209 | 666969 | 8921912 | Qtz-sulphide vein | 0.0 | 553 | FT5304 | 668085 | 8922235 | Andesite | 0.0 | 164 | ||
| FT5256 | 668050 | 8921950 | Basalt | 0.0 | 808 | FT008738 | 666928 | 8922033 | Andesite | 0.0 | 476 | ||
| FT0049 | 667348 | 8921915 | not logged | 0.0 | 548 | FT5322 | 667960 | 8921947 | Basalt | 0.0 | 145 | ||
| FT008607 | 667881 | 8921955 | Andesite | 0.0 | 471 | FT00802 | 667202 | 8923563 | Basalt | 0.0 | 312 | ||
| FT3034 | 667887 | 8924510 | Basalt | 0.0 | 1016 | FT00813 | 667172 | 8923050 | IAG | 0.0 | 3098 | ||
| FT5374 | 667527 | 8923840 | IMD | 0.0 | 155 | FT008735 | 666930 | 8922031 | Andesite | 0.0 | 265 | ||
| FT5547 | 669875 | 8922992 | Basalt | 0.0 | 670 | FT3049 | 667553 | 8923946 | Andesite | 0.0 | 70 | ||
| FT00839 | 666482 | 8922460 | Basalt | 0.0 | 481 | FT5080 | 667466 | 8923804 | Andesite | 0.0 | 479 | ||
| FT5530 | 667469 | 8924593 | IAG | 0.0 | 34 | FT00848 | 666482 | 8922469 | Basalt | 0.0 | 427 | ||
| FT5819 | 667373 | 8923637 | Basalt | 0.0 | 238 | FT008703 | 666896 | 8922200 | Andesite | 0.0 | 50 | ||
| FT008706 | 666893 | 8922200 | Andesite | 0.0 | 67 | FT009016 | 667492 | 8921955 | Basalt | 0.0 | 141 | ||
| FT5110 | 667064 | 8923493 | BHO | 0.0 | 7724 | FT009028 | 667491 | 8921936 | Basalt | 0.0 | 221 | ||
| FT5149 | 667554 | 8921965 | Basalt | 0.0 | 77 | FT5301 | 667434 | 8921824 | Basalt | 0.0 | 202 | ||
| FT5241 | 666568 | 8920695 | Basalt | 0.0 | 67 | FT5358 | 667560 | 8923840 | IAG | 0.0 | 80 | ||
| FT5293 | 667434 | 8921833 | Basalt | 0.0 | 655 | FT009042 | 667968 | 8921898 | Basalt | 0.0 | 3854 | ||
| FT008708 | 666895 | 8922196 | Andesite | 0.0 | 94 | FT00994 | 668638 | 8924776 | Qtz-sulphide vein | 0.0 | 36688 | ||
| FT009047 | 667972 | 8921899 | Basalt | 0.0 | 1455 | FT3055 | 667971 | 8924554 | Qtz-sulphide vein | 0.0 | 767 | ||
| FT5243 | 667624 | 8923725 | Basalt | 0.0 | 5934 | FT5194 | 666962 | 8921865 | Andesite | 0.0 | 101 | ||
| FT5800 | 667336 | 8923646 | Basalt | 0.0 | 691 | FT5344 | 666956 | 8921972 | Andesite | 0.0 | 90 | ||
| FT0062 | 666831 | 8921697 | not logged | 0.0 | 769 | FT5517 | 669343 | 8922735 | not logged | 0.0 | 114 | ||
| FT008705 | 666894 | 8922200 | Andesite | 0.0 | 92 | FT008791 | 666972 | 8921932 | Basalt | 0.0 | 46 | ||
| FT5519 | 667963 | 8924515 | Andesite | 0.0 | 61 | FT009011 | 667984 | 8921851 | Basalt | 0.0 | 473 | ||
| FT5789 | 667326 | 8923652 | Basalt | 0.0 | 76 | FT5074 | 667495 | 8923817 | Andesite | 0.0 | 200 | ||
| FT3042 | 667934 | 8924483 | Qtz-sulphide vein | 0.0 | 5059 | FT5540 | 668348 | 8923233 | PBI | 0.0 | 149 | ||
| FT5093 | 667309 | 8923642 | Basalt | 0.0 | 2206 | FT0045 | 648550 | 8941395 | PFH | 0.0 | 640 | ||
| FT3047 | 667039 | 8923867 | Andesite | 0.0 | 1135 | FT008718 | 666924 | 8922065 | Andesite | 0.0 | 53 | ||
| FT00847 | 666482 | 8922468 | Andesite | 0.0 | 465 | FT00964 | 667430 | 8922013 | Gossan | 0.0 | 8558 | ||
| FT008728 | 666919 | 8922073 | Andesite | 0.0 | 89 | FT3039 | 667936 | 8924481 | BHO | 0.0 | 4268 | ||
| FT00999 | 667922 | 8924377 | Qtz-sulphide vein | 0.0 | 359 | FT5803 | 667337 | 8923643 | Basalt | 0.0 | 1596 | ||
| FT5091 | 667680 | 8923956 | Andesite | 0.0 | 25 | FT5817 | 667302 | 8923652 | Basalt | 0.0 | 149 | ||
| FT5365 | 667551 | 8923840 | Basalt | 0.0 | 230 | FT009043 | 667968 | 8921899 | Qtz-sulphide vein | 0.0 | 3922 | ||
| FT5368 | 667548 | 8923840 | Basalt | 0.0 | 244 | FT5265 | 668059 | 8921950 | Basalt | 0.0 | 561 | ||
| FT5369 | 667547 | 8923840 | IDD | 0.0 | 776 | FT5273 | 668026 | 8921950 | Basalt | 0.0 | 1615 | ||
| FT5510 | 669123 | 8923239 | VMO | 0.0 | 2960 | FT008600 | 667905 | 8921945 | Andesite | 0.0 | 254 |
25
25 November 2022 ASX Announcement
==> picture [103 x 68] intentionally omitted <==
ASX: LCL
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT008719 | 666924 | 8922067 | Andesite | 0.0 | 159 | FT009027 | 667489 | 8921937 | Basalt | 0.0 | 179 | ||
| FT009049 | 667974 | 8921898 | Basalt | 0.0 | 1235 | FT00955 | 666939 | 8921908 | Basalt | 0.0 | 442 | ||
| FT5208 | 666969 | 8921913 | Qtz-sulphide vein | 0.0 | 342 | FT3028 | 667505 | 8924537 | Qtz-sulphide vein | 0.0 | 2216 | ||
| FT5210 | 666969 | 8921911 | Qtz-sulphide vein | 0.0 | 398 | FT3051 | 667639 | 8923981 | Andesite | 0.0 | 51 | ||
| FT5356 | 668015 | 8922076 | Basalt | 0.0 | 5727 | FT5181 | 667378 | 8922012 | Basalt | 0.0 | 95 | ||
| FT009051 | 667976 | 8921898 | Basalt | 0.0 | 1784 | FT5317 | 667963 | 8921949 | Basalt | 0.0 | 332 | ||
| FT5250 | 668044 | 8921950 | Basalt | 0.0 | 1610 | FT5351 | 667961 | 8922063 | not logged | 0.0 | 3807 | ||
| FT5543 | 668318 | 8922918 | Basalt | 0.0 | 156 | FT0050 | 667330 | 8921917 | not logged | 0.0 | 2283 | ||
| FT5544 | 668185 | 8923086 | Andesite | 0.0 | 39 | FT3079 | 668657 | 8923656 | Qtz-sulphide vein | 0.0 | 79 | ||
| FT00806 | 666467 | 8922466 | Basalt | 0.0 | 48 | FT5298 | 667434 | 8921828 | Basalt | 0.0 | 68 | ||
| FT00835 | 666482 | 8922456 | Basalt | 0.0 | 382 | FT5527 | 667924 | 8924525 | IDM | 0.0 | 254 | ||
| FT008599 | 667907 | 8921945 | Andesite | 0.0 | 357 | FT5534 | 669353 | 8924173 | not logged | 0.0 | 62 | ||
| FT009026 | 667487 | 8921937 | Basalt | 0.0 | 84 | FT5536 | 669575 | 8924130 | not logged | 0.0 | 44 | ||
| FT00949 | 666940 | 8922020 | Basalt | 0.0 | 154 | FT00830 | 666484 | 8922451 | Basalt | 0.0 | 129 | ||
| FT00954 | 666942 | 8922014 | Basalt | 0.0 | 94 | FT009017 | 667491 | 8921953 | Basalt | 0.0 | 107 | ||
| FT00971 | 667424 | 8922011 | Gossan | 0.0 | 402 | FT009018 | 667491 | 8921951 | Basalt | 0.0 | 82 | ||
| FT5506 | 668611 | 8923681 | not logged | 0.0 | 44 | FT3068 | 668722 | 8923395 | Andesite | 0.0 | 203 | ||
| FT0052 | 667333 | 8921920 | not logged | 0.0 | 720 | FT5109 | 667065 | 8923489 | BHO | 0.0 | 3106 | ||
| FT0059 | 666749 | 8921459 | not logged | 0.0 | 151 | FT5503 | 668904 | 8923710 | Andesite | 0.0 | 6320 | ||
| FT009013 | 667982 | 8921850 | Basalt | 0.0 | 413 | FT00815 | 667273 | 8923297 | Qtz-sulphide vein | 0.0 | 2228 | ||
| FT3065 | 669163 | 8923225 | Qtz-sulphide vein | 0.0 | 2028 | FT00836 | 666482 | 8922457 | Basalt | 0.0 | 233 | ||
| FT5523 | 668086 | 8924389 | IDM | 0.0 | 1414 | FT00855 | 666483 | 8922475 | Basalt | 0.0 | 674 | ||
| FT5825 | 667306 | 8923646 | Basalt | 0.0 | 64 | FT00856 | 666483 | 8922476 | Basalt | 0.0 | 236 | ||
| FT5829 | 667373 | 8923649 | Basalt | 0.0 | 42 | FT009015 | 667492 | 8921957 | Basalt | 0.0 | 84 | ||
| FT009025 | 667487 | 8921939 | Basalt | 0.0 | 112 | FT009024 | 667487 | 8921941 | Basalt | 0.0 | 176 | ||
| FT009053 | 667978 | 8921898 | Basalt | 0.0 | 1080 | FT009045 | 667970 | 8921899 | Qtz-sulphide vein | 0.0 | 3347 | ||
| FT5139 | 667973 | 8921850 | Basalt | 0.0 | 916 | FT00829 | 666484 | 8922450 | Basalt | 0.0 | 187 | ||
| FT5163 | 667006 | 8923263 | Basalt | 0.0 | 3797 | FT008712 | 666866 | 8922196 | Andesite | 0.0 | 36 | ||
| FT5182 | 667378 | 8922014 | Basalt | 0.0 | 119 | FT008789 | 666956 | 8921882 | Basalt | 0.0 | 7 | ||
| FT5371 | 667530 | 8923840 | IMD | 0.0 | 165 | FT00890 | 666845 | 8922400 | Basalt | 0.0 | 128 | ||
| FT5542 | 668336 | 8923196 | POO | 0.0 | 82 | FT009021 | 667489 | 8921946 | Basalt | 0.0 | 204 | ||
| FT00844 | 666481 | 8922465 | Basalt | 0.0 | 1318 | FT5049 | 667475 | 8923800 | Andesite | 0.0 | 66 | ||
| FT008604 | 667883 | 8921953 | Andesite | 0.0 | 370 | FT5138 | 667974 | 8921850 | Basalt | 0.0 | 1373 | ||
| FT008608 | 667881 | 8921956 | Andesite | 0.0 | 75 | FT5206 | 666969 | 8921915 | Qtz-sulphide vein | 0.0 | 300 | ||
| FT009001 | 666959 | 8921957 | Basalt | 0.0 | 84 | FT5268 | 668062 | 8921950 | Basalt | 0.0 | 489 |
26
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT5522 | 668502 | 8924306 | Andesite | 0.0 | 20 | FT5101 | 667202 | 8923574 | Basalt | 0.0 | 671 | ||
| FT5541 | 668348 | 8923225 | Basalt | 0.0 | 121 | FT5137 | 667975 | 8921850 | Basalt | 0.0 | 884 | ||
| FT00808 | 667064 | 8923081 | IAG | 0.0 | 31 | FT5254 | 668048 | 8921950 | Basalt | 0.0 | 837 | ||
| FT008702 | 666898 | 8922200 | Andesite | 0.0 | 162 | FT5269 | 668030 | 8921950 | Basalt | 0.0 | 718 | ||
| FT008713 | 666865 | 8922196 | Andesite | 0.0 | 60 | FT5345 | 666958 | 8921972 | Andesite | 0.0 | 97 | ||
| FT009019 | 667491 | 8921949 | Basalt | 0.0 | 92 | FT00832 | 666483 | 8922453 | Basalt | 0.0 | 186 | ||
| FT009022 | 667487 | 8921945 | Basalt | 0.0 | 167 | FT008697 | 668460 | 8924315 | Andesite | 0.0 | 1773 | ||
| FT009035 | 667962 | 8921895 | Basalt | 0.0 | 3634 | FT008704 | 666895 | 8922200 | Andesite | 0.0 | 310 | ||
| FT009036 | 667963 | 8921895 | Basalt | 0.0 | 3987 | FT008739 | 666928 | 8922034 | Andesite | 0.0 | 766 | ||
| FT5147 | 667556 | 8921965 | Basalt | 0.0 | 54 | FT008745 | 666950 | 8921979 | Andesite | 0.0 | 136 | ||
| FT5185 | 667378 | 8922020 | Basalt | 0.0 | 430 | FT009023 | 667487 | 8921943 | Basalt | 0.0 | 137 | ||
| FT5548 | 669929 | 8922905 | Basalt | 0.0 | 68 | FT00951 | 666941 | 8922019 | Basalt | 0.0 | 106 | ||
| FT00834 | 666483 | 8922455 | Basalt | 0.0 | 183 | FT3038 | 667937 | 8924481 | Qtz-sulphide vein | 0.0 | 1395 | ||
| FT009020 | 667490 | 8921947 | Basalt | 0.0 | 137 | FT5133 | 667979 | 8921850 | Basalt | 0.0 | 342 | ||
| FT009033 | 667484 | 8921912 | Basalt | 0.0 | 133 | FT5183 | 667378 | 8922016 | Basalt | 0.0 | 120 | ||
| FT00953 | 666942 | 8922015 | Basalt | 0.0 | 64 | FT5263 | 668057 | 8921950 | Basalt | 0.0 | 1157 | ||
| FT5205 | 666969 | 8921916 | Qtz-sulphide vein | 0.0 | 188 | FT008730 | 666918 | 8922075 | Andesite | 0.0 | 548 | ||
| FT5249 | 668043 | 8921950 | Basalt | 0.0 | 2700 | FT5299 | 667434 | 8921827 | Basalt | 0.0 | 95 | ||
| FT5262 | 668056 | 8921950 | Basalt | 0.0 | 1333 | FT5313 | 667975 | 8921950 | Basalt | 0.0 | 795 | ||
| FT5321 | 667958 | 8921946 | Basalt | 0.0 | 311 | FT5326 | 667981 | 8921951 | not logged | 0.0 | 858 | ||
| FT5821 | 667373 | 8923641 | Basalt | 0.0 | 8 | FT5831 | 667373 | 8923653 | Basalt | 0.0 | 27 | ||
| FT00831 | 666483 | 8922452 | Basalt | 0.0 | 259 | FT00838 | 666482 | 8922459 | Basalt | 0.0 | 176 | ||
| FT008701 | 666900 | 8922200 | Andesite | 0.0 | 69 | FT00842 | 666481 | 8922463 | Basalt | 0.0 | 51 | ||
| FT009054 | 667979 | 8921898 | Basalt | 0.0 | 885 | FT00861 | 666851 | 8922400 | Andesite | 0.0 | 47 | ||
| FT00996 | 668569 | 8924809 | Qtz-sulphide vein | 0.0 | 1524 | FT00863 | 666849 | 8922400 | Andesite | 0.0 | 74 | ||
| FT00997 | 668539 | 8924748 | Qtz-sulphide vein | 0.0 | 1991 | FT00864 | 666848 | 8922400 | Andesite | 0.0 | 26 | ||
| FT3043 | 667934 | 8924485 | Qtz-sulphide vein | 0.0 | 1249 | FT008737 | 666929 | 8922032 | Andesite | 0.0 | 183 | ||
| FT5135 | 667977 | 8921850 | Basalt | 0.0 | 959 | FT00947 | 666940 | 8922022 | Basalt | 0.0 | 16 | ||
| FT5315 | 667979 | 8921951 | Basalt | 0.0 | 404 | FT5132 | 667980 | 8921850 | Basalt | 0.0 | 813 | ||
| FT0051 | 667327 | 8921923 | not logged | 0.0 | 113 | FT5134 | 667978 | 8921850 | Basalt | 0.0 | 409 | ||
| FT00816 | 667184 | 8923388 | Andesite | 0.0 | 233 | FT0060 | 666746 | 8921461 | not logged | 0.0 | 187 | ||
| FT00837 | 666482 | 8922458 | Basalt | 0.0 | 255 | FT008750 | 666946 | 8921982 | Andesite | 0.0 | 107 | ||
| FT00843 | 666481 | 8922464 | Basalt | 0.0 | 49 | FT00882 | 666880 | 8922300 | Andesite | 0.0 | 111 | ||
| FT008603 | 667884 | 8921952 | Andesite | 0.0 | 315 | FT00884 | 666882 | 8922300 | Andesite | 0.0 | 46 | ||
| FT008609 | 667880 | 8921957 | Andesite | 0.0 | 80 | FT009040 | 667966 | 8921897 | Qtz-sulphide vein | 0.0 | 4823 |
27
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT3029 | 667517 | 8924576 | IAG | 0.0 | 451 | FT3035 | 667912 | 8924399 | Basalt | 0.0 | 1037 | ||
| FT5136 | 667976 | 8921850 | Basalt | 0.0 | 1058 | FT3046 | 666991 | 8923840 | Andesite | 0.0 | 1066 | ||
| FT5184 | 667378 | 8922018 | Basalt | 0.0 | 306 | FT5100 | 667218 | 8923587 | Basalt | 0.0 | 231 | ||
| FT5189 | 667378 | 8922024 | Basalt | 0.0 | 58 | FT5131 | 667981 | 8921850 | Basalt | 0.0 | 645 | ||
| FT5245 | 668039 | 8921950 | Basalt | 0.0 | 4597 | FT5140 | 667972 | 8921850 | Basalt | 0.0 | 944 | ||
| FT5359 | 667558 | 8923840 | IAG | 0.0 | 73 | FT5148 | 667555 | 8921965 | Basalt | 0.0 | 22 | ||
| FT5528 | 667938 | 8924528 | Basalt | 0.0 | 310 | FT5203 | 666969 | 8921917 | Qtz-sulphide vein | 0.0 | 246 | ||
| FT5533 | 669267 | 8924222 | not logged | 0.0 | 25 | FT5247 | 668041 | 8921950 | Basalt | 0.0 | 3367 | ||
| FT00862 | 666850 | 8922400 | Andesite | 0.0 | 56 | FT5272 | 668027 | 8921950 | Basalt | 0.0 | 122 | ||
| FT00868 | 666866 | 8922300 | Andesite | 0.0 | 114 | FT5316 | 667965 | 8921950 | Basalt | 0.0 | 355 | ||
| FT008744 | 666951 | 8921980 | Andesite | 0.0 | 80 | FT5320 | 667890 | 8924547 | Basalt | 0.0 | 272 | ||
| FT00876 | 666874 | 8922300 | Andesite | 0.0 | 57 | FT5327 | 667983 | 8921952 | not logged | 0.0 | 1103 | ||
| FT00886 | 667014 | 8922112 | Basalt | 0.0 | 1010 | FT5178 | 667378 | 8922006 | Basalt | 0.0 | 71 | ||
| FT009055 | 667980 | 8921898 | Basalt | 0.0 | 1034 | FT5318 | 667962 | 8921948 | Basalt | 0.0 | 693 | ||
| FT00944 | 666939 | 8922024 | Basalt | 0.0 | 51 | FT5328 | 667985 | 8921952 | not logged | 0.0 | 541 | ||
| FT00945 | 666940 | 8922023 | Basalt | 0.0 | 68 | FT5518 | 668537 | 8924810 | Andesite | 0.0 | 13 | ||
| FT00948 | 666940 | 8922021 | Basalt | 0.0 | 60 | FT5526 | 667932 | 8924521 | IDM | 0.0 | 216 | ||
| FT00958 | 666937 | 8921906 | Basalt | 0.0 | 34 | FT5121 | 667981 | 8921898 | Basalt | 0.0 | 1063 | ||
| FT00959 | 666936 | 8921905 | Gossan | 0.0 | 73 | FT5177 | 667378 | 8922004 | Basalt | 0.0 | 121 | ||
| FT00992 | 668380 | 8924770 | Qtz-sulphide vein | 0.0 | 692 | FT5195 | 666962 | 8921864 | Andesite | 0.0 | 7 | ||
| FT5113 | 667026 | 8923518 | IAG | 0.0 | 2180 | FT5207 | 666969 | 8921914 | Basalt | 0.0 | 73 | ||
| FT5150 | 667553 | 8921965 | Basalt | 0.0 | 114 | FT5239 | 667474 | 8921959 | Basalt | 0.0 | 193 | ||
| FT5176 | 667378 | 8922002 | Basalt | 0.0 | 114 | FT5244 | 668038 | 8921950 | Basalt | 0.0 | 5944 | ||
| FT5248 | 668042 | 8921950 | Basalt | 0.0 | 2737 | FT5246 | 668040 | 8921950 | Basalt | 0.0 | 1606 | ||
| FT5257 | 668051 | 8921950 | Basalt | 0.0 | 1552 | FT5325 | 667965 | 8921950 | Basalt | 0.0 | 547 | ||
| FT5323 | 667962 | 8921948 | Basalt | 0.0 | 203 | FT5520 | 667971 | 8924517 | IDM | 0.0 | 38 | ||
| FT00851 | 666482 | 8922471 | Basalt | 0.0 | 58 | FT5123 | 667983 | 8921898 | Basalt | 0.0 | 446 | ||
| FT00871 | 666869 | 8922300 | Andesite | 0.0 | 95 | FT5124 | 667984 | 8921898 | Basalt | 0.0 | 468 | ||
| FT00873 | 666871 | 8922300 | Andesite | 0.0 | 95 | FT5126 | 667986 | 8921898 | Basalt | 0.0 | 518 | ||
| FT008732 | 666932 | 8922029 | Andesite | 0.0 | 588 | FT5151 | 667552 | 8921965 | Basalt | 0.0 | 14 | ||
| FT008740 | 666927 | 8922035 | Andesite | 0.0 | 147 | FT5160 | 667543 | 8921965 | Basalt | 0.0 | 266 | ||
| FT008749 | 666947 | 8921981 | Andesite | 0.0 | 17 | FT5162 | 667541 | 8921965 | Basalt | 0.0 | 130 | ||
| FT00880 | 666878 | 8922300 | Andesite | 0.0 | 110 | FT5166 | 667061 | 8923139 | Basalt | 0.0 | 79 | ||
| FT00952 | 666941 | 8922017 | Basalt | 0.0 | 71 | FT00857 | 666855 | 8922400 | Andesite | 0.0 | 16 | ||
| FT3000 | 667800 | 8924386 | Gossan | 0.0 | 234 | FT00858 | 666854 | 8922400 | Andesite | 0.0 | 69 |
28
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
Sample ID |
Easting WGS84Z55S |
Northing WGS84Z55S |
Lithology | Au (g/t) |
Cu **ppm ** |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FT00859 | 666853 | 8922400 | Andesite | 0.0 | 6 | FT5125 | 667985 | 8921898 | Basalt | 0.0 | 317 | ||
| FT00865 | 666847 | 8922400 | Andesite | 0.0 | 48 | FT5127 | 667987 | 8921898 | Basalt | 0.0 | 582 | ||
| FT00866 | 666846 | 8922400 | Andesite | 0.0 | 55 | FT5130 | 667990 | 8921898 | Basalt | 0.0 | 606 | ||
| FT00869 | 666867 | 8922300 | Andesite | 0.0 | 52 | FT5146 | 667557 | 8921965 | Basalt | 0.0 | 25 | ||
| FT00870 | 666868 | 8922300 | Andesite | 0.0 | 298 | FT5152 | 667551 | 8921965 | Basalt | 0.0 | 20 | ||
| FT00872 | 666870 | 8922300 | Andesite | 0.0 | 133 | FT5153 | 667550 | 8921965 | Basalt | 0.0 | 50 | ||
| FT00874 | 666872 | 8922300 | Andesite | 0.0 | 81 | FT5158 | 667545 | 8921965 | Basalt | 0.0 | 131 | ||
| FT00875 | 666873 | 8922300 | Andesite | 0.0 | 55 | FT5159 | 667544 | 8921965 | Basalt | 0.0 | 80 | ||
| FT00877 | 666875 | 8922300 | Andesite | 0.0 | 55 | FT5535 | 669354 | 8924171 | not logged | 0.0 | 47 | ||
| FT00878 | 666876 | 8922300 | Andesite | 0.0 | 25 | FT5145 | 667558 | 8921965 | Basalt | 0.0 | 49 | ||
| FT00879 | 666877 | 8922300 | Andesite | 0.0 | 81 | FT5155 | 667548 | 8921965 | Basalt | 0.0 | 74 | ||
| FT00881 | 666879 | 8922300 | Andesite | 0.0 | 111 | FT5156 | 667547 | 8921965 | Basalt | 0.0 | 34 | ||
| FT00883 | 666881 | 8922300 | Andesite | 0.0 | 137 | FT5157 | 667546 | 8921965 | Basalt | 0.0 | 54 | ||
| FT00885 | 666883 | 8922300 | Andesite | 0.0 | 43 | FT5161 | 667542 | 8921965 | Basalt | 0.0 | 312 | ||
| FT00889 | 666979 | 8922005 | Andesite | 0.0 | 61 | FT5197 | 667537 | 8921965 | Basalt | 0.0 | 108 | ||
| FT00941 | 666938 | 8922027 | Basalt | 0.0 | 102 | FT5198 | 667535 | 8921965 | Basalt | 0.0 | 163 | ||
| FT00942 | 666939 | 8922026 | Basalt | 0.0 | 124 | FT5199 | 667533 | 8921965 | Basalt | 0.0 | 175 | ||
| FT00943 | 666939 | 8922025 | Basalt | 0.0 | 37 | FT5200 | 667531 | 8921965 | Basalt | 0.0 | 304 | ||
| FT00946 | 666940 | 8922023 | Basalt | 0.0 | 56 | FT5201 | 667529 | 8921965 | Basalt | 0.0 | 188 | ||
| FT00956 | 666938 | 8921907 | Basalt | 0.0 | 95 | FT5202 | 666969 | 8921917 | Basalt | 0.0 | 32 | ||
| FT00957 | 666937 | 8921907 | Basalt | 0.0 | 134 | FT5314 | 667977 | 8921950 | Basalt | 0.0 | 403 | ||
| FT5128 | 667988 | 8921898 | Basalt | 0.0 | 817 | FT5319 | 667890 | 8924547 | Basalt | 0.0 | 455 | ||
| FT5129 | 667989 | 8921898 | Basalt | 0.0 | 530 | FT5525 | 667952 | 8924522 | Basalt | 0.0 | 72 | ||
| FT5154 | 667549 | 8921965 | Basalt | 0.0 | 49 | FT5551 | 667692 | 8925047 | PHN | 0.0 | 70 | ||
| FT5196 | 667539 | 8921965 | Basalt | 0.0 | 280 | FT5823 | 667306 | 8923650 | Basalt | 0.0 | 52 | ||
| FT5240 | 666584 | 8920709 | Andesite | 0.0 | 116 | FT5827 | 667373 | 8923645 | Basalt | 0.0 | 61 | ||
| FT5524 | 667942 | 8924526 | Andesite | 0.0 | 72 | FT5804 | 667378 | 8923668 | Basalt | -999.0 | 194.41 | ||
| FT008698 | 668513 | 8924287 | Andesite | 0.0 | 17 | FT5805 | 667376 | 8923669 | Basalt | -999.0 | 92.23 | ||
| FT008731 | 666933 | 8922028 | Andesite | 0.0 | 156 | FT5806 | 667374 | 8923670 | Basalt | -999.0 | 157.85 | ||
| FT008736 | 666930 | 8922031 | Andesite | 0.0 | 45 | FT5807 | 667373 | 8923672 | Basalt | -999.0 | 319.61 | ||
| FT008741 | 666927 | 8922036 | Andesite | 0.0 | 72 | FT5808 | 667372 | 8923673 | Basalt | -999.0 | 293.65 | ||
| FT008742 | 666926 | 8922037 | Andesite | 0.0 | 64 | FT5809 | 667370 | 8923675 | Basalt | -999.0 | 97.72 | ||
| FT008747 | 666948 | 8921980 | Andesite | 0.0 | 117 | FT5810 | 667369 | 8923676 | Basalt | -999.0 | 130.34 | ||
| FT008748 | 666947 | 8921980 | Andesite | 0.0 | 45 | FT5811 | 667368 | 8923678 | Basalt | -999.0 | 67.9 | ||
| FT5122 | 667982 | 8921898 | Basalt | 0.0 | 559 | FT5812 | 667367 | 8923679 | Basalt | -999.0 | 128.44 |
29
25 November 2022 ASX Announcement
ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Table 9:Drill hole IM19DD001 assay results. Imou Project From (m) To (m) Lithology Au (g/t) Cu (ppm) Mo (ppm) 4.7 6 Diorite 0.894 8445 13.3 6 8 Diorite 0.314 3652 15 8 10 Diorite 0.729 7835 17.7 10 12 Diorite 0.247 2430 6.1 12 14 Diorite 0.486 4078 4.3 14 16 Diorite 0.318 2446 7.3 16 18 Diorite 0.189 2212 3.7 18 20 Diorite 0.366 2334 21.8 20 24 Diorite 0.328 2462 9.2 24 26 Diorite 0.235 2416 3.2 26 28 Diorite 0.42 3415 11 28 30 Diorite 0.48 4275 43.8 30 32 Diorite 0.478 4967 6.2 32 34 Diorite 0.647 4713 6.9 34 36 Diorite 0.336 2716 7.5 36 38 Diorite 0.255 5153 13 38 40 Diorite 0.575 12435 8.1 40 42 Diorite 0.324 5613 4.7 42 44 Diorite 0.289 2596 14.9 44 46 Diorite 0.289 3344 6.5 46 48 Diorite 0.214 1628 2 48 50 Diorite 0.8 9075 8.5 50 52 Feldspar porphyry 0.158 2148 9.6 52 54 Hornfels 0.252 3358 31.4 54 56 Hornfels 0.218 2978 37.9 56 58 Hornfels 0.242 2834 29.7 58 60 Hornfels 0.233 3319 21.2 60 62 Diorite 0.244 2136 13.2 62 64 Diorite 0.165 1718 16.2 64 66 Diorite 0.104 1023 10 66 68 Diorite 0.118 1716 2.2 68 70 Diorite 0.123 1562 19.2 70 72 Diorite 0.12 1809 2 72 74 Diorite 0.342 3950 32 74 76 Diorite 0.196 2487 5.3 76 78 Diorite 0.197 2905 5.6 78 80 Diorite 0.156 1878 2 80 82 Diorite 0.139 1495 2.9 82 84 Diorite 0.236 3662 16.5 84 86 Diorite 0.113 1937 11.6 86 88 Diorite 0.161 2728 17.4 88 90 Diorite 0.089 1228 9.7 90 92 Diorite 0.143 1555 1.8 92 94 Diorite 0.202 1777 3.1 94 96 Diorite 0.168 2229 9.7 96 98 Diorite 0.643 7267 3 98 100 Diorite 0.205 2054 5.9 100 102 Diorite 0.343 3701 7.6 |
Table 9:Drill hole IM19DD001 assay results. Imou Project From (m) To (m) Lithology Au (g/t) Cu (ppm) Mo (ppm) 4.7 6 Diorite 0.894 8445 13.3 6 8 Diorite 0.314 3652 15 8 10 Diorite 0.729 7835 17.7 10 12 Diorite 0.247 2430 6.1 12 14 Diorite 0.486 4078 4.3 14 16 Diorite 0.318 2446 7.3 16 18 Diorite 0.189 2212 3.7 18 20 Diorite 0.366 2334 21.8 20 24 Diorite 0.328 2462 9.2 24 26 Diorite 0.235 2416 3.2 26 28 Diorite 0.42 3415 11 28 30 Diorite 0.48 4275 43.8 30 32 Diorite 0.478 4967 6.2 32 34 Diorite 0.647 4713 6.9 34 36 Diorite 0.336 2716 7.5 36 38 Diorite 0.255 5153 13 38 40 Diorite 0.575 12435 8.1 40 42 Diorite 0.324 5613 4.7 42 44 Diorite 0.289 2596 14.9 44 46 Diorite 0.289 3344 6.5 46 48 Diorite 0.214 1628 2 48 50 Diorite 0.8 9075 8.5 50 52 Feldspar porphyry 0.158 2148 9.6 52 54 Hornfels 0.252 3358 31.4 54 56 Hornfels 0.218 2978 37.9 56 58 Hornfels 0.242 2834 29.7 58 60 Hornfels 0.233 3319 21.2 60 62 Diorite 0.244 2136 13.2 62 64 Diorite 0.165 1718 16.2 64 66 Diorite 0.104 1023 10 66 68 Diorite 0.118 1716 2.2 68 70 Diorite 0.123 1562 19.2 70 72 Diorite 0.12 1809 2 72 74 Diorite 0.342 3950 32 74 76 Diorite 0.196 2487 5.3 76 78 Diorite 0.197 2905 5.6 78 80 Diorite 0.156 1878 2 80 82 Diorite 0.139 1495 2.9 82 84 Diorite 0.236 3662 16.5 84 86 Diorite 0.113 1937 11.6 86 88 Diorite 0.161 2728 17.4 88 90 Diorite 0.089 1228 9.7 90 92 Diorite 0.143 1555 1.8 92 94 Diorite 0.202 1777 3.1 94 96 Diorite 0.168 2229 9.7 96 98 Diorite 0.643 7267 3 98 100 Diorite 0.205 2054 5.9 100 102 Diorite 0.343 3701 7.6 |
Table 9:Drill hole IM19DD001 assay results. Imou Project From (m) To (m) Lithology Au (g/t) Cu (ppm) Mo (ppm) 4.7 6 Diorite 0.894 8445 13.3 6 8 Diorite 0.314 3652 15 8 10 Diorite 0.729 7835 17.7 10 12 Diorite 0.247 2430 6.1 12 14 Diorite 0.486 4078 4.3 14 16 Diorite 0.318 2446 7.3 16 18 Diorite 0.189 2212 3.7 18 20 Diorite 0.366 2334 21.8 20 24 Diorite 0.328 2462 9.2 24 26 Diorite 0.235 2416 3.2 26 28 Diorite 0.42 3415 11 28 30 Diorite 0.48 4275 43.8 30 32 Diorite 0.478 4967 6.2 32 34 Diorite 0.647 4713 6.9 34 36 Diorite 0.336 2716 7.5 36 38 Diorite 0.255 5153 13 38 40 Diorite 0.575 12435 8.1 40 42 Diorite 0.324 5613 4.7 42 44 Diorite 0.289 2596 14.9 44 46 Diorite 0.289 3344 6.5 46 48 Diorite 0.214 1628 2 48 50 Diorite 0.8 9075 8.5 50 52 Feldspar porphyry 0.158 2148 9.6 52 54 Hornfels 0.252 3358 31.4 54 56 Hornfels 0.218 2978 37.9 56 58 Hornfels 0.242 2834 29.7 58 60 Hornfels 0.233 3319 21.2 60 62 Diorite 0.244 2136 13.2 62 64 Diorite 0.165 1718 16.2 64 66 Diorite 0.104 1023 10 66 68 Diorite 0.118 1716 2.2 68 70 Diorite 0.123 1562 19.2 70 72 Diorite 0.12 1809 2 72 74 Diorite 0.342 3950 32 74 76 Diorite 0.196 2487 5.3 76 78 Diorite 0.197 2905 5.6 78 80 Diorite 0.156 1878 2 80 82 Diorite 0.139 1495 2.9 82 84 Diorite 0.236 3662 16.5 84 86 Diorite 0.113 1937 11.6 86 88 Diorite 0.161 2728 17.4 88 90 Diorite 0.089 1228 9.7 90 92 Diorite 0.143 1555 1.8 92 94 Diorite 0.202 1777 3.1 94 96 Diorite 0.168 2229 9.7 96 98 Diorite 0.643 7267 3 98 100 Diorite 0.205 2054 5.9 100 102 Diorite 0.343 3701 7.6 |
Table 9:Drill hole IM19DD001 assay results. Imou Project From (m) To (m) Lithology Au (g/t) Cu (ppm) Mo (ppm) 4.7 6 Diorite 0.894 8445 13.3 6 8 Diorite 0.314 3652 15 8 10 Diorite 0.729 7835 17.7 10 12 Diorite 0.247 2430 6.1 12 14 Diorite 0.486 4078 4.3 14 16 Diorite 0.318 2446 7.3 16 18 Diorite 0.189 2212 3.7 18 20 Diorite 0.366 2334 21.8 20 24 Diorite 0.328 2462 9.2 24 26 Diorite 0.235 2416 3.2 26 28 Diorite 0.42 3415 11 28 30 Diorite 0.48 4275 43.8 30 32 Diorite 0.478 4967 6.2 32 34 Diorite 0.647 4713 6.9 34 36 Diorite 0.336 2716 7.5 36 38 Diorite 0.255 5153 13 38 40 Diorite 0.575 12435 8.1 40 42 Diorite 0.324 5613 4.7 42 44 Diorite 0.289 2596 14.9 44 46 Diorite 0.289 3344 6.5 46 48 Diorite 0.214 1628 2 48 50 Diorite 0.8 9075 8.5 50 52 Feldspar porphyry 0.158 2148 9.6 52 54 Hornfels 0.252 3358 31.4 54 56 Hornfels 0.218 2978 37.9 56 58 Hornfels 0.242 2834 29.7 58 60 Hornfels 0.233 3319 21.2 60 62 Diorite 0.244 2136 13.2 62 64 Diorite 0.165 1718 16.2 64 66 Diorite 0.104 1023 10 66 68 Diorite 0.118 1716 2.2 68 70 Diorite 0.123 1562 19.2 70 72 Diorite 0.12 1809 2 72 74 Diorite 0.342 3950 32 74 76 Diorite 0.196 2487 5.3 76 78 Diorite 0.197 2905 5.6 78 80 Diorite 0.156 1878 2 80 82 Diorite 0.139 1495 2.9 82 84 Diorite 0.236 3662 16.5 84 86 Diorite 0.113 1937 11.6 86 88 Diorite 0.161 2728 17.4 88 90 Diorite 0.089 1228 9.7 90 92 Diorite 0.143 1555 1.8 92 94 Diorite 0.202 1777 3.1 94 96 Diorite 0.168 2229 9.7 96 98 Diorite 0.643 7267 3 98 100 Diorite 0.205 2054 5.9 100 102 Diorite 0.343 3701 7.6 |
Table 9:Drill hole IM19DD001 assay results. Imou Project From (m) To (m) Lithology Au (g/t) Cu (ppm) Mo (ppm) 4.7 6 Diorite 0.894 8445 13.3 6 8 Diorite 0.314 3652 15 8 10 Diorite 0.729 7835 17.7 10 12 Diorite 0.247 2430 6.1 12 14 Diorite 0.486 4078 4.3 14 16 Diorite 0.318 2446 7.3 16 18 Diorite 0.189 2212 3.7 18 20 Diorite 0.366 2334 21.8 20 24 Diorite 0.328 2462 9.2 24 26 Diorite 0.235 2416 3.2 26 28 Diorite 0.42 3415 11 28 30 Diorite 0.48 4275 43.8 30 32 Diorite 0.478 4967 6.2 32 34 Diorite 0.647 4713 6.9 34 36 Diorite 0.336 2716 7.5 36 38 Diorite 0.255 5153 13 38 40 Diorite 0.575 12435 8.1 40 42 Diorite 0.324 5613 4.7 42 44 Diorite 0.289 2596 14.9 44 46 Diorite 0.289 3344 6.5 46 48 Diorite 0.214 1628 2 48 50 Diorite 0.8 9075 8.5 50 52 Feldspar porphyry 0.158 2148 9.6 52 54 Hornfels 0.252 3358 31.4 54 56 Hornfels 0.218 2978 37.9 56 58 Hornfels 0.242 2834 29.7 58 60 Hornfels 0.233 3319 21.2 60 62 Diorite 0.244 2136 13.2 62 64 Diorite 0.165 1718 16.2 64 66 Diorite 0.104 1023 10 66 68 Diorite 0.118 1716 2.2 68 70 Diorite 0.123 1562 19.2 70 72 Diorite 0.12 1809 2 72 74 Diorite 0.342 3950 32 74 76 Diorite 0.196 2487 5.3 76 78 Diorite 0.197 2905 5.6 78 80 Diorite 0.156 1878 2 80 82 Diorite 0.139 1495 2.9 82 84 Diorite 0.236 3662 16.5 84 86 Diorite 0.113 1937 11.6 86 88 Diorite 0.161 2728 17.4 88 90 Diorite 0.089 1228 9.7 90 92 Diorite 0.143 1555 1.8 92 94 Diorite 0.202 1777 3.1 94 96 Diorite 0.168 2229 9.7 96 98 Diorite 0.643 7267 3 98 100 Diorite 0.205 2054 5.9 100 102 Diorite 0.343 3701 7.6 |
Table 9:Drill hole IM19DD001 assay results. Imou Project From (m) To (m) Lithology Au (g/t) Cu (ppm) Mo (ppm) 4.7 6 Diorite 0.894 8445 13.3 6 8 Diorite 0.314 3652 15 8 10 Diorite 0.729 7835 17.7 10 12 Diorite 0.247 2430 6.1 12 14 Diorite 0.486 4078 4.3 14 16 Diorite 0.318 2446 7.3 16 18 Diorite 0.189 2212 3.7 18 20 Diorite 0.366 2334 21.8 20 24 Diorite 0.328 2462 9.2 24 26 Diorite 0.235 2416 3.2 26 28 Diorite 0.42 3415 11 28 30 Diorite 0.48 4275 43.8 30 32 Diorite 0.478 4967 6.2 32 34 Diorite 0.647 4713 6.9 34 36 Diorite 0.336 2716 7.5 36 38 Diorite 0.255 5153 13 38 40 Diorite 0.575 12435 8.1 40 42 Diorite 0.324 5613 4.7 42 44 Diorite 0.289 2596 14.9 44 46 Diorite 0.289 3344 6.5 46 48 Diorite 0.214 1628 2 48 50 Diorite 0.8 9075 8.5 50 52 Feldspar porphyry 0.158 2148 9.6 52 54 Hornfels 0.252 3358 31.4 54 56 Hornfels 0.218 2978 37.9 56 58 Hornfels 0.242 2834 29.7 58 60 Hornfels 0.233 3319 21.2 60 62 Diorite 0.244 2136 13.2 62 64 Diorite 0.165 1718 16.2 64 66 Diorite 0.104 1023 10 66 68 Diorite 0.118 1716 2.2 68 70 Diorite 0.123 1562 19.2 70 72 Diorite 0.12 1809 2 72 74 Diorite 0.342 3950 32 74 76 Diorite 0.196 2487 5.3 76 78 Diorite 0.197 2905 5.6 78 80 Diorite 0.156 1878 2 80 82 Diorite 0.139 1495 2.9 82 84 Diorite 0.236 3662 16.5 84 86 Diorite 0.113 1937 11.6 86 88 Diorite 0.161 2728 17.4 88 90 Diorite 0.089 1228 9.7 90 92 Diorite 0.143 1555 1.8 92 94 Diorite 0.202 1777 3.1 94 96 Diorite 0.168 2229 9.7 96 98 Diorite 0.643 7267 3 98 100 Diorite 0.205 2054 5.9 100 102 Diorite 0.343 3701 7.6 |
From (m) |
To (m) | Lithology | Au (g/t) | Cu (ppm) |
Mo (ppm) |
|
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 102 | 104 | Diorite | 0.255 | 2805 | 1.8 | |||||||
| From (m) |
To (m) | Lithology | Au (g/t) | Cu (ppm) |
Mo (ppm) |
|||||||
| 104 | 106 | Diorite | 0.29 | 2505 | 5.1 | |||||||
| 4.7 | 6 | Diorite | 0.894 | 8445 | 13.3 | 106 | 108 | Diorite | 0.47 | 4149 | 5.9 | |
| 6 | 8 | Diorite | 0.314 | 3652 | 15 | 108 | 110 | Diorite | 0.174 | 2309 | 1.8 | |
| 8 | 10 | Diorite | 0.729 | 7835 | 17.7 | 110 | 112 | Diorite | 0.322 | 4457 | 4.6 | |
| 10 | 12 | Diorite | 0.247 | 2430 | 6.1 | 112 | 114 | Diorite | 0.507 | 4376 | 4 | |
| 12 | 14 | Diorite | 0.486 | 4078 | 4.3 | 114 | 116 | Diorite | 0.219 | 1653 | 1.6 | |
| 14 | 16 | Diorite | 0.318 | 2446 | 7.3 | 116 | 118 | Diorite | 0.255 | 1590 | 9.4 | |
| 16 | 18 | Diorite | 0.189 | 2212 | 3.7 | 118 | 120 | Diorite | 0.173 | 2036 | 9.1 | |
| 18 | 20 | Diorite | 0.366 | 2334 | 21.8 | 120 | 122 | Diorite | 0.405 | 3589 | 3.6 | |
| 20 | 24 | Diorite | 0.328 | 2462 | 9.2 | 122 | 124 | Diorite | 0.219 | 1660 | 7.2 | |
| 24 | 26 | Diorite | 0.235 | 2416 | 3.2 | 124 | 126 | Diorite | 0.147 | 1562 | 6.1 | |
| 26 | 28 | Diorite | 0.42 | 3415 | 11 | 126 | 128 | Diorite | 0.215 | 2130 | 2.2 | |
| 28 | 30 | Diorite | 0.48 | 4275 | 43.8 | 128 | 130 | Diorite | 0.119 | 1052 | 3.5 | |
| 30 | 32 | Diorite | 0.478 | 4967 | 6.2 | 130 | 132 | Diorite | 0.181 | 1424 | 16.9 | |
| 32 | 34 | Diorite | 0.647 | 4713 | 6.9 | 132 | 134 | Diorite | 0.322 | 2329 | 1.9 | |
| 34 | 36 | Diorite | 0.336 | 2716 | 7.5 | 134 | 136 | Diorite | 0.147 | 1245 | 2.3 | |
| 36 | 38 | Diorite | 0.255 | 5153 | 13 | 136 | 138 | Diorite | 0.122 | 1083 | 2.5 | |
| 38 | 40 | Diorite | 0.575 | 12435 | 8.1 | 138 | 140 | Diorite | 0.189 | 1538 | 2.2 | |
| 40 | 42 | Diorite | 0.324 | 5613 | 4.7 | 140 | 142 | Diorite | 0.422 | 3069 | 2.6 | |
| 42 | 44 | Diorite | 0.289 | 2596 | 14.9 | 142 | 144 | Diorite | 0.25 | 1374 | 2.8 | |
| 44 | 46 | Diorite | 0.289 | 3344 | 6.5 | 144 | 146 | Diorite | 0.123 | 1668 | 3.1 | |
| 46 | 48 | Diorite | 0.214 | 1628 | 2 | 146 | 148 | Diorite | 0.386 | 2712 | 17 | |
| 48 | 50 | Diorite | 0.8 | 9075 | 8.5 | 148 | 150 | Diorite | 0.273 | 2043 | 8.2 | |
| 50 | 52 | Feldspar porphyry | 0.158 | 2148 | 9.6 | 150 | 152 | Diorite | 0.277 | 2101 | 1.7 | |
| 52 | 54 | Hornfels | 0.252 | 3358 | 31.4 | 152 | 154 | Diorite | 0.127 | 2472 | 2.5 | |
| 54 | 56 | Hornfels | 0.218 | 2978 | 37.9 | 154 | 156 | Diorite | 0.122 | 1107 | 1 | |
| 56 | 58 | Hornfels | 0.242 | 2834 | 29.7 | 156 | 158 | Diorite | 0.318 | 2694 | 2.9 | |
| 58 | 60 | Hornfels | 0.233 | 3319 | 21.2 | 158 | 160 | Diorite | 0.235 | 2733 | 1.3 | |
| 60 | 62 | Diorite | 0.244 | 2136 | 13.2 | 160 | 162 | Diorite | 0.252 | 1822 | 1.8 | |
| 62 | 64 | Diorite | 0.165 | 1718 | 16.2 | 162 | 164 | Diorite | 0.219 | 1737 | 2.6 | |
| 64 | 66 | Diorite | 0.104 | 1023 | 10 | 164 | 166 | Diorite | 0.234 | 2617 | 4.8 | |
| 66 | 68 | Diorite | 0.118 | 1716 | 2.2 | 166 | 168 | Diorite | 0.156 | 1377 | 1 | |
| 68 | 70 | Diorite | 0.123 | 1562 | 19.2 | 168 | 170 | Diorite | 0.245 | 2478 | 2.8 | |
| 70 | 72 | Diorite | 0.12 | 1809 | 2 | 170 | 172 | Diorite | 0.33 | 3755 | 8.7 | |
| 72 | 74 | Diorite | 0.342 | 3950 | 32 | 172 | 174 | Diorite | 0.2 | 1767 | 2.5 | |
| 74 | 76 | Diorite | 0.196 | 2487 | 5.3 | 174 | 176 | Diorite | 0.249 | 2287 | 4.7 | |
| 76 | 78 | Diorite | 0.197 | 2905 | 5.6 | 176 | 178 | Diorite | 0.131 | 1441 | 7.4 | |
| 78 | 80 | Diorite | 0.156 | 1878 | 2 | 178 | 180 | Diorite | 0.125 | 1402 | 2.3 | |
| 80 | 82 | Diorite | 0.139 | 1495 | 2.9 | 180 | 182 | Diorite | 0.21 | 2211 | 8.2 | |
| 82 | 84 | Diorite | 0.236 | 3662 | 16.5 | 182 | 184 | Diorite | 0.16 | 1874 | 7.1 | |
| 84 | 86 | Diorite | 0.113 | 1937 | 11.6 | 184 | 186 | Diorite | 0.203 | 2309 | 4.5 | |
| 86 | 88 | Diorite | 0.161 | 2728 | 17.4 | 186 | 188 | Diorite | 0.516 | 5564 | 9.5 | |
| 88 | 90 | Diorite | 0.089 | 1228 | 9.7 | 188 | 190 | Hydrothermal Breccia |
4.69 | 37967 | 116 | |
| 90 | 92 | Diorite | 0.143 | 1555 | 1.8 | |||||||
| 190 | 192 | Hydrothermal Breccia |
5 | 41674 | 152 | |||||||
| 92 | 94 | Diorite | 0.202 | 1777 | 3.1 | |||||||
| 94 | 96 | Diorite | 0.168 | 2229 | 9.7 | 192 | 194 | Hydrothermal Breccia |
5.87 | 51865 | 558 | |
| 96 | 98 | Diorite | 0.643 | 7267 | 3 | |||||||
| 194 | 196 | Hydrothermal Breccia |
1.8 | 17758 | 26.8 | |||||||
| 98 | 100 | Diorite | 0.205 | 2054 | 5.9 | |||||||
| 100 | 102 | Diorite | 0.343 | 3701 | 7.6 | 196 | 198 | Diorite | 0.796 | 8403 | 23 |
30
25 November 2022 ASX Announcement
==> picture [103 x 68] intentionally omitted <==
ASX: LCL
| From (m) |
To (m) | Lithology | Au (g/t) | Cu (ppm) |
Mo (ppm) |
From (m) |
To (m) | Lithology | Au (g/t) | Cu (ppm) |
Mo (ppm) |
|
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 198 | 200 | Diorite | 0.818 | 6745 | 8.3 | 298 | 300 | Feldspar porphyry | 0.165 | 1166 | 1.8 | |
| 200 | 202 | Diorite | 0.391 | 3998 | 10.3 | 300 | 302 | Feldspar porphyry | 0.327 | 3500 | 17 | |
| 202 | 204 | Diorite | 0.419 | 3926 | 3.1 | 302 | 304 | Feldspar porphyry | 0.268 | 3419 | 60.9 | |
| 204 | 206 | Diorite | 0.524 | 5576 | 19.8 | 304 | 306 | Feldspar porphyry | 0.165 | 1975 | 14.6 | |
| 206 | 208 | Diorite | 0.258 | 2801 | 8.3 | 306 | 308 | Feldspar porphyry | 0.155 | 1683 | 17.6 | |
| 208 | 210 | Diorite | 0.304 | 3040 | 10 | 308 | 310 | Feldspar porphyry | 0.108 | 1118 | 8.4 | |
| 210 | 212 | Diorite | 0.335 | 3350 | 10 | 310 | 312 | Feldspar porphyry | 0.061 | 889 | 8.5 | |
| 212 | 214 | Diorite | 0.285 | 2693 | 5.4 | 312 | 314 | Feldspar porphyry | 0.067 | 810 | 3 | |
| 214 | 216 | Diorite | 0.214 | 2305 | 13.7 | 314 | 316 | Feldspar porphyry | 0.116 | 1817 | 11.2 | |
| 216 218 220 |
218 220 222 |
Diorite Diorite Diorite |
0.391 0.187 0.617 |
3825 2359 4446 |
31.8 30.4 125 |
316 318 |
318 320 |
Hydrothermal Breccia Hydrothermal Breccia |
0.076 0.04 |
980 875 |
7.3 28.6 |
|
| 222 224 |
224 226 |
Diorite Diorite |
0.314 0.193 |
3569 1946 |
31.3 12.7 |
320 | 322 | Hydrothermal Breccia |
0.036 | 497 | 21.3 | |
| 226 | 228 | Diorite | 0.137 | 1410 | 1.7 | 322 | 324 | Hydrothermal Breccia |
0.068 | 1264 | 19 | |
| 228 230 |
230 232 |
Diorite Diorite |
0.127 0.171 |
1135 1324 |
1.5 23.1 |
324 | 326 | Hydrothermal Breccia |
0.051 | 889 | 2.6 | |
| 232 | 234 | Diorite | 0.189 | 1449 | 2.4 | 326 | 328 | Hydrothermal Breccia |
0.103 | 457 | 7.7 | |
| 234 236 |
236 238 |
Diorite Diorite |
0.114 0.136 |
1364 1469 |
31.3 5.1 |
328 | 330 | Hydrothermal Breccia |
0.062 | 591 | 8.9 | |
| 330 | 332 | Hornfels | 0.043 | 1299 | 46 | |||||||
| 238 | 240 | Diorite | 0.222 | 1995 | 6.8 | |||||||
| 332 | 334 | Hornfels | 0.057 | 857 | 31.2 | |||||||
| 240 | 242 | Diorite | 0.237 | 2633 | 7.7 | |||||||
| 334 | 336 | Hornfels | 0.037 | 659 | 42.6 | |||||||
| 242 | 244 | Diorite | 0.324 | 3914 | 95.2 | |||||||
| 336 | 338 | Hornfels | 0.059 | 988 | 26.3 | |||||||
| 244 | 246 | Diorite | 0.289 | 2223 | 19.5 | |||||||
| 338 | 340 | Hornfels | 0.062 | 644 | 25.2 | |||||||
| 246 | 248 | Diorite | 0.251 | 3324 | 13.6 | |||||||
| 340 | 342 | Hornfels | 0.084 | 600 | 73 | |||||||
| 248 | 250 | Diorite | 0.158 | 2114 | 4.5 | |||||||
| 342 | 344 | Hornfels | 0.065 | 1017 | 9.1 | |||||||
| 250 | 252 | Diorite | 0.191 | 2509 | 10.3 | |||||||
| 344 | 346 | Hornfels | 0.272 | 4236 | 11.7 | |||||||
| 252 | 254 | Diorite | 0.176 | 2058 | 4.5 | |||||||
| 346 | 348 | Hornfels | 0.124 | 974 | 8.4 | |||||||
| 254 | 256 | Diorite | 0.193 | 2405 | 3.6 | |||||||
| 348 | 350 | Hornfels | 0.043 | 801 | 18.1 | |||||||
| 256 | 258 | Diorite | 0.168 | 1956 | 8.4 | |||||||
| 350 | 352 | Hornfels | 0.03 | 677 | 23.9 | |||||||
| 258 | 260 | Diorite | 0.186 | 2043 | 6.9 | |||||||
| 260 | 262 | Feldspar porphyry | 0.117 | 1645 | 7 | 352 | 354 | Hornfels | 0.02 | 511 | 35.9 | |
| 262 | 264 | Feldspar porphyry | 0.116 | 1246 | 3 | 354 | 356 | Hornfels | 0.026 | 644 | 18.8 | |
| 264 | 266 | Feldspar porphyry | 0.505 | 4995 | 14.1 | 356 | 358 | Hornfels | 0.018 | 730 | 27.4 | |
| 266 | 268 | Feldspar porphyry | 0.165 | 2252 | 5.6 | 358 | 360 | Hornfels | 0.198 | 1178 | 23.5 | |
| 268 | 270 | Feldspar porphyry | 0.199 | 2222 | 9.1 | 360 | 362 | Hornfels | 0.12 | 1711 | 24.2 | |
| 362 | 364 | Hornfels | 0.027 | 697 | 10.3 | |||||||
| 270 | 272 | Feldspar porphyry | 0.154 | 1811 | 2.5 | |||||||
| 272 | 274 | Feldspar porphyry | 0.266 | 3040 | 8.3 | 364 | 366 | Hornfels | 0.029 | 849 | 12.3 | |
| 274 | 276 | Feldspar porphyry | 0.148 | 1807 | 6.5 | 366 | 368 | Hornfels | 0.055 | 1114 | 20.8 | |
| 276 | 278 | Feldspar porphyry | 0.307 | 3205 | 11.4 | 368 | 370 | Hornfels | 0.027 | 952 | 40.6 | |
| 278 | 280 | Feldspar porphyry | 0.254 | 2941 | 7.4 | 370 | 372 | Hornfels | 0.048 | 1216 | 21.9 | |
| 280 | 282 | Feldspar porphyry | 0.214 | 3771 | 17.5 | 372 | 374 | Hornfels | 0.028 | 1056 | 12.2 | |
| 282 | 284 | Feldspar porphyry | 0.148 | 5573 | 27 | 374 | 376 | Hornfels | 0.085 | 1721 | 27.9 | |
| 284 | 286 | Feldspar porphyry | 0.15 | 2139 | 27.6 | 376 | 378 | Hornfels | 0.072 | 1594 | 24 | |
| 286 | 288 | Feldspar porphyry | 0.285 | 3335 | 2.5 | 378 | 380 | Hornfels | 0.037 | 1426 | 24.3 | |
| 288 | 290 | Feldspar porphyry | 0.186 | 2151 | 2.8 | 380 | 382 | Hornfels | 0.028 | 1462 | 18.5 | |
| 290 | 292 | Feldspar porphyry | 0.166 | 1373 | 6 | 382 | 384 | Hornfels | 0.132 | 2313 | 39.4 | |
| 292 | 294 | Feldspar porphyry | 0.102 | 1042 | 2.3 | 384 | 386 | Hornfels | 0.188 | 3973 | 10.6 | |
| 386 | 388 | Hornfels | 0.071 | 1616 | 17.4 | |||||||
| 294 | 296 | Feldspar porphyry | 0.11 | 1344 | 5.6 | |||||||
| 296 | 298 | Feldspar porphyry | 0.125 | 1562 | 5.7 | 388 | 390 | Hornfels | 0.106 | 2104 | 8.2 | |
| 390 | 392 | Feldspar porphyry | 0.136 | 4143 | 39.4 |
31
25 November 2022 ASX Announcement
==> picture [103 x 68] intentionally omitted <==
ASX: LCL
| From (m) |
To (m) | Lithology | Au (g/t) | Cu (ppm) |
Mo (ppm) |
From (m) |
To (m) | Lithology | Au (g/t) | Cu (ppm) |
Mo (ppm) |
||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 392 | 394 | Feldspar porphyry | 0.188 | 3948 | 24.6 | 492 | 494 | Diorite | 0.088 | 905 | 23.6 | ||
| 394 | 396 | Feldspar porphyry | 0.377 | 6745 | 41.7 | 494 | 496 | Diorite | 0.039 | 645 | 12.2 | ||
| 396 | 398 | Hornfels | 0.276 | 6116 | 87.1 | 496 | 498 | Diorite | 0.044 | 910 | 13.6 | ||
| 398 | 400 | Feldspar porphyry | 0.093 | 3373 | 13.5 | 498 | 500 | Hornfels | 0.043 | 722 | 20.4 | ||
| 400 | 402 | Feldspar porphyry | 0.179 | 2713 | 7.5 | 500 | 502 | Diorite | 0.078 | 417 | 17 | ||
| 402 | 404 | Feldspar porphyry | 0.121 | 2034 | 7.2 | 502 | 504 | Diorite | 0.043 | 540 | 22.3 | ||
| 404 | 406 | Feldspar porphyry | 0.027 | 975 | 3.6 | 504 | 506 | Diorite | 0.118 | 1191 | 45 | ||
| 406 | 408 | Feldspar porphyry | 0.022 | 617 | 3.3 | 506 | 508 | Diorite | 0.067 | 591 | 122 | ||
| 408 | 410 | Feldspar porphyry | 0.028 | 810 | 1 | 508 | 510 | Diorite | 0.079 | 297 | 25.8 | ||
| 410 | 412 | Feldspar porphyry | 0.035 | 1150 | 2.3 | 510 | 512 | Diorite | 0.049 | 685 | 17.5 | ||
| 412 | 414 | Hornfels | 0.019 | 773 | 3 | 512 | 514 | Diorite | 0.024 | 332 | 35.9 | ||
| 414 | 416 | Hornfels | 0.046 | 977 | 2.4 | 514 | 516 | Diorite | 0.018 | 296 | 13.9 | ||
| 416 | 418 | Hornfels | 0.065 | 1154 | 2.1 | 516 | 518 | Diorite | 0.034 | 375 | 55.9 | ||
| 418 | 420 | Hornfels | 0.063 | 1636 | 13.3 | 518 | 520 | Diorite | 0.031 | 341 | 51.9 | ||
| 420 | 422 | Hornfels | 0.031 | 901 | 8.1 | 520 | 522 | Diorite | 0.039 | 683 | 109 | ||
| 422 | 424 | Hornfels | 0.05 | 1213 | 13.5 | 522 | 524 | Diorite | 0.032 | 397 | 29.2 | ||
| 424 | 426 | Hornfels | 0.024 | 827 | 9.6 | 524 | 526 | Diorite | 0.034 | 626 | 35 | ||
| 426 | 428 | Hornfels | 0.044 | 876 | 12.6 | 526 | 528 | Diorite | 0.046 | 548 | 48.5 | ||
| 428 | 430 | Hornfels | 1.03 | 9680 | 12.3 | 528 | 530 | Diorite | 0.039 | 417 | 92.5 | ||
| 430 | 432 | Hornfels | 0.404 | 8772 | 9.5 | 530 | 532 | Feldspar porphyry | 0.023 | 405 | 27.6 | ||
| 432 | 434 | Hornfels | 0.039 | 817 | 16.4 | 532 | 534 | Feldspar porphyry | 0.067 | 1501 | 35.3 | ||
| 434 | 436 | Hornfels | 0.036 | 674 | 10 | 534 | 536 | Feldspar porphyry | 0.048 | 1183 | 98.5 | ||
| 436 | 438 | Hornfels | 0.044 | 1282 | 16.4 | 536 | 538 | Feldspar porphyry | 0.035 | 839 | 54.2 | ||
| 438 | 440 | Hornfels | 0.023 | 658 | 9.4 | 538 | 540 | Diorite | 0.04 | 795 | 48.8 | ||
| 440 | 442 | Hornfels | 0.25 | 631 | 27 | 540 | 542 | Diorite | 0.051 | 1048 | 23.2 | ||
| 442 | 444 | Hornfels | 0.027 | 838 | 18.4 | 542 | 544 | Diorite | 0.052 | 1187 | 22 | ||
| 444 | 446 | Hornfels | 0.023 | 496 | 35.5 | 544 | 546 | Diorite | 0.091 | 1428 | 27.2 | ||
| 446 | 448 | Hornfels | 0.053 | 1178 | 12.8 | 546 | 548 | Diorite | 0.041 | 850 | 14.8 | ||
| 448 | 450 | Hornfels | 0.034 | 827 | 54.2 | 548 | 550 | Diorite | 0.023 | 405 | 29.2 | ||
| 450 | 452 | Hornfels | 0.03 | 818 | 26.1 | 550 | 552 | Diorite | 0.034 | 570 | 27.8 | ||
| 452 | 454 | Hornfels | 0.037 | 830 | 56.5 | 552 | 554 | Diorite | 0.044 | 662 | 25.4 | ||
| 454 | 456 | Hornfels | 0.314 | 1941 | 11.3 | 554 | 556 | Diorite | 0.022 | 411 | 28.6 | ||
| 456 | 458 | Hornfels | 0.319 | 1750 | 25.8 | 556 | 558 | Diorite | 0.011 | 253 | 24.1 | ||
| 458 | 460 | Hornfels | 0.031 | 887 | 86 | 558 | 560 | Diorite | 0.032 | 771 | 50.4 | ||
| 460 | 462 | Hornfels | 0.026 | 1032 | 26 | 560 | 562 | Diorite | 0.028 | 512 | 48.9 | ||
| 462 | 464 | Hornfels | 0.047 | 1144 | 31.9 | 562 | 564 | Diorite | 0.023 | 390 | 26.2 | ||
| 464 | 466 | Hornfels | 0.027 | 554 | 24 | 564 | 566 | Diorite | 0.012 | 424 | 28.7 | ||
| 466 | 468 | Hornfels | 0.105 | 2105 | 127 | 566 | 568 | Diorite | 0.036 | 706 | 12.2 | ||
| 468 | 470 | Hornfels | 0.034 | 726 | 60.2 | 568 | 570 | Diorite | 0.023 | 605 | 27 | ||
| 470 | 472 | Hornfels | 0.022 | 490 | 29 | 570 | 572 | Diorite | 0.028 | 852 | 42.3 | ||
| 472 | 474 | Hornfels | 0.049 | 611 | 36.2 | 572 | 574 | Diorite | 0.018 | 607 | 169 | ||
| 474 | 476 | Hornfels | 0.04 | 545 | 17.5 | 574 | 576 | Diorite | 0.012 | 438 | 27.2 | ||
| 476 | 478 | Hornfels | 0.198 | 1832 | 54.3 | 576 | 578 | Diorite | 0.007 | 260 | 57 | ||
| 478 | 480 | Hornfels | 0.093 | 1780 | 22.1 | 578 | 580 | Diorite | 0.013 | 355 | 43.6 | ||
| 480 | 482 | Diorite | 0.048 | 844 | 15.5 | 580 | 582 | Diorite | 0.007 | 359 | 107 | ||
| 482 | 484 | Diorite | 0.081 | 1376 | 34.5 | 582 | 584 | Diorite | 0.021 | 709 | 25.8 | ||
| 484 | 486 | Diorite | 0.151 | 2678 | 36.8 | 584 | 586 | Diorite | 0.011 | 373 | 16.9 | ||
| 486 | 488 | Diorite | 0.097 | 1746 | 15.4 | 586 | 588 | Diorite | 0.02 | 592 | 21.1 | ||
| 488 | 490 | Diorite | 0.093 | 1780 | 33.8 | 588 | 590 | Diorite | 0.014 | 588 | 34.2 | ||
| 490 | 492 | Diorite | 0.075 | 1438 | 17.6 | 590 | 592 | Diorite | 0.014 | 555 | 94.5 |
32
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| From (m) |
To (m) | To (m) | To (m) | Lithology | Lithology | Lithology | Lithology | Au (g/t) Cu (ppm) |
Au (g/t) Cu (ppm) |
Au (g/t) Cu (ppm) |
Au (g/t) Cu (ppm) |
Mo (ppm) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 592 | 594 | Diorite | 0.006 | 429 |
42.6 | KSDD001 | 36 | 37 | Phyllite | 0.05 | ||||||||||
| 594 | 596 | Diorite | 0.009 | 364 |
17.3 | KSDD001 | 37 | 38 | Phyllite | 0.04 | ||||||||||
| 596 | 598 | Diorite | 0.017 | 495 |
47.4 | |||||||||||||||
| 598 | 599.6 (EOH) |
Diorite | 0.022 | 518 |
80.2 | KSDD001 KSDD001 |
38 39 |
39 40 |
Phyllite Phyllite |
0.03 0.09 |
||||||||||
| KSDD001 | 40 | 41 | Phyllite | 0.11 | ||||||||||||||||
| KSDD001 | 41 | 42 | Phyllite | 0.11 | ||||||||||||||||
| **Table 10: ** | Kusi | Diamond | Drilling, -999 = not assayed | KSDD001 | 42 | 43 | Phyllite | 0.04 | ||||||||||||
| KSDD001 | 43 | 44 | Phyllite | 0.13 | ||||||||||||||||
| From | To | Au | KSDD001 | 44 | 45 | Phyllite | 0.16 | |||||||||||||
| Hole_ID | (m) | (m) | Lithology | (g/t) | KSDD001 | 45 | 46 | Phyllite | 0.28 | |||||||||||
| KSDD001 | 0 | 2.5 | Colluvium | 0.01 | KSDD001 | 46 | 47 | Phyllite | 0.13 | |||||||||||
| KSDD001 | 2.5 | 3.5 | Colluvium | 0.01 | KSDD001 | 47 | 48 | Phyllite | 0.04 | |||||||||||
| KSDD001 | 3.5 | 4.2 | Phyllite | 0.01 | KSDD001 | 48 | 49 | Phyllite | 0.09 | |||||||||||
| KSDD001 | 4.2 | 5 | Fault | 0.03 | KSDD001 | 49 | 50 | Phyllite | 0.16 | |||||||||||
| KSDD001 | 5 | 6 | Fault | 0.09 | KSDD001 | 50 | 51 | Phyllite | 0.08 | |||||||||||
| KSDD001 | 6 | 7.1 | Fault | 0.01 | KSDD001 | 51 | 52 | Fault | 0.11 | |||||||||||
| KSDD001 | 7.1 | 7.9 | Fault | -999 | KSDD001 | 52 | 54 | Fault | 0.21 | |||||||||||
| KSDD001 | 7.9 | 9 | Fault | 0.04 | KSDD001 | 54 | 55 | Phyllite | 0.13 | |||||||||||
| KSDD001 | 9 | 10 | Fault | 0.04 | KSDD001 | 55 | 56 | Phyllite | 0.61 | |||||||||||
| KSDD001 | 10 | 12 | Phyllite | 0.01 | KSDD001 | 56 | 57 | Phyllite | 0.92 | |||||||||||
| KSDD001 | 12 | 12 | Phyllite | 0.13 | KSDD001 | 57 | 58 | Phyllite | 0.16 | |||||||||||
| KSDD001 | 12 | 14 | Phyllite | -999 | KSDD001 | 58 | 59 | Phyllite | 0.14 | |||||||||||
| KSDD001 | 14 | 14 | Phyllite | 0.57 | KSDD001 | 59 | 60 | Phyllite | 0.15 | |||||||||||
| KSDD001 | 14 | 15 | Phyllite | -999 | KSDD001 | 60 | 61 | Phyllite | 0.24 | |||||||||||
| KSDD001 | 15 | 16 | Phyllite | 1.37 | KSDD001 | 61 | 62 | Phyllite | 0.37 | |||||||||||
| KSDD001 | 16 | 17 | Phyllite | 6.29 | KSDD001 | 62 | 63 | Phyllite | 0.24 | |||||||||||
| KSDD001 | 17 | 18 | Phyllite | 3.06 | KSDD001 | 63 | 64 | Phyllite | 0.08 | |||||||||||
| KSDD001 | 18 | 19 | Phyllite | 0.93 | KSDD001 | 64 | 65 | Phyllite | 0.09 | |||||||||||
| KSDD001 | 19 | 20 | Phyllite | 1.85 | KSDD001 | 65 | 66 | Phyllite | 0.06 | |||||||||||
| KSDD001 | 20 | 21 | Phyllite | 0.33 | KSDD001 | 66 | 67 | Phyllite | 0.1 | |||||||||||
| KSDD001 | 21 | 22 | Phyllite | 0.19 | KSDD001 | 67 | 68 | Phyllite | 0.25 | |||||||||||
| KSDD001 | 22 | 23 | Phyllite | 0.14 | KSDD001 | 68 | 69 | Phyllite | 0.18 | |||||||||||
| KSDD001 | 23 | 24 | Phyllite | 0.05 | KSDD001 | 69 | 70 | Phyllite | 0.22 | |||||||||||
| KSDD001 | 24 | 25 | Phyllite | 0.09 | KSDD001 | 70 | 71 | Phyllite | 0.58 | |||||||||||
| KSDD001 | 25 | 27 | Phyllite | -999 | KSDD001 | 71 | 72 | Phyllite | 0.2 | |||||||||||
| KSDD001 | 27 | 27 | Phyllite | 0.2 | KSDD001 | 72 | 73 | Phyllite | 0.15 | |||||||||||
| KSDD001 | 27 | 28 | Phyllite | 0.23 | KSDD001 | 73 | 74 | Phyllite | 0.41 | |||||||||||
| KSDD001 | 28 | 29 | Phyllite | 0.06 | KSDD001 | 74 | 75 | Phyllite | 0.41 | |||||||||||
| KSDD001 | 29 | 30 | Phyllite | 0.16 | KSDD001 | 75 | 76 | Phyllite | 0.77 | |||||||||||
| KSDD001 | 30 | 31 | Phyllite | 0.08 | KSDD001 | 76 | 77 | Phyllite | 0.24 | |||||||||||
| KSDD001 | 31 | 32 | Phyllite | 0.12 | KSDD001 | 77 | 78 | Phyllite | 1.12 | |||||||||||
| KSDD001 | 32 | 33 | Phyllite | 0.04 | KSDD001 | 78 | 79 | Phyllite | 0.26 | |||||||||||
| KSDD001 | 33 | 34 | Phyllite | 0.06 | KSDD001 | 79 | 80 | Phyllite | 0.19 | |||||||||||
| KSDD001 | 34 | 35 | Phyllite | 0.18 | KSDD001 | 80 | 81 | Phyllite | 0.13 | |||||||||||
| KSDD001 | 35 | 36 | Phyllite | 0.43 | KSDD001 | 81 | 82 | Phyllite | 0.2 |
33
25 November 2022 ASX Announcement
ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD001 | 82 | 83 | Phyllite | 0.13 | KSDD001 | 127 | 128 | Phyllite | 0.04 | |
| KSDD001 | 83 | 84 | Phyllite | 0.08 | KSDD001 | 128 | 129 | Phyllite | 0.02 | |
| KSDD001 | 84 | 85 | Phyllite | 0.2 | KSDD001 | 129 | 130 | Phyllite | 0.02 | |
| KSDD001 | 85 | 86 | Phyllite | 0.12 | KSDD001 | 130 | 131 | Phyllite | 0.02 | |
| KSDD001 | 86 | 87 | Phyllite | 0.11 | KSDD001 | 131 | 132 | Phyllite | 0.05 | |
| KSDD001 | 87 | 88 | Phyllite | 2.72 | KSDD001 | 132 | 133 | Phyllite | 0.03 | |
| KSDD001 | 88 | 89 | Phyllite | 0.23 | KSDD001 | 133 | 134 | Skarn | 0.16 | |
| KSDD001 | 89 | 90 | Phyllite | 0.15 | KSDD001 | 134 | 135 | Skarn | 0.09 | |
| KSDD001 | 90 | 91 | Phyllite | 0.12 | KSDD001 | 135 | 136 | Skarn | 0.05 | |
| KSDD001 | 91 | 92 | Phyllite | 0.27 | KSDD001 | 136 | 137 | Skarn | 0.01 | |
| KSDD001 | 92 | 93 | Phyllite | 0.18 | KSDD001 | 137 | 138 | Skarn | 0.05 | |
| KSDD001 | 93 | 94 | Phyllite | 0.46 | KSDD001 | 138 | 139 | Skarn | 0.04 | |
| KSDD001 | 94 | 95 | Phyllite | 0.15 | KSDD001 | 139 | 140 | Skarn | -999 | |
| KSDD001 | 95 | 96 | Phyllite | 0.1 | KSDD001 | 140 | 141 | Skarn | 0.22 | |
| KSDD001 | 96 | 97 | Phyllite | 0.08 | KSDD001 | 141 | 141 | Skarn | -999 | |
| KSDD001 | 97 | 98 | Phyllite | 0.06 | KSDD001 | 141 | 142 | Skarn | 0.03 | |
| KSDD001 | 98 | 99 | Phyllite | 0.14 | KSDD001 | 142 | 143 | Skarn | -999 | |
| KSDD001 | 99 | 100 | Fault | 0.09 | KSDD001 | 143 | 144 | Skarn | 0.01 | |
| KSDD001 | 100 | 101 | Fault | 0.27 | KSDD001 | 144 | 145 | Skarn | -999 | |
| KSDD001 | 101 | 102 | Phyllite | 0.08 | KSDD001 | 145 | 147 | Skarn | -999 | |
| KSDD001 | 102 | 103 | Phyllite | 0.05 | KSDD001 | 147 | 147 | Skarn | 0.08 | |
| KSDD001 | 103 | 104 | Phyllite | 0.04 | KSDD001 | 147 | 151 | Skarn | -999 | |
| KSDD001 | 104 | 105 | Phyllite | 0.04 | KSDD001 | 151 | 151 | Skarn | 0.03 | |
| KSDD001 | 105 | 106 | Phyllite | 0.15 | KSDD001 | 151 | 152 | Skarn | -999 | |
| KSDD001 | 106 | 107 | Phyllite | 0.15 | KSDD001 | 152 | 153 | Skarn | 0.01 | |
| KSDD001 | 107 | 108 | Phyllite | 0.02 | KSDD001 | 153 | 154 | Skarn | -999 | |
| KSDD001 | 108 | 109 | Phyllite | 0.02 | KSDD001 | 154 | 155 | Skarn | 0.04 | |
| KSDD001 | 109 | 110 | Phyllite | 0.05 | KSDD001 | 155 | 156 | Skarn | -999 | |
| KSDD001 | 110 | 111 | Phyllite | 1.02 | KSDD001 | 156 | 156 | Skarn | 0.06 | |
| KSDD001 | 111 | 112 | Phyllite | 0.04 | KSDD001 | 156 | 158 | Skarn | 0.08 | |
| KSDD001 | 112 | 113 | Phyllite | 0.02 | KSDD001 | 158 | 159 | Skarn | -999 | |
| KSDD001 | 113 | 114 | Phyllite | 0.05 | KSDD001 | 159 | 160 | Skarn | 0.25 | |
| KSDD001 | 114 | 115 | Phyllite | 0.02 | KSDD001 | 160 | 161 | Skarn | 0.39 | |
| KSDD001 | 115 | 116 | Phyllite | 0.03 | KSDD001 | 161 | 162 | Skarn | 0.71 | |
| KSDD001 | 116 | 117 | Phyllite | 0.04 | KSDD001 | 162 | 163 | Skarn | 0.09 | |
| KSDD001 | 117 | 118 | Phyllite | 0.03 | KSDD001 | 163 | 164 | Skarn | 0.01 | |
| KSDD001 | 118 | 119 | Phyllite | 0.01 | KSDD001 | 164 | 165 | Skarn | 0.06 | |
| KSDD001 | 119 | 120 | Phyllite | 0.01 | KSDD001 | 165 | 166 | Skarn | 0.1 | |
| KSDD001 | 120 | 121 | Phyllite | 0.01 | KSDD001 | 166 | 167 | Skarn | -999 | |
| KSDD001 | 121 | 122 | Phyllite | 0.01 | KSDD001 | 167 | 168 | Skarn | -999 | |
| KSDD001 | 122 | 123 | Phyllite | 0.05 | KSDD001 | 168 | 169 | Skarn | -999 | |
| KSDD001 | 123 | 124 | Phyllite | 0.03 | KSDD001 | 169 | 170 | Skarn | -999 | |
| KSDD001 | 124 | 125 | Phyllite | 0.04 | KSDD001 | 170 | 171 | Skarn | -999 | |
| KSDD001 | 125 | 126 | Phyllite | 0.02 | KSDD001 | 171 | 172 | Skarn | -999 | |
| KSDD001 | 126 | 127 | Phyllite | 0.03 | KSDD001 | 172 | 172 | Skarn | -999 |
34
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD001 | 172 | 173 | Skarn | -999 | KSDD001 | 217 | 218 | Skarn | 0.08 | |
| KSDD001 | 173 | 174 | Skarn | -999 | KSDD001 | 218 | 219 | Skarn | 0.02 | |
| KSDD001 | 174 | 176 | Skarn | 0.01 | KSDD001 | 219 | 220 | Skarn | 0.02 | |
| KSDD001 | 176 | 177 | Skarn | 0.01 | KSDD001 | 220 | 221 | Skarn | 0.04 | |
| KSDD001 | 177 | 178 | Skarn | 0.01 | KSDD001 | 221 | 222 | Skarn | 0.02 | |
| KSDD001 | 178 | 179 | Skarn | -999 | KSDD001 | 222 | 223 | Skarn | 0.14 | |
| KSDD001 | 179 | 180 | Skarn | 0.03 | KSDD001 | 223 | 224 | Skarn | 0.22 | |
| KSDD001 | 180 | 181 | Skarn | 0.01 | KSDD001 | 224 | 225 | Skarn | 0.24 | |
| KSDD001 | 181 | 182 | Skarn | -999 | KSDD001 | 225 | 226 | Skarn | 0.26 | |
| KSDD001 | 182 | 183 | Skarn | -999 | KSDD001 | 226 | 227 | Skarn | 0.3 | |
| KSDD001 | 183 | 184 | Skarn | -999 | KSDD001 | 227 | 228 | Skarn | 0.23 | |
| KSDD001 | 184 | 185 | Skarn | -999 | KSDD001 | 228 | 229 | Skarn | 0.4 | |
| KSDD001 | 185 | 186 | Skarn | 0.03 | KSDD001 | 229 | 230 | Skarn | 0.4 | |
| KSDD001 | 186 | 187 | Skarn | 0.02 | KSDD001 | 230 | 231 | Skarn | 0.04 | |
| KSDD001 | 187 | 188 | Skarn | 0.03 | KSDD001 | 231 | 232 | Skarn | 0.04 | |
| KSDD001 | 188 | 189 | Skarn | 0.02 | KSDD001 | 232 | 233 | Skarn | 0.03 | |
| KSDD001 | 189 | 190 | Skarn | 0.02 | KSDD001 | 233 | 234 | Phyllite | 0.04 | |
| KSDD001 | 190 | 191 | Skarn | 0.03 | KSDD001 | 234 | 235 | Phyllite | 0.03 | |
| KSDD001 | 191 | 192 | Skarn | 0.02 | KSDD001 | 235 | 236 | Phyllite | 0.05 | |
| KSDD001 | 192 | 193 | Skarn | 0.02 | KSDD001 | 236 | 237 | Phyllite | 0.02 | |
| KSDD001 | 193 | 194 | Skarn | 0.02 | KSDD001 | 237 | 238 | Phyllite | 0.02 | |
| KSDD001 | 194 | 195 | Skarn | 0.01 | KSDD001 | 238 | 239 | Phyllite | 0.03 | |
| KSDD001 | 195 | 196 | Skarn | 0.04 | KSDD001 | 239 | 240 | Phyllite | 0.02 | |
| KSDD001 | 196 | 197 | Skarn | 0.03 | KSDD001 | 240 | 241 | Phyllite | 0.02 | |
| KSDD001 | 197 | 198 | Skarn | 0.04 | KSDD001 | 241 | 242 | Phyllite | 0.02 | |
| KSDD001 | 198 | 199 | Skarn | -999 | KSDD001 | 242 | 243 | Phyllite | 0.02 | |
| KSDD001 | 199 | 200 | Skarn | 0.08 | KSDD001 | 243 | 244 | Phyllite | 0.01 | |
| KSDD001 | 200 | 201 | Skarn | -999 | KSDD001 | 244 | 245 | Phyllite | 0.01 | |
| KSDD001 | 201 | 202 | Skarn | 0.1 | KSDD001 | 245 | 246 | Phyllite | 0.02 | |
| KSDD001 | 202 | 202 | Skarn | 0.04 | KSDD001 | 246 | 247 | Phyllite | 0.01 | |
| KSDD001 | 202 | 203 | Skarn | 0.06 | KSDD001 | 247 | 248 | Phyllite | 0.02 | |
| KSDD001 | 203 | 204 | Skarn | 0.02 | KSDD001 | 248 | 249 | Phyllite | 0.02 | |
| KSDD001 | 204 | 205 | Skarn | 0.04 | KSDD001 | 249 | 250 | Phyllite | 0.01 | |
| KSDD001 | 205 | 206 | Skarn | 0.12 | KSDD001 | 250 | 251 | Phyllite | 0.02 | |
| KSDD001 | 206 | 207 | Skarn | 0.04 | KSDD001 | 251 | 252 | Phyllite | 0.02 | |
| KSDD001 | 207 | 208 | Skarn | 0.02 | KSDD001 | 252 | 253 | Phyllite | 0.01 | |
| KSDD001 | 208 | 209 | Skarn | 0.05 | KSDD001 | 253 | 254 | Plutonic | 0.02 | |
| KSDD001 | 209 | 210 | Skarn | 0.03 | KSDD001 | 254 | 255 | Plutonic | 0.01 | |
| KSDD001 | 210 | 211 | Skarn | 0.02 | KSDD001 | 255 | 255 | Phyllite | 0.02 | |
| KSDD001 | 211 | 212 | Skarn | 0.04 | KSDD001 | 255 | 256 | Phyllite | 0.02 | |
| KSDD001 | 212 | 213 | Skarn | 0.05 | KSDD001 | 256 | 257 | Phyllite | 0.02 | |
| KSDD001 | 213 | 214 | Skarn | 0.05 | KSDD001 | 257 | 258 | Phyllite | 0.01 | |
| KSDD001 | 214 | 215 | Skarn | 0.04 | KSDD001 | 258 | 259 | Phyllite | 0.04 | |
| KSDD001 | 215 | 216 | Skarn | 0.05 | KSDD001 | 259 | 260 | Phyllite | 0.02 | |
| KSDD001 | 216 | 217 | Skarn | 0.07 | KSDD001 | 260 | 261 | Phyllite | 0.02 |
35
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD001 | 261 | 262 | Phyllite | 0.01 | KSDD002 | 46 | 47 | Phyllite | 0.08 | |
| KSDD001 | 262 | 263 | Phyllite | 0.01 | KSDD002 | 47 | 48 | Phyllite | 0.06 | |
| KSDD001 | 263 | 264 | Phyllite | 0.07 | KSDD002 | 48 | 49 | Phyllite | 0.16 | |
| KSDD001 | 264 | 265 | Phyllite | 0.02 | KSDD002 | 49 | 50 | Phyllite | 0.07 | |
| KSDD001 | 265 | 266 | Phyllite | -999 | KSDD002 | 50 | 51 | Phyllite | 0.04 | |
| KSDD001 | 266 | 267 | Phyllite | 0.02 | KSDD002 | 51 | 52 | Phyllite | 0.04 | |
| KSDD001 | 267 | 268 | Phyllite | 0.01 | KSDD002 | 52 | 53 | Phyllite | 0.04 | |
| KSDD001 | 268 | 269 | Phyllite | 0.01 | KSDD002 | 53 | 54 | Phyllite | 0.09 | |
| KSDD002 | 0 | 4.1 | Colluvium | 0.07 | KSDD002 | 54 | 55 | Phyllite | 0.15 | |
| KSDD002 | 4.1 | 6 | Phyllite | 0.03 | KSDD002 | 55 | 56 | Phyllite | 0.07 | |
| KSDD002 | 6 | 8 | Phyllite | 0.03 | KSDD002 | 56 | 57 | Shear zone | 0.03 | |
| KSDD002 | 8 | 10 | Fault | 0.04 | KSDD002 | 57 | 58 | Shear zone | 0.22 | |
| KSDD002 | 10 | 11 | Phyllite | 0.02 | KSDD002 | 58 | 59 | Shear zone | 0.19 | |
| KSDD002 | 11 | 12 | Phyllite | 0.04 | KSDD002 | 59 | 60 | Phyllite | 0.04 | |
| KSDD002 | 12 | 13 | Phyllite | 0.53 | KSDD002 | 60 | 62 | Phyllite | 0.05 | |
| KSDD002 | 13 | 15 | Phyllite | 2.45 | KSDD002 | 62 | 63 | Phyllite | 0.82 | |
| KSDD002 | 15 | 16 | Phyllite | 2.85 | KSDD002 | 63 | 64 | Phyllite | 0.23 | |
| KSDD002 | 16 | 17 | Phyllite | 2.24 | KSDD002 | 64 | 66 | Fault | 0.25 | |
| KSDD002 | 17 | 18 | Phyllite | 0.25 | KSDD002 | 66 | 67 | Fault | 0.45 | |
| KSDD002 | 18 | 20 | Phyllite | 0.1 | KSDD002 | 67 | 68 | Fault | 0.42 | |
| KSDD002 | 20 | 22 | Phyllite | 0.18 | KSDD002 | 68 | 69 | Phyllite | -999 | |
| KSDD002 | 22 | 23 | Phyllite | 0.11 | KSDD002 | 69 | 69 | Phyllite | 0.35 | |
| KSDD002 | 23 | 25 | Phyllite | 0.11 | KSDD002 | 69 | 70 | Phyllite | 0.06 | |
| KSDD002 | 25 | 26 | Phyllite | 1.4 | KSDD002 | 70 | 71 | Phyllite | 0.05 | |
| KSDD002 | 26 | 27 | Phyllite | 0.23 | KSDD002 | 71 | 72 | Phyllite | 0.18 | |
| KSDD002 | 27 | 28 | Phyllite | 0.46 | KSDD002 | 72 | 73 | Phyllite | 0.16 | |
| KSDD002 | 28 | 29 | Phyllite | 0.16 | KSDD002 | 73 | 74 | Phyllite | 0.09 | |
| KSDD002 | 29 | 30 | Phyllite | 0.13 | KSDD002 | 74 | 75 | Phyllite | 0.14 | |
| KSDD002 | 30 | 31 | Phyllite | 0.5 | KSDD002 | 75 | 76 | Phyllite | 0.09 | |
| KSDD002 | 31 | 32 | Phyllite | 0.17 | KSDD002 | 76 | 77 | Phyllite | 0.18 | |
| KSDD002 | 32 | 33 | Phyllite | 0.06 | KSDD002 | 77 | 78 | Phyllite | 0.05 | |
| KSDD002 | 33 | 34 | Phyllite | 0.07 | KSDD002 | 78 | 79 | Phyllite | 0.04 | |
| KSDD002 | 34 | 35 | Phyllite | 0.11 | KSDD002 | 79 | 80 | Phyllite | 0.03 | |
| KSDD002 | 35 | 36 | Phyllite | 0.11 | KSDD002 | 80 | 81 | Phyllite | 0.06 | |
| KSDD002 | 36 | 37 | Phyllite | 0.02 | KSDD002 | 81 | 82 | Phyllite | 0.07 | |
| KSDD002 | 37 | 38 | Fault | 0.31 | KSDD002 | 82 | 83 | Phyllite | 0.24 | |
| KSDD002 | 38 | 39 | Fault | 0.25 | KSDD002 | 83 | 84 | Phyllite | 0.08 | |
| KSDD002 | 39 | 40 | Fault | 1.95 | KSDD002 | 84 | 85 | Phyllite | 0.12 | |
| KSDD002 | 40 | 41 | Phyllite | 0.04 | KSDD002 | 85 | 86 | Phyllite | 0.04 | |
| KSDD002 | 41 | 42 | Phyllite | 0.02 | KSDD002 | 86 | 87 | Phyllite | 0.03 | |
| KSDD002 | 42 | 42 | Phyllite | 0.04 | KSDD002 | 87 | 88 | Phyllite | 0.03 | |
| KSDD002 | 42 | 43 | Phyllite | 0.03 | KSDD002 | 88 | 89 | Phyllite | 0.06 | |
| KSDD002 | 43 | 44 | Phyllite | 0.08 | KSDD002 | 89 | 90 | Phyllite | 0.02 | |
| KSDD002 | 44 | 45 | Phyllite | 0.09 | KSDD002 | 90 | 91 | Phyllite | 0.03 | |
| KSDD002 | 45 | 46 | Phyllite | 0.06 | KSDD002 | 91 | 92 | Phyllite | 0.03 |
36
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD002 | 92 | 93 | Phyllite | 0.02 | KSDD002 | 137 | 138 | Skarn | -999 | |
| KSDD002 | 93 | 94 | Phyllite | 0.04 | KSDD002 | 138 | 139 | Skarn | 0.01 | |
| KSDD002 | 94 | 95 | Phyllite | 0.04 | KSDD002 | 139 | 140 | Skarn | -999 | |
| KSDD002 | 95 | 96 | Phyllite | 0.05 | KSDD002 | 140 | 141 | Skarn | -999 | |
| KSDD002 | 96 | 97 | Phyllite | 0.01 | KSDD002 | 141 | 142 | Skarn | -999 | |
| KSDD002 | 97 | 98 | Phyllite | 0.03 | KSDD002 | 142 | 143 | Skarn | 0.01 | |
| KSDD002 | 98 | 99 | Phyllite | 0.04 | KSDD002 | 143 | 144 | Skarn | 0.01 | |
| KSDD002 | 99 | 100 | Phyllite | 0.05 | KSDD002 | 144 | 145 | Skarn | 0.02 | |
| KSDD002 | 100 | 101 | Phyllite | 0.01 | KSDD002 | 145 | 146 | Skarn | 0.02 | |
| KSDD002 | 101 | 102 | Phyllite | 0.02 | KSDD002 | 146 | 147 | Skarn | 0.05 | |
| KSDD002 | 102 | 103 | Phyllite | 0.03 | KSDD002 | 147 | 148 | Skarn | 0.01 | |
| KSDD002 | 103 | 104 | Phyllite | 0.02 | KSDD002 | 148 | 149 | Skarn | 0.01 | |
| KSDD002 | 104 | 105 | Phyllite | 0.01 | KSDD002 | 149 | 150 | Skarn | 0.01 | |
| KSDD002 | 105 | 106 | Phyllite | 0.01 | KSDD002 | 150 | 151 | Skarn | -999 | |
| KSDD002 | 106 | 107 | Phyllite | 0.01 | KSDD002 | 151 | 152 | Shear zone | 0.01 | |
| KSDD002 | 107 | 108 | Skarn | -999 | KSDD002 | 152 | 153 | Shear zone | 0.05 | |
| KSDD002 | 108 | 109 | Skarn | 0.01 | KSDD002 | 153 | 156 | Shear zone | -999 | |
| KSDD002 | 109 | 110 | Skarn | 0.01 | KSDD002 | 156 | 157 | Shear zone | 0.11 | |
| KSDD002 | 110 | 111 | Skarn | 0.02 | KSDD002 | 157 | 157 | Shear zone | -999 | |
| KSDD002 | 111 | 112 | Skarn | 0.02 | KSDD002 | 157 | 158 | Shear zone | 0.06 | |
| KSDD002 | 112 | 113 | Skarn | 0.02 | KSDD002 | 158 | 159 | Shear zone | 0.44 | |
| KSDD002 | 113 | 114 | Skarn | 0.01 | KSDD002 | 159 | 160 | Shear zone | -999 | |
| KSDD002 | 114 | 115 | Skarn | 0.02 | KSDD002 | 160 | 161 | Shear zone | 0.06 | |
| KSDD002 | 115 | 116 | Skarn | 0.02 | KSDD002 | 161 | 162 | Shear zone | 0.05 | |
| KSDD002 | 116 | 117 | Skarn | 0.01 | KSDD002 | 162 | 164 | Shear zone | -999 | |
| KSDD002 | 117 | 118 | Skarn | -999 | KSDD002 | 164 | 165 | Phyllite | 0.12 | |
| KSDD002 | 118 | 119 | Skarn | 0.01 | KSDD002 | 165 | 165 | Phyllite | 0.01 | |
| KSDD002 | 119 | 120 | Skarn | -999 | KSDD002 | 165 | 166 | Phyllite | 0.03 | |
| KSDD002 | 120 | 121 | Skarn | -999 | KSDD002 | 166 | 167 | Phyllite | 0.01 | |
| KSDD002 | 121 | 122 | Skarn | -999 | KSDD002 | 167 | 168 | Phyllite | 0.11 | |
| KSDD002 | 122 | 123 | Skarn | -999 | KSDD002 | 168 | 169 | Phyllite | 0.02 | |
| KSDD002 | 123 | 124 | Skarn | -999 | KSDD002 | 169 | 170 | Phyllite | 0.01 | |
| KSDD002 | 124 | 125 | Skarn | 0.02 | KSDD002 | 170 | 171 | Phyllite | -999 | |
| KSDD002 | 125 | 126 | Skarn | -999 | KSDD002 | 171 | 172 | Phyllite | 0.01 | |
| KSDD002 | 126 | 127 | Skarn | 0.01 | KSDD002 | 172 | 173 | Phyllite | 0.04 | |
| KSDD002 | 127 | 128 | Skarn | -999 | KSDD002 | 173 | 174 | Phyllite | 0.02 | |
| KSDD002 | 128 | 129 | Skarn | -999 | KSDD002 | 174 | 175 | Phyllite | 0.02 | |
| KSDD002 | 129 | 130 | Skarn | 0.03 | KSDD002 | 175 | 177 | Phyllite | 0.02 | |
| KSDD002 | 130 | 131 | Skarn | 0.02 | KSDD002 | 177 | 177 | Plutonic | -999 | |
| KSDD002 | 131 | 132 | Skarn | 0.02 | KSDD002 | 177 | 178 | Plutonic | -999 | |
| KSDD002 | 132 | 133 | Skarn | 0.02 | KSDD002 | 178 | 179 | Plutonic | 0.01 | |
| KSDD002 | 133 | 134 | Skarn | 0.01 | KSDD002 | 179 | 180 | Plutonic | -999 | |
| KSDD002 | 134 | 135 | Skarn | -999 | KSDD002 | 180 | 181 | Phyllite | 0.01 | |
| KSDD002 | 135 | 136 | Skarn | -999 | KSDD002 | 181 | 182 | Phyllite | 0.01 | |
| KSDD002 | 136 | 137 | Skarn | -999 | KSDD002 | 182 | 183 | Phyllite | 0.02 |
37
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD002 | 183 | 184 | Phyllite | 0.01 | KSDD003 | 2.1 | 2.9 | Phyllite | 0.45 | |
| KSDD002 | 184 | 185 | Plutonic | -999 | KSDD003 | 2.9 | 3.6 | Phyllite | 0.46 | |
| KSDD002 | 185 | 186 | Plutonic | -999 | KSDD003 | 3.6 | 4.6 | Skarn | 0.98 | |
| KSDD002 | 186 | 187 | Plutonic | -999 | KSDD003 | 4.6 | 5.1 | Skarn | -999 | |
| KSDD002 | 187 | 188 | Plutonic | 0.01 | KSDD003 | 5.1 | 6 | Skarn | 3.79 | |
| KSDD002 | 188 | 189 | Plutonic | -999 | KSDD003 | 6 | 7 | Skarn | 2.5 | |
| KSDD002 | 189 | 190 | Plutonic | 0.01 | KSDD003 | 7 | 8 | Skarn | 3.89 | |
| KSDD002 | 190 | 191 | Phyllite | 0.02 | KSDD003 | 8 | 9 | Skarn | 8.29 | |
| KSDD002 | 191 | 192 | Phyllite | 0.02 | KSDD003 | 9 | 10 | Skarn | 3.53 | |
| KSDD002 | 192 | 193 | Phyllite | -999 | KSDD003 | 10 | 11 | Limestone | 0.03 | |
| KSDD002 | 193 | 194 | Phyllite | 0.01 | KSDD003 | 11 | 12 | Limestone | 0.03 | |
| KSDD002 | 194 | 194 | Phyllite | 0.01 | KSDD003 | 12 | 13 | Limestone | 0.39 | |
| KSDD002 | 194 | 195 | Phyllite | 0.02 | KSDD003 | 13 | 14 | Limestone | 0.53 | |
| KSDD002 | 195 | 196 | Phyllite | 0.01 | KSDD003 | 14 | 15 | Limestone | 0.24 | |
| KSDD002 | 196 | 197 | Phyllite | 0.01 | KSDD003 | 15 | 16 | Limestone | 0.05 | |
| KSDD002 | 197 | 198 | Phyllite | 0.01 | KSDD003 | 16 | 17 | Limestone | 0.06 | |
| KSDD002 | 198 | 199 | Phyllite | 0.01 | KSDD003 | 17 | 18 | Limestone | 0.56 | |
| KSDD002 | 199 | 200 | Plutonic | 0.01 | KSDD003 | 18 | 19 | Limestone | 0.03 | |
| KSDD002 | 200 | 201 | Plutonic | 0.01 | KSDD003 | 19 | 20 | Limestone | 0.03 | |
| KSDD002 | 201 | 202 | Plutonic | 0.01 | KSDD003 | 20 | 21 | Limestone | 0.05 | |
| KSDD002 | 202 | 203 | Plutonic | -999 | KSDD003 | 21 | 22 | Limestone | 0.04 | |
| KSDD002 | 203 | 204 | Phyllite | 0.01 | KSDD003 | 22 | 23 | Limestone | 0.1 | |
| KSDD002 | 204 | 205 | Phyllite | 0.01 | KSDD003 | 23 | 24 | Limestone | 0.03 | |
| KSDD002 | 205 | 206 | Phyllite | 0.01 | KSDD003 | 24 | 25 | Limestone | 0.03 | |
| KSDD002 | 206 | 207 | Phyllite | 0.01 | KSDD003 | 25 | 26 | Limestone | 0.04 | |
| KSDD002 | 207 | 208 | Phyllite | 0.01 | KSDD003 | 26 | 27 | Limestone | 0.02 | |
| KSDD002 | 208 | 209 | Phyllite | 0.01 | KSDD003 | 27 | 28 | Limestone | 0.03 | |
| KSDD002 | 209 | 210 | Phyllite | 0.01 | KSDD003 | 28 | 29 | Limestone | 0.03 | |
| KSDD002 | 210 | 210 | Plutonic | -999 | KSDD003 | 29 | 30 | Limestone | 0.02 | |
| KSDD002 | 210 | 211 | Plutonic | -999 | KSDD003 | 30 | 31 | Limestone | 0.15 | |
| KSDD002 | 211 | 212 | Phyllite | 0.01 | KSDD003 | 31 | 32 | Limestone | 0.18 | |
| KSDD002 | 212 | 213 | Phyllite | 0.01 | KSDD003 | 32 | 33 | Limestone | 0.07 | |
| KSDD002 | 213 | 214 | Phyllite | 0.02 | KSDD003 | 33 | 34 | Limestone | 0.02 | |
| KSDD002 | 214 | 215 | Phyllite | 0.01 | KSDD003 | 34 | 35 | Limestone | 0.02 | |
| KSDD002 | 215 | 216 | Plutonic | 0.01 | KSDD003 | 35 | 36 | Limestone | 0.02 | |
| KSDD002 | 216 | 217 | Plutonic | -999 | KSDD003 | 36 | 37 | Limestone | 0.01 | |
| KSDD002 | 217 | 218 | Plutonic | 0.01 | KSDD003 | 37 | 38 | Limestone | 0.02 | |
| KSDD002 | 218 | 219 | Plutonic | -999 | KSDD003 | 38 | 39 | Limestone | 0.08 | |
| KSDD002 | 219 | 220 | Plutonic | 0.01 | KSDD003 | 39 | 40 | Limestone | 0.06 | |
| KSDD002 | 220 | 221 | Plutonic | 0.01 | KSDD003 | 40 | 41 | Limestone | 0.17 | |
| KSDD002 | 221 | 222 | Plutonic | 0.01 | KSDD003 | 41 | 42 | Shear zone | 0.13 | |
| KSDD002 | 222 | 223 | Plutonic | 0.01 | KSDD003 | 42 | 43 | Phyllite | 0.04 | |
| KSDD002 | 223 | 224 | Plutonic | -999 | KSDD003 | 43 | 44 | Plutonic | 0.02 | |
| KSDD002 | 224 | 225 | Plutonic | -999 | KSDD003 | 44 | 45 | Phyllite | 0.03 | |
| KSDD003 | 0 | 2.1 | Phyllite | 0.3 | KSDD003 | 45 | 46 | Phyllite | 0.05 |
38
25 November 2022 ASX Announcement
ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD003 | 46 | 47 | Phyllite | 0.03 | KSDD003 | 91 | 92 | Phyllite | 0.02 | |
| KSDD003 | 47 | 48 | Phyllite | 0.05 | KSDD003 | 92 | 93 | Phyllite | 0.02 | |
| KSDD003 | 48 | 49 | Phyllite | 0.03 | KSDD003 | 93 | 94 | Phyllite | 0.02 | |
| KSDD003 | 49 | 50 | Plutonic | 0.02 | KSDD003 | 94 | 95 | Phyllite | 0.02 | |
| KSDD003 | 50 | 51 | Plutonic | 0.02 | KSDD003 | 95 | 96 | Phyllite | 0.01 | |
| KSDD003 | 51 | 52 | Phyllite | 0.05 | KSDD003 | 96 | 97 | Phyllite | 0.05 | |
| KSDD003 | 52 | 53 | Phyllite | 0.03 | KSDD003 | 97 | 98 | Phyllite | 0.02 | |
| KSDD003 | 53 | 54 | Phyllite | 0.02 | KSDD003 | 98 | 99 | Phyllite | 0.02 | |
| KSDD003 | 54 | 55 | Phyllite | 0.03 | KSDD003 | 99 | 100 | Phyllite | 0.01 | |
| KSDD003 | 55 | 56 | Phyllite | 0.05 | KSDD003 | 100 | 101 | Phyllite | 0.03 | |
| KSDD003 | 56 | 57 | Plutonic | 0.08 | KSDD003 | 101 | 102 | Phyllite | 0.05 | |
| KSDD003 | 57 | 58 | Phyllite | 0.03 | KSDD003 | 102 | 103 | Phyllite | 0.03 | |
| KSDD003 | 58 | 59 | Phyllite | 0.02 | KSDD003 | 103 | 104 | Phyllite | 0.03 | |
| KSDD003 | 59 | 60 | Phyllite | 0.03 | KSDD003 | 104 | 105 | Phyllite | 0.02 | |
| KSDD003 | 60 | 61 | Phyllite | 0.05 | KSDD003 | 105 | 106 | Phyllite | 0.02 | |
| KSDD003 | 61 | 62 | Plutonic | 0.02 | KSDD003 | 106 | 107 | Phyllite | 0.02 | |
| KSDD003 | 62 | 63 | Phyllite | 0.02 | KSDD003 | 107 | 108 | Phyllite | 0.02 | |
| KSDD003 | 63 | 64 | Phyllite | 0.04 | KSDD003 | 108 | 109 | Phyllite | 0.01 | |
| KSDD003 | 64 | 65 | Plutonic | 0.24 | KSDD003 | 109 | 110 | Phyllite | 0.03 | |
| KSDD003 | 65 | 66 | Plutonic | 0.02 | KSDD003 | 110 | 111 | Phyllite | 0.02 | |
| KSDD003 | 66 | 67 | Phyllite | 0.02 | KSDD003 | 111 | 112 | Phyllite | 0.02 | |
| KSDD003 | 67 | 68 | Plutonic | 0.02 | KSDD003 | 112 | 113 | Phyllite | 0.02 | |
| KSDD003 | 68 | 69 | Plutonic | 0.01 | KSDD003 | 113 | 114 | Phyllite | 0.02 | |
| KSDD003 | 69 | 70 | Phyllite | 0.02 | KSDD003 | 114 | 115 | Phyllite | 0.01 | |
| KSDD003 | 70 | 71 | Phyllite | 0.04 | KSDD003 | 115 | 116 | Phyllite | 0.01 | |
| KSDD003 | 71 | 72 | Phyllite | 0.06 | KSDD003 | 116 | 117 | Phyllite | 0.02 | |
| KSDD003 | 72 | 73 | Phyllite | 0.11 | KSDD003 | 117 | 118 | Phyllite | 0.02 | |
| KSDD003 | 73 | 74 | Phyllite | 1.08 | KSDD003 | 118 | 119 | Phyllite | 0.02 | |
| KSDD003 | 74 | 75 | Phyllite | 0.12 | KSDD003 | 119 | 120 | Phyllite | 0.02 | |
| KSDD003 | 75 | 76 | Phyllite | 0.03 | KSDD003 | 120 | 121 | Phyllite | 0.02 | |
| KSDD003 | 76 | 77 | Phyllite | 0.04 | KSDD003 | 121 | 122 | Phyllite | 0.02 | |
| KSDD003 | 77 | 78 | Plutonic | 0.05 | KSDD003 | 122 | 123 | Phyllite | 0.02 | |
| KSDD003 | 78 | 79 | Phyllite | 0.11 | KSDD003 | 123 | 124 | Phyllite | 0.01 | |
| KSDD003 | 79 | 80 | Plutonic | 0.03 | KSDD003 | 124 | 125 | Phyllite | 0.02 | |
| KSDD003 | 80 | 81 | Plutonic | 0.02 | KSDD003 | 125 | 126 | Phyllite | 0.06 | |
| KSDD003 | 81 | 82 | Plutonic | 0.12 | KSDD003 | 126 | 127 | Phyllite | 0.03 | |
| KSDD003 | 82 | 83 | Plutonic | 0.72 | KSDD003 | 127 | 128 | Phyllite | 0.06 | |
| KSDD003 | 83 | 84 | Plutonic | 0.5 | KSDD003 | 128 | 129 | Phyllite | 0.01 | |
| KSDD003 | 84 | 85 | Phyllite | 0.02 | KSDD003 | 129 | 130 | Diorite | 0.02 | |
| KSDD003 | 85 | 86 | Phyllite | 0.02 | KSDD003 | 130 | 131 | Diorite | 0.01 | |
| KSDD003 | 86 | 87 | Phyllite | 0.01 | KSDD003 | 131 | 132 | Diorite | -999 | |
| KSDD003 | 87 | 88 | Phyllite | 0.03 | KSDD003 | 132 | 133 | Diorite | 0.01 | |
| KSDD003 | 88 | 89 | Phyllite | 0.02 | KSDD003 | 133 | 134 | Diorite | -999 | |
| KSDD003 | 89 | 90 | Phyllite | 0.01 | KSDD003 | 134 | 135 | Diorite | -999 | |
| KSDD003 | 90 | 91 | Phyllite | 0.02 | KSDD003 | 135 | 136 | Diorite | 0.01 |
39
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD003 | 136 | 137 | Diorite | 0.03 | KSDD003 | 182 | 183 | Diorite | 0.02 | |
| KSDD003 | 137 | 138 | Diorite | 0.03 | KSDD003 | 183 | 184 | Diorite | 0.02 | |
| KSDD003 | 138 | 139 | Diorite | 0.02 | KSDD003 | 184 | 185 | Diorite | 0.02 | |
| KSDD003 | 139 | 140 | Diorite | 0.03 | KSDD003 | 185 | 186 | Diorite | 0.02 | |
| KSDD003 | 140 | 141 | Diorite | 0.02 | KSDD003 | 186 | 187 | Diorite | 0.02 | |
| KSDD003 | 141 | 142 | Diorite | 0.03 | KSDD003 | 187 | 188 | Diorite | 0.02 | |
| KSDD003 | 142 | 143 | Diorite | 0.02 | KSDD003 | 188 | 189 | Diorite | 0.02 | |
| KSDD003 | 143 | 144 | Diorite | 0.02 | KSDD003 | 189 | 190 | Phyllite | 0.02 | |
| KSDD003 | 144 | 145 | Diorite | 0.02 | KSDD003 | 190 | 191 | Phyllite | 0.02 | |
| KSDD003 | 145 | 146 | Diorite | 0.02 | KSDD003 | 191 | 192 | Phyllite | 0.02 | |
| KSDD003 | 146 | 147 | Diorite | 0.03 | KSDD003 | 192 | 193 | Phyllite | 0.02 | |
| KSDD003 | 147 | 148 | Phyllite | 0.03 | KSDD003 | 193 | 194 | Phyllite | 0.02 | |
| KSDD003 | 148 | 149 | Phyllite | 0.02 | KSDD003 | 194 | 195 | Phyllite | 0.02 | |
| KSDD003 | 149 | 150 | Phyllite | 0.02 | KSDD003 | 195 | 196 | Phyllite | 0.02 | |
| KSDD003 | 150 | 151 | Phyllite | 0.02 | KSDD003 | 196 | 197 | Phyllite | 0.02 | |
| KSDD003 | 151 | 152 | Phyllite | 0.02 | KSDD003 | 197 | 198 | Phyllite | 0.01 | |
| KSDD003 | 152 | 153 | Phyllite | 0.02 | KSDD003 | 198 | 199 | Diorite | 0.01 | |
| KSDD003 | 153 | 154 | Phyllite | 0.02 | KSDD003 | 199 | 200 | Diorite | 0.01 | |
| KSDD003 | 154 | 155 | Phyllite | 0.03 | KSDD003 | 200 | 201 | Diorite | 0.01 | |
| KSDD003 | 155 | 156 | Phyllite | 0.04 | KSDD003 | 201 | 202 | Phyllite | 0.02 | |
| KSDD003 | 156 | 157 | Phyllite | 0.04 | KSDD003 | 202 | 204 | Phyllite | 0.02 | |
| KSDD003 | 157 | 158 | Phyllite | 0.02 | KSDD003 | 204 | 205 | Phyllite | -999 | |
| KSDD003 | 158 | 159 | Phyllite | 0.07 | KSDD003 | 205 | 206 | Phyllite | 0.02 | |
| KSDD003 | 159 | 160 | Phyllite | 0.02 | KSDD003 | 206 | 208 | Phyllite | 0.02 | |
| KSDD003 | 160 | 161 | Phyllite | 0.05 | KSDD003 | 208 | 210 | Diorite | 0.02 | |
| KSDD003 | 161 | 162 | Phyllite | 0.02 | KSDD003 | 210 | 212 | Phyllite | 0.02 | |
| KSDD003 | 162 | 163 | Phyllite | 0.08 | KSDD003 | 212 | 214 | Phyllite | 0.02 | |
| KSDD003 | 163 | 164 | Phyllite | 0.05 | KSDD003 | 214 | 216 | Phyllite | 0.02 | |
| KSDD003 | 164 | 165 | Phyllite | 0.02 | KSDD003 | 216 | 218 | Phyllite | 0.02 | |
| KSDD003 | 165 | 166 | Phyllite | 0.06 | KSDD003 | 218 | 219 | Phyllite | 0.02 | |
| KSDD003 | 166 | 167 | Phyllite | 0.03 | KSDD003 | 219 | 220 | Phyllite | 0.01 | |
| KSDD003 | 167 | 168 | Phyllite | 0.02 | KSDD003 | 220 | 221 | Phyllite | 0.01 | |
| KSDD003 | 168 | 169 | Phyllite | 0.02 | KSDD003 | 221 | 222 | Phyllite | 0.02 | |
| KSDD003 | 169 | 170 | Phyllite | 0.02 | KSDD003 | 222 | 223 | Phyllite | 0.01 | |
| KSDD003 | 170 | 171 | Phyllite | 0.04 | KSDD003 | 223 | 224 | Phyllite | 0.01 | |
| KSDD003 | 171 | 172 | Phyllite | 0.02 | KSDD003 | 224 | 225 | Phyllite | 0.01 | |
| KSDD003 | 172 | 173 | Phyllite | 0.03 | KSDD003 | 225 | 226 | Phyllite | 0.02 | |
| KSDD003 | 173 | 174 | Phyllite | 0.02 | KSDD003 | 226 | 227 | Phyllite | 0.02 | |
| KSDD003 | 174 | 175 | Phyllite | 0.02 | KSDD003 | 227 | 228 | Phyllite | 0.01 | |
| KSDD003 | 175 | 176 | Phyllite | 0.02 | KSDD003 | 228 | 229 | Phyllite | 0.01 | |
| KSDD003 | 176 | 177 | Diorite | 0.02 | KSDD003 | 229 | 230 | Phyllite | 0.01 | |
| KSDD003 | 177 | 179 | Diorite | 0.02 | KSDD003 | 230 | 231 | Phyllite | 0.01 | |
| KSDD003 | 179 | 180 | Phyllite | 0.02 | KSDD003 | 231 | 232 | Phyllite | 0.02 | |
| KSDD003 | 180 | 181 | Phyllite | 0.02 | KSDD003 | 232 | 233 | Phyllite | 0.01 | |
| KSDD003 | 181 | 182 | Phyllite | 0.02 | KSDD003 | 233 | 234 | Phyllite | 0.02 |
40
25 November 2022 ASX Announcement
ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD003 | 234 | 235 | Phyllite | 0.01 | KSDD003 | 279 | 280 | Phyllite | 0.02 | |
| KSDD003 | 235 | 236 | Phyllite | 0.01 | KSDD003 | 280 | 281 | Phyllite | 0.02 | |
| KSDD003 | 236 | 237 | Phyllite | -999 | KSDD003 | 281 | 282 | Phyllite | 0.03 | |
| KSDD003 | 237 | 238 | Phyllite | 0.01 | KSDD003 | 282 | 283 | Phyllite | 0.06 | |
| KSDD003 | 238 | 239 | Phyllite | 0.02 | KSDD003 | 283 | 284 | Phyllite | 0.03 | |
| KSDD003 | 239 | 240 | Phyllite | 0.02 | KSDD003 | 284 | 285 | Phyllite | 0.04 | |
| KSDD003 | 240 | 241 | Phyllite | 0.01 | KSDD003 | 285 | 286 | Phyllite | 0.03 | |
| KSDD003 | 241 | 242 | Phyllite | 0.02 | KSDD003 | 286 | 287 | Phyllite | 0.01 | |
| KSDD003 | 242 | 243 | Phyllite | 0.02 | KSDD003 | 287 | 288 | Phyllite | 0.02 | |
| KSDD003 | 243 | 244 | Phyllite | 0.02 | KSDD003 | 288 | 289 | Phyllite | 0.02 | |
| KSDD003 | 244 | 245 | Phyllite | 0.01 | KSDD003 | 289 | 290 | Phyllite | 0.01 | |
| KSDD003 | 245 | 246 | Phyllite | 0.02 | KSDD003 | 290 | 291 | Phyllite | 0.04 | |
| KSDD003 | 246 | 247 | Phyllite | 0.01 | KSDD003 | 291 | 292 | Phyllite | 0.04 | |
| KSDD003 | 247 | 248 | Phyllite | 0.01 | KSDD003 | 292 | 293 | Phyllite | 0.02 | |
| KSDD003 | 248 | 249 | Phyllite | 0.01 | KSDD003 | 293 | 294 | Phyllite | 0.01 | |
| KSDD003 | 249 | 250 | Phyllite | 0.45 | KSDD003 | 294 | 295 | Phyllite | 0.01 | |
| KSDD003 | 250 | 251 | Phyllite | 0.01 | KSDD003 | 295 | 296 | Phyllite | 0.01 | |
| KSDD003 | 251 | 252 | Phyllite | 0.02 | KSDD003 | 296 | 297 | Phyllite | 0.02 | |
| KSDD003 | 252 | 253 | Phyllite | 0.05 | KSDD003 | 297 | 298 | Phyllite | 0.01 | |
| KSDD003 | 253 | 254 | Phyllite | 0.01 | KSDD003 | 298 | 299 | Phyllite | 0.08 | |
| KSDD003 | 254 | 255 | Phyllite | 0.02 | KSDD003 | 299 | 300 | Phyllite | 0.04 | |
| KSDD003 | 255 | 256 | Phyllite | 0.02 | KSDD003 | 300 | 301 | Phyllite | 0.02 | |
| KSDD003 | 256 | 257 | Phyllite | 0.02 | KSDD003 | 301 | 302 | Phyllite | 0.08 | |
| KSDD003 | 257 | 258 | Phyllite | 0.05 | KSDD003 | 302 | 303 | Phyllite | 0.03 | |
| KSDD003 | 258 | 259 | Phyllite | 0.06 | KSDD003 | 303 | 304 | Phyllite | 0.02 | |
| KSDD003 | 259 | 260 | Phyllite | 0.04 | KSDD003 | 304 | 305 | Phyllite | 0.03 | |
| KSDD003 | 260 | 261 | Phyllite | 0.02 | KSDD003 | 305 | 306 | Phyllite | 0.03 | |
| KSDD003 | 261 | 262 | Phyllite | 0.04 | KSDD003 | 306 | 307 | Phyllite | 0.05 | |
| KSDD003 | 262 | 263 | Phyllite | 0.06 | KSDD003 | 307 | 308 | Phyllite | 0.05 | |
| KSDD003 | 263 | 264 | Phyllite | 0.02 | KSDD003 | 308 | 309 | Phyllite | 0.04 | |
| KSDD003 | 264 | 265 | Phyllite | 0.02 | KSDD003 | 309 | 310 | Phyllite | 0.04 | |
| KSDD003 | 265 | 266 | Diorite | 0.01 | KSDD003 | 310 | 311 | Phyllite | 0.04 | |
| KSDD003 | 266 | 267 | Diorite | 0.02 | KSDD003 | 311 | 312 | Phyllite | 0.03 | |
| KSDD003 | 267 | 268 | Diorite | 0.06 | KSDD003 | 312 | 313 | Phyllite | 0.02 | |
| KSDD003 | 268 | 269 | Diorite | 0.08 | KSDD003 | 313 | 314 | Phyllite | 0.02 | |
| KSDD003 | 269 | 270 | Diorite | 0.12 | KSDD003 | 314 | 315 | Phyllite | 0.02 | |
| KSDD003 | 270 | 271 | Phyllite | 0.02 | KSDD003 | 315 | 316 | Phyllite | 0.04 | |
| KSDD003 | 271 | 272 | Phyllite | 0.02 | KSDD003 | 316 | 317 | Phyllite | 0.06 | |
| KSDD003 | 272 | 273 | Phyllite | 0.02 | KSDD003 | 317 | 318 | Phyllite | 0.02 | |
| KSDD003 | 273 | 274 | Phyllite | 0.02 | KSDD003 | 318 | 319 | Phyllite | 0.05 | |
| KSDD003 | 274 | 275 | Phyllite | 0.04 | KSDD003 | 319 | 320 | Phyllite | 0.13 | |
| KSDD003 | 275 | 276 | Phyllite | 0.06 | KSDD003 | 320 | 321 | Phyllite | 0.42 | |
| KSDD003 | 276 | 277 | Phyllite | 0.02 | KSDD003 | 321 | 322 | Phyllite | 0.06 | |
| KSDD003 | 277 | 278 | Phyllite | 0.02 | KSDD003 | 322 | 323 | Phyllite | 0.03 | |
| KSDD003 | 278 | 279 | Phyllite | 0.02 | KSDD003 | 323 | 324 | Phyllite | 0.02 |
41
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD003 | 324 | 325 | Phyllite | 0.01 | KSDD004 | 4 | 4.4 | Phyllite | 0.03 | |
| KSDD003 | 325 | 326 | Phyllite | 0.06 | KSDD004 | 4.4 | 5 | Diorite | -999 | |
| KSDD003 | 326 | 327 | Phyllite | 0.03 | KSDD004 | 5 | 6 | Diorite | 0.19 | |
| KSDD003 | 327 | 328 | Phyllite | 0.02 | KSDD004 | 6 | 7 | Diorite | 0.06 | |
| KSDD003 | 328 | 329 | Phyllite | 0.03 | KSDD004 | 7 | 7.4 | Diorite | -999 | |
| KSDD003 | 329 | 330 | Phyllite | 0.01 | KSDD004 | 7.4 | 8 | Diorite | 0.06 | |
| KSDD003 | 330 | 331 | Phyllite | 0.02 | KSDD004 | 8 | 9 | Diorite | 0.06 | |
| KSDD003 | 331 | 332 | Phyllite | 0.02 | KSDD004 | 9 | 10 | Diorite | 0.12 | |
| KSDD003 | 332 | 333 | Phyllite | 0.01 | KSDD004 | 10 | 11 | Diorite | -999 | |
| KSDD003 | 333 | 334 | Phyllite | 0.01 | KSDD004 | 11 | 11 | Diorite | 0.07 | |
| KSDD003 | 334 | 335 | Phyllite | 0.02 | KSDD004 | 11 | 12 | Diorite | -999 | |
| KSDD003 | 335 | 336 | Phyllite | 0.02 | KSDD004 | 12 | 13 | Diorite | 0.05 | |
| KSDD003 | 336 | 337 | Phyllite | 0.15 | KSDD004 | 13 | 13 | Diorite | 0.05 | |
| KSDD003 | 337 | 338 | Phyllite | 0.18 | KSDD004 | 13 | 14 | Diorite | -999 | |
| KSDD003 | 338 | 339 | Phyllite | 0.09 | KSDD004 | 14 | 15 | Diorite | 0.06 | |
| KSDD003 | 339 | 340 | Phyllite | 0.03 | KSDD004 | 15 | 15 | Diorite | 0.12 | |
| KSDD003 | 340 | 341 | Phyllite | 0.11 | KSDD004 | 15 | 16 | Diorite | 0.36 | |
| KSDD003 | 341 | 342 | Phyllite | 0.03 | KSDD004 | 16 | 17 | Diorite | 0.43 | |
| KSDD003 | 342 | 343 | Phyllite | 0.01 | KSDD004 | 17 | 18 | Diorite | 0.27 | |
| KSDD003 | 343 | 344 | Phyllite | 0.01 | KSDD004 | 18 | 19 | Andesite | 0.65 | |
| KSDD003 | 344 | 345 | Phyllite | 0.01 | KSDD004 | 19 | 20 | Andesite | 0.68 | |
| KSDD003 | 345 | 346 | Phyllite | 0.01 | KSDD004 | 20 | 21 | Andesite | 0.74 | |
| KSDD003 | 346 | 347 | Phyllite | 0.01 | KSDD004 | 21 | 22 | Diorite | 0.54 | |
| KSDD003 | 347 | 348 | Phyllite | 0.01 | KSDD004 | 22 | 22 | Diorite | -999 | |
| KSDD003 | 348 | 349 | Phyllite | 0.01 | KSDD004 | 22 | 23 | Diorite | 0.56 | |
| KSDD003 | 349 | 350 | Phyllite | 0.01 | KSDD004 | 23 | 24 | Diorite | 0.28 | |
| KSDD003 | 350 | 351 | Phyllite | 0.01 | KSDD004 | 24 | 24 | Diorite | -999 | |
| KSDD003 | 351 | 352 | Phyllite | 0.01 | KSDD004 | 24 | 25 | Diorite | 0.15 | |
| KSDD003 | 352 | 353 | Phyllite | 0.01 | KSDD004 | 25 | 25 | Diorite | 0.3 | |
| KSDD003 | 353 | 354 | Phyllite | 0.01 | KSDD004 | 25 | 26 | Diorite | -999 | |
| KSDD003 | 354 | 355 | Phyllite | 0.02 | KSDD004 | 26 | 27 | Diorite | 0.22 | |
| KSDD003 | 355 | 356 | Phyllite | 0.01 | KSDD004 | 27 | 28 | Diorite | -999 | |
| KSDD003 | 356 | 357 | Phyllite | 0.01 | KSDD004 | 28 | 28 | Diorite | 0.02 | |
| KSDD003 | 357 | 358 | Phyllite | -999 | KSDD004 | 28 | 29 | Diorite | 0.1 | |
| KSDD003 | 358 | 359 | Phyllite | 0.02 | KSDD004 | 29 | 30 | Diorite | 0.05 | |
| KSDD003 | 359 | 360 | Phyllite | 0.01 | KSDD004 | 30 | 31 | Diorite | 0.04 | |
| KSDD003 | 360 | 361 | Phyllite | 0.01 | KSDD004 | 31 | 31 | Diorite | -999 | |
| KSDD003 | 361 | 362 | Phyllite | -999 | KSDD004 | 31 | 32 | Diorite | 0.03 | |
| KSDD003 | 362 | 363 | Phyllite | 0.01 | KSDD004 | 32 | 33 | Diorite | -999 | |
| KSDD003 | 363 | 364 | Phyllite | 0.01 | KSDD004 | 33 | 33 | Diorite | 0.05 | |
| KSDD003 | 364 | 365 | Phyllite | 0.01 | KSDD004 | 33 | 34 | Diorite | 0.07 | |
| KSDD004 | 0 | 1.8 | Phyllite | -999 | KSDD004 | 34 | 35 | Diorite | 0.09 | |
| KSDD004 | 1.8 | 2.2 | Phyllite | 0.3 | KSDD004 | 35 | 36 | Diorite | 0.05 | |
| KSDD004 | 2.2 | 3.7 | Phyllite | -999 | KSDD004 | 36 | 37 | Diorite | 0.04 | |
| KSDD004 | 3.7 | 4 | Phyllite | 0.07 | KSDD004 | 37 | 38 | Diorite | 0.05 |
42
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD004 | 38 | 39 | Diorite | 0.04 | KSDD004 | 82 | 83 | Phyllite | 0.06 | |
| KSDD004 | 39 | 40 | Diorite | 0.08 | KSDD004 | 83 | 84 | Phyllite | 0.05 | |
| KSDD004 | 40 | 41 | Diorite | 0.07 | KSDD004 | 84 | 85 | Phyllite | 0.06 | |
| KSDD004 | 41 | 42 | Diorite | 0.05 | KSDD004 | 85 | 86 | Phyllite | 0.06 | |
| KSDD004 | 42 | 43 | Diorite | 0.08 | KSDD004 | 86 | 87 | Phyllite | 0.07 | |
| KSDD004 | 43 | 44 | Diorite | 0.06 | KSDD004 | 87 | 88 | Diorite | 0.07 | |
| KSDD004 | 44 | 45 | Diorite | 0.03 | KSDD004 | 88 | 89 | Diorite | 0.02 | |
| KSDD004 | 45 | 46 | Diorite | 0.05 | KSDD004 | 89 | 90 | Diorite | 0.06 | |
| KSDD004 | 46 | 47 | Diorite | 0.03 | KSDD004 | 90 | 91 | Diorite | 0.08 | |
| KSDD004 | 47 | 48 | Diorite | 0.04 | KSDD004 | 91 | 92 | Diorite | 0.06 | |
| KSDD004 | 48 | 49 | Diorite | 0.04 | KSDD004 | 92 | 93 | Diorite | 0.04 | |
| KSDD004 | 49 | 50 | Diorite | 0.03 | KSDD004 | 93 | 94 | Phyllite | 0.06 | |
| KSDD004 | 50 | 51 | Diorite | 0.05 | KSDD004 | 94 | 95 | Phyllite | 0.04 | |
| KSDD004 | 51 | 52 | Diorite | 0.12 | KSDD004 | 95 | 96 | Phyllite | 0.04 | |
| KSDD004 | 52 | 53 | Diorite | 0.03 | KSDD004 | 96 | 97 | Phyllite | 0.04 | |
| KSDD004 | 53 | 54 | Diorite | 0.03 | KSDD004 | 97 | 98 | Phyllite | 0.08 | |
| KSDD004 | 54 | 55 | Diorite | 0.04 | KSDD004 | 98 | 99 | Phyllite | 0.06 | |
| KSDD004 | 55 | 56 | Diorite | 0.04 | KSDD004 | 99 | 100 | Phyllite | 0.04 | |
| KSDD004 | 56 | 57 | Diorite | 0.05 | KSDD004 | 100 | 101 | Phyllite | 0.09 | |
| KSDD004 | 57 | 58 | Diorite | 0.1 | KSDD004 | 101 | 102 | Phyllite | 0.06 | |
| KSDD004 | 58 | 59 | Diorite | 0.11 | KSDD004 | 102 | 103 | Phyllite | 0.06 | |
| KSDD004 | 59 | 60 | Diorite | 0.05 | KSDD004 | 103 | 104 | Phyllite | 0.07 | |
| KSDD004 | 60 | 61 | Diorite | 0.04 | KSDD004 | 104 | 105 | Andesite | 0.14 | |
| KSDD004 | 61 | 62 | Diorite | 0.05 | KSDD004 | 105 | 106 | Andesite | 0.05 | |
| KSDD004 | 62 | 63 | Diorite | 0.05 | KSDD004 | 106 | 106 | Andesite | -999 | |
| KSDD004 | 63 | 64 | Diorite | 0.12 | KSDD004 | 106 | 107 | Andesite | 0.06 | |
| KSDD004 | 64 | 65 | Diorite | 0.11 | KSDD004 | 107 | 108 | Andesite | 0.77 | |
| KSDD004 | 65 | 66 | Diorite | 0.1 | KSDD004 | 108 | 109 | Andesite | 2.07 | |
| KSDD004 | 66 | 67 | Diorite | 0.06 | KSDD004 | 109 | 110 | Andesite | 0.24 | |
| KSDD004 | 67 | 68 | Diorite | 0.09 | KSDD004 | 110 | 110 | Andesite | 1.17 | |
| KSDD004 | 68 | 69 | Diorite | 0.05 | KSDD004 | 110 | 111 | Andesite | -999 | |
| KSDD004 | 69 | 69 | Diorite | 0.06 | KSDD004 | 111 | 112 | Andesite | 1.17 | |
| KSDD004 | 69 | 70 | Diorite | 0.1 | KSDD004 | 112 | 113 | Marble | 0.27 | |
| KSDD004 | 70 | 71 | Phyllite | 0.08 | KSDD004 | 113 | 114 | Marble | 0.79 | |
| KSDD004 | 71 | 72 | Phyllite | 0.08 | KSDD004 | 114 | 115 | Marble | 1.48 | |
| KSDD004 | 72 | 73 | Phyllite | 0.07 | KSDD004 | 115 | 115 | Marble | -999 | |
| KSDD004 | 73 | 74 | Phyllite | 0.05 | KSDD004 | 115 | 116 | Marble | 1.39 | |
| KSDD004 | 74 | 75 | Phyllite | 0.09 | KSDD004 | 116 | 117 | Marble | 0.76 | |
| KSDD004 | 75 | 76 | Phyllite | 0.04 | KSDD004 | 117 | 117 | Marble | -999 | |
| KSDD004 | 76 | 77 | Phyllite | 0.03 | KSDD004 | 117 | 117 | Marble | 3.61 | |
| KSDD004 | 77 | 79 | Phyllite | 0.03 | KSDD004 | 117 | 118 | Marble | 0.6 | |
| KSDD004 | 79 | 79 | Diorite | 0.04 | KSDD004 | 118 | 119 | Marble | 1.61 | |
| KSDD004 | 79 | 80 | Diorite | 0.05 | KSDD004 | 119 | 120 | Marble | 2.42 | |
| KSDD004 | 80 | 81 | Phyllite | 0.07 | KSDD004 | 120 | 121 | Marble | 1.21 | |
| KSDD004 | 81 | 82 | Phyllite | 0.06 | KSDD004 | 121 | 122 | Marble | 1.43 |
43
25 November 2022 ASX Announcement
ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD004 | 122 | 122 | Marble | 12.4 | KSDD004 | 164 | 165 | Phyllite | 0.03 | |
| KSDD004 | 122 | 123 | Marble | -999 | KSDD004 | 165 | 166 | Phyllite | 0.02 | |
| KSDD004 | 123 | 124 | Marble | 23.5 | KSDD004 | 166 | 167 | Phyllite | 0.05 | |
| KSDD004 | 124 | 125 | Marble | 1.61 | KSDD004 | 167 | 168 | Phyllite | 0.06 | |
| KSDD004 | 125 | 126 | Marble | 0.08 | KSDD004 | 168 | 169 | Phyllite | 0.04 | |
| KSDD004 | 126 | 127 | Marble | 0.39 | KSDD004 | 169 | 170 | Phyllite | 0.03 | |
| KSDD004 | 127 | 128 | Marble | 0.16 | KSDD004 | 170 | 171 | Phyllite | 0.03 | |
| KSDD004 | 128 | 129 | Marble | 0.03 | KSDD004 | 171 | 172 | Phyllite | 0.04 | |
| KSDD004 | 129 | 130 | Marble | 0.28 | KSDD004 | 172 | 173 | Phyllite | -999 | |
| KSDD004 | 130 | 131 | Marble | 0.13 | KSDD004 | 173 | 174 | Phyllite | 0.04 | |
| KSDD004 | 131 | 132 | Marble | 1.07 | KSDD004 | 174 | 175 | Phyllite | 0.04 | |
| KSDD004 | 132 | 133 | Marble | 0.1 | KSDD004 | 175 | 176 | Phyllite | 0.04 | |
| KSDD004 | 133 | 134 | Marble | 0.04 | KSDD004 | 176 | 177 | Phyllite | 0.03 | |
| KSDD004 | 134 | 135 | Marble | 0.06 | KSDD004 | 177 | 178 | Phyllite | 0.07 | |
| KSDD004 | 135 | 136 | Marble | 0.03 | KSDD004 | 178 | 179 | Phyllite | -999 | |
| KSDD004 | 136 | 136 | Marble | 0.15 | KSDD004 | 179 | 180 | Phyllite | 0.06 | |
| KSDD004 | 136 | 137 | Marble | -999 | KSDD004 | 180 | 182 | Phyllite | 0.03 | |
| KSDD004 | 137 | 138 | Marble | 0.03 | KSDD004 | 182 | 184 | Phyllite | 0.03 | |
| KSDD004 | 138 | 139 | Marble | 0.41 | KSDD004 | 184 | 186 | Phyllite | 0.03 | |
| KSDD004 | 139 | 140 | Marble | 0.03 | KSDD004 | 186 | 188 | Phyllite | 0.03 | |
| KSDD004 | 140 | 141 | Marble | 0.73 | KSDD004 | 188 | 190 | Phyllite | 0.04 | |
| KSDD004 | 141 | 142 | Marble | 0.45 | KSDD004 | 190 | 192 | Phyllite | 0.03 | |
| KSDD004 | 142 | 143 | Marble | 0.91 | KSDD004 | 192 | 194 | Phyllite | 0.04 | |
| KSDD004 | 143 | 144 | Marble | 0.03 | KSDD004 | 194 | 195 | Phyllite | 0.07 | |
| KSDD004 | 144 | 145 | Marble | 0.43 | KSDD004 | 195 | 196 | Phyllite | 0.06 | |
| KSDD004 | 145 | 146 | Marble | 0.12 | KSDD004 | 196 | 197 | Phyllite | 0.08 | |
| KSDD004 | 146 | 147 | Marble | 0.03 | KSDD004 | 197 | 198 | Phyllite | 0.13 | |
| KSDD004 | 147 | 148 | Marble | 0.16 | KSDD004 | 198 | 199 | Phyllite | 0.06 | |
| KSDD004 | 148 | 149 | Marble | 0.13 | KSDD004 | 199 | 200 | Phyllite | 0.05 | |
| KSDD004 | 149 | 150 | Phyllite | 0.1 | KSDD004 | 200 | 201 | Phyllite | 0.12 | |
| KSDD004 | 150 | 151 | Phyllite | 0.14 | KSDD004 | 201 | 203 | Phyllite | 0.06 | |
| KSDD004 | 151 | 152 | Phyllite | 0.11 | KSDD004 | 203 | 205 | Phyllite | 0.03 | |
| KSDD004 | 152 | 153 | Phyllite | 0.06 | KSDD004 | 205 | 207 | Phyllite | 0.05 | |
| KSDD004 | 153 | 154 | Phyllite | 0.11 | KSDD004 | 207 | 209 | Phyllite | 0.06 | |
| KSDD004 | 154 | 155 | Phyllite | 0.17 | KSDD004 | 209 | 211 | Phyllite | 0.09 | |
| KSDD004 | 155 | 156 | Phyllite | 0.16 | KSDD004 | 211 | 213 | Phyllite | 0.41 | |
| KSDD004 | 156 | 157 | Phyllite | 0.06 | KSDD004 | 213 | 215 | Phyllite | 0.33 | |
| KSDD004 | 157 | 158 | Phyllite | 0.07 | KSDD004 | 215 | 216 | Phyllite | 0.07 | |
| KSDD004 | 158 | 159 | Phyllite | 0.16 | KSDD004 | 216 | 217 | Phyllite | 0.29 | |
| KSDD004 | 159 | 160 | Phyllite | 0.05 | KSDD004 | 217 | 218 | Phyllite | 0.24 | |
| KSDD004 | 160 | 161 | Phyllite | 0.03 | KSDD004 | 218 | 219 | Phyllite | 0.26 | |
| KSDD004 | 161 | 162 | Phyllite | 0.04 | KSDD004 | 219 | 221 | Phyllite | 0.13 | |
| KSDD004 | 162 | 163 | Phyllite | 0.05 | KSDD004 | 221 | 223 | Phyllite | 0.17 | |
| KSDD004 | 163 | 164 | Phyllite | 0.05 | KSDD004 | 223 | 224 | Phyllite | 0.21 | |
| KSDD004 | 164 | 164 | Phyllite | 0.03 | KSDD004 | 224 | 225 | Phyllite | 0.18 |
44
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD004 | 225 | 226 | Phyllite | 0.21 | KSDD004 | 268 | 269 | Phyllite | 0.38 | |
| KSDD004 | 226 | 227 | Phyllite | 0.19 | KSDD004 | 269 | 270 | Phyllite | 0.48 | |
| KSDD004 | 227 | 228 | Phyllite | 0.15 | KSDD004 | 270 | 271 | Phyllite | 0.26 | |
| KSDD004 | 228 | 229 | Phyllite | 0.21 | KSDD004 | 271 | 272 | Phyllite | 0.12 | |
| KSDD004 | 229 | 230 | Phyllite | 0.29 | KSDD004 | 272 | 273 | Phyllite | 0.32 | |
| KSDD004 | 230 | 231 | Phyllite | 0.33 | KSDD004 | 273 | 274 | Phyllite | 0.12 | |
| KSDD004 | 231 | 232 | Phyllite | 0.31 | KSDD004 | 274 | 275 | Phyllite | 0.14 | |
| KSDD004 | 232 | 233 | Phyllite | 0.43 | KSDD004 | 275 | 276 | Phyllite | 0.12 | |
| KSDD004 | 233 | 234 | Phyllite | 0.26 | KSDD004 | 276 | 277 | Phyllite | 0.23 | |
| KSDD004 | 234 | 235 | Phyllite | 0.38 | KSDD004 | 277 | 278 | Phyllite | 0.27 | |
| KSDD004 | 235 | 236 | Phyllite | 0.11 | KSDD004 | 278 | 279 | Phyllite | 0.07 | |
| KSDD004 | 236 | 237 | Phyllite | 0.05 | KSDD004 | 279 | 279 | Phyllite | 0.12 | |
| KSDD004 | 237 | 238 | Phyllite | 0.04 | KSDD004 | 279 | 280 | Phyllite | -999 | |
| KSDD004 | 238 | 239 | Phyllite | 0.07 | KSDD004 | 280 | 281 | Phyllite | 0.1 | |
| KSDD004 | 239 | 240 | Phyllite | 0.04 | KSDD004 | 281 | 281 | Phyllite | 0.19 | |
| KSDD004 | 240 | 241 | Phyllite | 0.11 | KSDD004 | 281 | 282 | Phyllite | 0.17 | |
| KSDD004 | 241 | 242 | Phyllite | 0.03 | KSDD004 | 282 | 283 | Phyllite | 0.2 | |
| KSDD004 | 242 | 243 | Phyllite | 0.06 | KSDD004 | 283 | 283 | Phyllite | -999 | |
| KSDD004 | 243 | 244 | Phyllite | 0.04 | KSDD004 | 283 | 284 | Phyllite | 0.2 | |
| KSDD004 | 244 | 245 | Phyllite | 0.09 | KSDD004 | 284 | 285 | Phyllite | 0.35 | |
| KSDD004 | 245 | 246 | Phyllite | 0.25 | KSDD004 | 285 | 286 | Phyllite | 0.49 | |
| KSDD004 | 246 | 247 | Phyllite | 0.35 | KSDD004 | 286 | 287 | Breccia | -999 | |
| KSDD004 | 247 | 248 | Phyllite | 0.21 | KSDD004 | 287 | 287 | Breccia | 0.48 | |
| KSDD004 | 248 | 249 | Phyllite | 0.42 | KSDD004 | 287 | 288 | Breccia | 0.64 | |
| KSDD004 | 249 | 250 | Phyllite | 1 | KSDD004 | 288 | 288 | Breccia | 3.75 | |
| KSDD004 | 250 | 250 | Phyllite | -999 | KSDD004 | 288 | 289 | Phyllite | 0.43 | |
| KSDD004 | 250 | 251 | Phyllite | 0.32 | KSDD004 | 289 | 290 | Phyllite | 0.09 | |
| KSDD004 | 251 | 252 | Diorite | 0.1 | KSDD004 | 290 | 291 | Phyllite | 0.07 | |
| KSDD004 | 252 | 253 | Diorite | 0.03 | KSDD004 | 291 | 293 | Phyllite | 0.22 | |
| KSDD004 | 253 | 254 | Diorite | 0.07 | KSDD004 | 293 | 294 | Phyllite | 0.12 | |
| KSDD004 | 254 | 255 | Diorite | 0.01 | KSDD004 | 294 | 295 | Phyllite | 0.03 | |
| KSDD004 | 255 | 256 | Diorite | 0.03 | KSDD004 | 295 | 297 | Phyllite | 0.06 | |
| KSDD004 | 256 | 257 | Phyllite | 0.1 | KSDD004 | 297 | 299 | Phyllite | 0.95 | |
| KSDD004 | 257 | 258 | Phyllite | 0.14 | KSDD004 | 299 | 300 | Phyllite | 0.19 | |
| KSDD004 | 258 | 259 | Phyllite | 0.26 | KSDD004 | 300 | 301 | Phyllite | 0.27 | |
| KSDD004 | 259 | 260 | Phyllite | 0.18 | KSDD004 | 301 | 303 | Phyllite | 0.04 | |
| KSDD004 | 260 | 261 | Phyllite | 0.21 | KSDD004 | 303 | 305 | Phyllite | 0.03 | |
| KSDD004 | 261 | 261 | Diorite | 0.06 | KSDD004 | 305 | 306 | Phyllite | 0.04 | |
| KSDD004 | 261 | 262 | Diorite | 0.12 | KSDD004 | 306 | 308 | Phyllite | 0.25 | |
| KSDD004 | 262 | 263 | Diorite | 0.14 | KSDD004 | 308 | 309 | Phyllite | 0.14 | |
| KSDD004 | 263 | 264 | Diorite | 0.34 | KSDD004 | 309 | 310 | Phyllite | 0.92 | |
| KSDD004 | 264 | 265 | Diorite | 0.17 | KSDD004 | 310 | 312 | Phyllite | 0.05 | |
| KSDD004 | 265 | 266 | Diorite | 0.14 | KSDD004 | 312 | 313 | Phyllite | 0.14 | |
| KSDD004 | 266 | 267 | Diorite | 0.4 | KSDD004 | 313 | 315 | Phyllite | 0.2 | |
| KSDD004 | 267 | 268 | Phyllite | 0.28 | KSDD004 | 315 | 316 | Phyllite | 0.18 |
45
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD004 | 316 | 318 | Phyllite | 0.25 | KSDD005 | 3.1 | 4.4 | Saprolite | 0.01 | |
| KSDD004 | 318 | 320 | Phyllite | 0.08 | KSDD005 | 4.4 | 5.9 | Saprolite | 0.01 | |
| KSDD004 | 320 | 321 | Phyllite | 0.09 | KSDD005 | 5.9 | 7.4 | Saprolite | 0.01 | |
| KSDD004 | 321 | 322 | Fault | 0.1 | KSDD005 | 7.4 | 8.9 | Saprock | 0.02 | |
| KSDD004 | 322 | 323 | Fault | 0.17 | KSDD005 | 8.9 | 10 | Saprock | -999 | |
| KSDD004 | 323 | 324 | Fault | 0.66 | KSDD005 | 10 | 12 | Saprock | -999 | |
| KSDD004 | 324 | 325 | Fault | 3.86 | KSDD005 | 12 | 13 | Saprock | 0.01 | |
| KSDD004 | 325 | 326 | Fault | 0.74 | KSDD005 | 13 | 14 | Saprock | 0.05 | |
| KSDD004 | 326 | 327 | Fault | 0.21 | KSDD005 | 14 | 16 | Mudstone | 0.01 | |
| KSDD004 | 327 | 329 | Phyllite | 0.24 | KSDD005 | 16 | 18 | Mudstone | 0.01 | |
| KSDD004 | 329 | 330 | Phyllite | 0.12 | KSDD005 | 18 | 21 | Mudstone | 0.41 | |
| KSDD004 | 330 | 331 | Fault | 0.09 | KSDD005 | 21 | 22 | Mudstone | 0.01 | |
| KSDD004 | 331 | 332 | Fault | 0.07 | KSDD005 | 22 | 24 | Mudstone | 0.01 | |
| KSDD004 | 332 | 333 | Fault | 0.12 | KSDD005 | 24 | 25 | Mudstone | -999 | |
| KSDD004 | 333 | 334 | Fault | 0.17 | KSDD005 | 25 | 27 | Mudstone | 0.01 | |
| KSDD004 | 334 | 335 | Fault | 0.14 | KSDD005 | 27 | 28 | Mudstone | 0.01 | |
| KSDD004 | 335 | 336 | Fault | 0.14 | KSDD005 | 28 | 30 | Mudstone | -999 | |
| KSDD004 | 336 | 337 | Phyllite | 0.03 | KSDD005 | 30 | 32 | Mudstone | 0.01 | |
| KSDD004 | 337 | 339 | Phyllite | 0.7 | KSDD005 | 32 | 34 | Mudstone | 0.01 | |
| KSDD004 | 339 | 341 | Phyllite | 0.03 | KSDD005 | 34 | 36 | Mudstone | 0.01 | |
| KSDD004 | 341 | 343 | Phyllite | 0.03 | KSDD005 | 36 | 37 | Mudstone | 0.01 | |
| KSDD004 | 343 | 345 | Phyllite | 0.04 | KSDD005 | 37 | 38 | Mudstone | 0.01 | |
| KSDD004 | 345 | 347 | Phyllite | 0.05 | KSDD005 | 38 | 39 | Mudstone | -999 | |
| KSDD004 | 347 | 349 | Phyllite | 0.16 | KSDD005 | 39 | 41 | Mudstone | 0.01 | |
| KSDD004 | 349 | 351 | Phyllite | 0.04 | KSDD005 | 41 | 42 | Mudstone | 0.01 | |
| KSDD004 | 351 | 353 | Phyllite | 0.05 | KSDD005 | 42 | 43 | Mudstone | 0.01 | |
| KSDD004 | 353 | 355 | Phyllite | 0.17 | KSDD005 | 43 | 44 | Mudstone | 0.01 | |
| KSDD004 | 355 | 356 | Phyllite | 0.03 | KSDD005 | 44 | 45 | Mudstone | 0.01 | |
| KSDD004 | 356 | 357 | Phyllite | -999 | KSDD005 | 45 | 46 | Mudstone | 0.01 | |
| KSDD004 | 357 | 358 | Fault | 0.05 | KSDD005 | 46 | 48 | Mudstone | 0.01 | |
| KSDD004 | 358 | 359 | Phyllite | 0.45 | KSDD005 | 48 | 50 | Mudstone | 0.01 | |
| KSDD004 | 359 | 360 | Phyllite | -999 | KSDD005 | 50 | 52 | Mudstone | 0.01 | |
| KSDD004 | 360 | 360 | Phyllite | 0.04 | KSDD005 | 52 | 54 | Mudstone | -999 | |
| KSDD004 | 360 | 362 | Phyllite | 0.05 | KSDD005 | 54 | 56 | Fault | 0.03 | |
| KSDD004 | 362 | 364 | Phyllite | 0.05 | KSDD005 | 56 | 57 | Fault | -999 | |
| KSDD004 | 364 | 366 | Phyllite | 0.05 | KSDD005 | 57 | 59 | Fault | 0.01 | |
| KSDD004 | 366 | 368 | Phyllite | 0.06 | KSDD005 | 59 | 60 | Fault | -999 | |
| KSDD004 | 368 | 368 | Fault | 3.91 | KSDD005 | 60 | 61 | Fault | 0.02 | |
| KSDD004 | 368 | 370 | Fault | 0.1 | KSDD005 | 61 | 62 | Skarn | 0.07 | |
| KSDD004 | 370 | 372 | Phyllite | 0.14 | KSDD005 | 62 | 63 | Massive Sulfide | 0.16 | |
| KSDD004 | 372 | 374 | Phyllite | 0.13 | KSDD005 | 63 | 63 | Skarn | 0.04 | |
| KSDD004 | 374 | 376 | Phyllite | 0.28 | KSDD005 | 63 | 64 | Massive Sulfide | 0.19 | |
| KSDD004 | 376 | 377 | Fault | 0.11 | KSDD005 | 64 | 65 | Massive Sulfide | 0.92 | |
| KSDD005 | 0 | 1.6 | Clay | 0.01 | KSDD005 | 65 | 67 | Skarn | 0.22 | |
| KSDD005 | 1.6 | 3.1 | Saprolite | -999 | KSDD005 | 67 | 68 | Skarn | 0.04 |
46
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD005 | 68 | 69 | Skarn | 0.07 | KSDD006 | 14 | 17 | Saprock | -999 | |
| KSDD005 | 69 | 70 | Skarn | 0.21 | KSDD006 | 17 | 19 | Saprock | 0.01 | |
| KSDD005 | 70 | 71 | Skarn | -999 | KSDD006 | 19 | 20 | Mudstone | 0.34 | |
| KSDD005 | 71 | 72 | Skarn | 0.32 | KSDD006 | 20 | 21 | Mudstone | 0.08 | |
| KSDD005 | 72 | 73 | Skarn | 0.05 | KSDD006 | 21 | 22 | Mudstone | 0.01 | |
| KSDD005 | 73 | 73 | Skarn | 0.25 | KSDD006 | 22 | 23 | Mudstone | -999 | |
| KSDD005 | 73 | 74 | Skarn | 0.11 | KSDD006 | 23 | 24 | Mudstone | 0.02 | |
| KSDD005 | 74 | 75 | Skarn | 0.42 | KSDD006 | 24 | 25 | Mudstone | 0.02 | |
| KSDD005 | 75 | 76 | Skarn | 0.09 | KSDD006 | 25 | 26 | Mudstone | 0.03 | |
| KSDD005 | 76 | 77 | Skarn | 0.14 | KSDD006 | 26 | 27 | Mudstone | 0.01 | |
| KSDD005 | 77 | 78 | Skarn | 0.03 | KSDD006 | 27 | 28 | Mudstone | 0.01 | |
| KSDD005 | 78 | 79 | Skarn | 0.03 | KSDD006 | 28 | 29 | Mudstone | 0.01 | |
| KSDD005 | 79 | 80 | Skarn | 0.16 | KSDD006 | 29 | 30 | Mudstone | 0.01 | |
| KSDD005 | 80 | 81 | Skarn | 0.04 | KSDD006 | 30 | 31 | Mudstone | 0.01 | |
| KSDD005 | 81 | 81 | Skarn | -999 | KSDD006 | 31 | 32 | Mudstone | 0.01 | |
| KSDD005 | 81 | 82 | Skarn | 0.05 | KSDD006 | 32 | 34 | Mudstone | 0.02 | |
| KSDD005 | 82 | 83 | Skarn | 0.09 | KSDD006 | 34 | 35 | Mudstone | 0.01 | |
| KSDD005 | 83 | 83 | Skarn | -999 | KSDD006 | 35 | 36 | Mudstone | -999 | |
| KSDD005 | 83 | 84 | Phyllite | 0.32 | KSDD006 | 36 | 37 | Mudstone | -999 | |
| KSDD005 | 84 | 85 | Phyllite | 0.27 | KSDD006 | 37 | 38 | Mudstone | 0.01 | |
| KSDD005 | 85 | 86 | Phyllite | 0.16 | KSDD006 | 38 | 39 | Mudstone | 0.01 | |
| KSDD005 | 86 | 87 | Phyllite | 0.08 | KSDD006 | 39 | 40 | Mudstone | -999 | |
| KSDD005 | 87 | 88 | Phyllite | 0.24 | KSDD006 | 40 | 41 | Mudstone | -999 | |
| KSDD005 | 88 | 89 | Phyllite | 0.57 | KSDD006 | 41 | 42 | Mudstone | 0.01 | |
| KSDD005 | 89 | 89 | Phyllite | -999 | KSDD006 | 42 | 43 | Mudstone | -999 | |
| KSDD005 | 89 | 90 | Phyllite | 0.78 | KSDD006 | 43 | 44 | Mudstone | 0.01 | |
| KSDD005 | 90 | 91 | Phyllite | 0.04 | KSDD006 | 44 | 45 | Mudstone | -999 | |
| KSDD005 | 91 | 92 | Phyllite | 0.54 | KSDD006 | 45 | 46 | Mudstone | 0.01 | |
| KSDD005 | 92 | 93 | Phyllite | 0.53 | KSDD006 | 46 | 47 | Mudstone | 0.01 | |
| KSDD005 | 93 | 94 | Phyllite | 0.18 | KSDD006 | 47 | 48 | Mudstone | 0.01 | |
| KSDD005 | 94 | 95 | Phyllite | 0.09 | KSDD006 | 48 | 49 | Mudstone | 0.03 | |
| KSDD005 | 95 | 95 | Phyllite | -999 | KSDD006 | 49 | 50 | Phyllite | 0.03 | |
| KSDD005 | 95 | 96 | Phyllite | 0.1 | KSDD006 | 50 | 51 | Shear zone | 0.01 | |
| KSDD005 | 96 | 97 | Phyllite | 0.08 | KSDD006 | 51 | 53 | Shear zone | 0.03 | |
| KSDD005 | 97 | 99 | Phyllite | 0.42 | KSDD006 | 53 | 54 | Shear zone | 0.43 | |
| KSDD006 | 0 | 0.8 | Saprolite | -999 | KSDD006 | 54 | 55 | Shear zone | 0.35 | |
| KSDD006 | 0.8 | 2.4 | Saprolite | 0.02 | KSDD006 | 55 | 56 | Phyllite | 0.39 | |
| KSDD006 | 2.4 | 4.3 | Saprolite | 0.01 | KSDD006 | 56 | 57 | Phyllite | 0.2 | |
| KSDD006 | 4.3 | 5.3 | Saprolite | 0.01 | KSDD006 | 57 | 58 | Phyllite | 0.13 | |
| KSDD006 | 5.3 | 6.8 | Saprolite | -999 | KSDD006 | 58 | 59 | Phyllite | 0.19 | |
| KSDD006 | 6.8 | 8 | Saprolite | 0.02 | KSDD006 | 59 | 60 | Phyllite | 0.07 | |
| KSDD006 | 8 | 10 | Saprolite | 0.01 | KSDD006 | 60 | 61 | Phyllite | 0.06 | |
| KSDD006 | 10 | 12 | Saprolite | 0.01 | KSDD006 | 61 | 62 | Phyllite | 0.06 | |
| KSDD006 | 12 | 13 | Saprock | -999 | KSDD006 | 62 | 63 | Phyllite | 0.08 | |
| KSDD006 | 13 | 14 | Saprock | -999 | KSDD006 | 63 | 64 | Phyllite | 0.05 |
47
25 November 2022 ASX Announcement
ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD006 | 64 | 65 | Phyllite | 0.04 | KSDD006 | 110 | 111 | Phyllite | 0.06 | |
| KSDD006 | 65 | 66 | Phyllite | 0.05 | KSDD006 | 111 | 112 | Phyllite | 0.07 | |
| KSDD006 | 66 | 67 | Phyllite | 0.18 | KSDD006 | 112 | 113 | Phyllite | 0.06 | |
| KSDD006 | 67 | 68 | Phyllite | 0.28 | KSDD006 | 113 | 114 | Phyllite | 0.05 | |
| KSDD006 | 68 | 69 | Phyllite | 0.25 | KSDD006 | 114 | 115 | Breccia | 0.2 | |
| KSDD006 | 69 | 70 | Phyllite | 0.24 | KSDD006 | 115 | 116 | Breccia | 0.23 | |
| KSDD006 | 70 | 71 | Phyllite | 0.25 | KSDD006 | 116 | 117 | Phyllite | 0.08 | |
| KSDD006 | 71 | 72 | Phyllite | 0.21 | KSDD006 | 117 | 118 | Phyllite | 0.1 | |
| KSDD006 | 72 | 73 | Phyllite | 0.1 | KSDD006 | 118 | 119 | Phyllite | 0.09 | |
| KSDD006 | 73 | 74 | Phyllite | 0.07 | KSDD006 | 119 | 120 | Phyllite | 0.09 | |
| KSDD006 | 74 | 75 | Phyllite | 0.16 | KSDD006 | 120 | 121 | Fault | 0.11 | |
| KSDD006 | 75 | 76 | Phyllite | 0.09 | KSDD006 | 121 | 122 | Fault | 0.08 | |
| KSDD006 | 76 | 77 | Phyllite | 0.08 | KSDD006 | 122 | 123 | Fault | 0.04 | |
| KSDD006 | 77 | 78 | Phyllite | 0.16 | KSDD006 | 123 | 124 | Fault | 0.07 | |
| KSDD006 | 78 | 79 | Phyllite | 0.09 | KSDD006 | 124 | 125 | Fault | 0.06 | |
| KSDD006 | 79 | 80 | Phyllite | 0.1 | KSDD006 | 125 | 127 | Fault | 0.05 | |
| KSDD006 | 80 | 81 | Phyllite | 0.34 | KSDD006 | 127 | 128 | Phyllite | 0.04 | |
| KSDD006 | 81 | 82 | Phyllite | 0.29 | KSDD006 | 128 | 129 | Diorite | 0.03 | |
| KSDD006 | 82 | 83 | Phyllite | 0.19 | KSDD006 | 129 | 130 | Phyllite | 0.05 | |
| KSDD006 | 83 | 84 | Phyllite | 0.18 | KSDD006 | 130 | 131 | Diorite | 0.06 | |
| KSDD006 | 84 | 85 | Phyllite | 0.16 | KSDD006 | 131 | 132 | Phyllite | 0.04 | |
| KSDD006 | 85 | 86 | Phyllite | 0.11 | KSDD006 | 132 | 133 | Phyllite | 0.04 | |
| KSDD006 | 86 | 87 | Phyllite | 0.06 | KSDD006 | 133 | 134 | Phyllite | 0.07 | |
| KSDD006 | 87 | 88 | Phyllite | 0.07 | KSDD006 | 134 | 135 | Phyllite | 0.07 | |
| KSDD006 | 88 | 89 | Phyllite | 0.08 | KSDD006 | 135 | 136 | Diorite | 0.05 | |
| KSDD006 | 89 | 90 | Phyllite | 0.05 | KSDD006 | 136 | 137 | Phyllite | 0.03 | |
| KSDD006 | 90 | 91 | Phyllite | 0.08 | KSDD006 | 137 | 138 | Phyllite | 0.03 | |
| KSDD006 | 91 | 92 | Phyllite | 0.12 | KSDD006 | 138 | 139 | Phyllite | 0.03 | |
| KSDD006 | 92 | 93 | Phyllite | 0.18 | KSDD006 | 139 | 140 | Phyllite | 0.04 | |
| KSDD006 | 93 | 94 | Phyllite | 0.32 | KSDD006 | 140 | 141 | Phyllite | 0.05 | |
| KSDD006 | 94 | 95 | Phyllite | 0.3 | KSDD006 | 141 | 142 | Phyllite | 0.04 | |
| KSDD006 | 95 | 96 | Phyllite | 0.32 | KSDD006 | 142 | 143 | Phyllite | 0.03 | |
| KSDD006 | 96 | 97 | Phyllite | 0.09 | KSDD006 | 143 | 144 | Phyllite | 0.03 | |
| KSDD006 | 97 | 98 | Phyllite | 0.1 | KSDD006 | 144 | 145 | Phyllite | 0.02 | |
| KSDD006 | 98 | 99 | Phyllite | 0.12 | KSDD006 | 145 | 146 | Phyllite | 0.03 | |
| KSDD006 | 99 | 100 | Phyllite | 0.12 | KSDD006 | 146 | 147 | Phyllite | 0.03 | |
| KSDD006 | 100 | 101 | Phyllite | 0.06 | KSDD006 | 147 | 148 | Phyllite | 0.03 | |
| KSDD006 | 101 | 102 | Phyllite | 0.15 | KSDD006 | 148 | 149 | Fault | 0.02 | |
| KSDD006 | 102 | 103 | Phyllite | 0.09 | KSDD006 | 149 | 150 | Fault | 0.02 | |
| KSDD006 | 103 | 104 | Phyllite | 0.09 | KSDD006 | 150 | 151 | Breccia | 0.03 | |
| KSDD006 | 104 | 105 | Phyllite | 0.06 | KSDD006 | 151 | 152 | Breccia | 0.06 | |
| KSDD006 | 105 | 106 | Phyllite | 0.08 | KSDD006 | 152 | 153 | Breccia | 0.03 | |
| KSDD006 | 106 | 107 | Phyllite | 0.21 | KSDD006 | 153 | 154 | Breccia | 0.04 | |
| KSDD006 | 107 | 109 | Phyllite | 0.11 | KSDD006 | 154 | 155 | Breccia | 0.07 | |
| KSDD006 | 109 | 110 | Phyllite | 0.08 | KSDD006 | 155 | 156 | Breccia | 0.03 |
48
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD006 | 156 | 157 | Breccia | 0.11 | KSDD006 | 200 | 201 | Diorite | 0.09 | |
| KSDD006 | 157 | 158 | Breccia | 0.05 | KSDD006 | 201 | 202 | Diorite | 0.06 | |
| KSDD006 | 158 | 159 | Monzogabbro | 0.08 | KSDD006 | 202 | 203 | Diorite | 0.02 | |
| KSDD006 | 159 | 160 | Monzogabbro | 0.05 | KSDD006 | 203 | 204 | Diorite | 0.02 | |
| KSDD006 | 160 | 161 | Monzogabbro | 0.07 | KSDD006 | 204 | 205 | Diorite | -999 | |
| KSDD006 | 161 | 162 | Monzogabbro | 0.03 | KSDD006 | 205 | 206 | Diorite | 0.04 | |
| KSDD006 | 162 | 163 | Monzogabbro | 0.04 | KSDD006 | 206 | 207 | Diorite | 0.19 | |
| KSDD006 | 163 | 164 | Monzogabbro | 0.05 | KSDD006 | 207 | 208 | Diorite | 0.11 | |
| KSDD006 | 164 | 165 | Monzogabbro | 0.25 | KSDD006 | 208 | 209 | Diorite | 0.14 | |
| KSDD006 | 165 | 166 | Monzogabbro | 0.04 | KSDD006 | 209 | 210 | Diorite | 0.12 | |
| KSDD006 | 166 | 167 | Monzogabbro | 0.08 | KSDD006 | 210 | 211 | Diorite | 0.01 | |
| KSDD006 | 167 | 168 | Monzogabbro | 0.7 | KSDD006 | 211 | 212 | Diorite | -999 | |
| KSDD006 | 168 | 169 | Monzogabbro | 0.42 | KSDD006 | 212 | 213 | Diorite | 0.01 | |
| KSDD006 | 169 | 170 | Monzogabbro | 0.72 | KSDD006 | 213 | 214 | Diorite | 0.01 | |
| KSDD006 | 170 | 171 | Monzogabbro | 0.86 | KSDD006 | 214 | 215 | Diorite | 0.01 | |
| KSDD006 | 171 | 172 | Monzogabbro | 0.05 | KSDD006 | 215 | 216 | Diorite | -999 | |
| KSDD006 | 172 | 173 | Monzogabbro | 0.06 | KSDD006 | 216 | 217 | Diorite | 0.01 | |
| KSDD006 | 173 | 174 | Monzogabbro | 0.03 | KSDD006 | 217 | 218 | Diorite | 0.01 | |
| KSDD006 | 174 | 175 | Monzogabbro | 0.15 | KSDD006 | 218 | 219 | Diorite | 0.01 | |
| KSDD006 | 175 | 176 | Monzogabbro | 0.04 | KSDD006 | 219 | 220 | Diorite | 0.01 | |
| KSDD006 | 176 | 177 | Monzogabbro | 0.1 | KSDD006 | 220 | 221 | Diorite | 0.01 | |
| KSDD006 | 177 | 178 | Monzogabbro | 0.06 | KSDD006 | 221 | 222 | Diorite | -999 | |
| KSDD006 | 178 | 179 | Monzogabbro | 0.04 | KSDD006 | 222 | 223 | Diorite | 0.01 | |
| KSDD006 | 179 | 180 | Monzogabbro | 0.07 | KSDD006 | 223 | 224 | Diorite | 0.01 | |
| KSDD006 | 180 | 181 | Monzogabbro | 0.07 | KSDD006 | 224 | 225 | Diorite | 0.01 | |
| KSDD006 | 181 | 182 | Monzogabbro | 0.04 | KSDD006 | 225 | 226 | Diorite | 0.01 | |
| KSDD006 | 182 | 183 | Monzogabbro | 0.02 | KSDD006 | 226 | 227 | Diorite | 0.01 | |
| KSDD006 | 183 | 184 | Monzogabbro | 0.07 | KSDD006 | 227 | 228 | Diorite | 0.02 | |
| KSDD006 | 184 | 185 | Diorite | 0.03 | KSDD006 | 228 | 229 | Diorite | -999 | |
| KSDD006 | 185 | 186 | Diorite | 0.02 | KSDD006 | 229 | 230 | Diorite | 0.01 | |
| KSDD006 | 186 | 187 | Diorite | 0.02 | KSDD006 | 230 | 231 | Diorite | -999 | |
| KSDD006 | 187 | 188 | Diorite | 0.03 | KSDD006 | 231 | 232 | Diorite | -999 | |
| KSDD006 | 188 | 189 | Skarn | 0.06 | KSDD006 | 232 | 233 | Diorite | 0.01 | |
| KSDD006 | 189 | 191 | Skarn | -999 | KSDD006 | 233 | 234 | Diorite | 0.01 | |
| KSDD006 | 191 | 191 | Skarn | 0.17 | KSDD006 | 234 | 235 | Diorite | 0.01 | |
| KSDD006 | 191 | 192 | Skarn | 0.02 | KSDD006 | 235 | 236 | Diorite | 0.01 | |
| KSDD006 | 192 | 194 | Skarn | -999 | KSDD006 | 236 | 237 | Diorite | 0.01 | |
| KSDD006 | 194 | 195 | Skarn | 0.13 | KSDD006 | 237 | 238 | Diorite | -999 | |
| KSDD006 | 195 | 196 | Skarn | 0.1 | KSDD006 | 238 | 239 | Diorite | 0.02 | |
| KSDD006 | 196 | 197 | Skarn | 0.4 | KSDD006 | 239 | 240 | Diorite | 0.01 | |
| KSDD006 | 197 | 197 | Skarn | -999 | KSDD006 | 240 | 241 | Diorite | 0.01 | |
| KSDD006 | 197 | 198 | Skarn | 0.21 | KSDD006 | 241 | 242 | Diorite | -999 | |
| KSDD006 | 198 | 199 | Skarn | 0.03 | KSDD006 | 242 | 243 | Diorite | -999 | |
| KSDD006 | 199 | 199 | Diorite | -999 | KSDD006 | 243 | 244 | Diorite | 0.01 | |
| KSDD006 | 199 | 200 | Diorite | 0.28 | KSDD006 | 244 | 245 | Diorite | -999 |
49
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD006 | 245 | 246 | Diorite | 0.01 | KSDD006 | 290 | 291 | Diorite | 0.01 | |
| KSDD006 | 246 | 247 | Diorite | 0.01 | KSDD006 | 291 | 292 | Diorite | -999 | |
| KSDD006 | 247 | 248 | Diorite | 0.01 | KSDD006 | 292 | 293 | Diorite | 0.01 | |
| KSDD006 | 248 | 249 | Diorite | 0.01 | KSDD006 | 293 | 294 | Diorite | 0.01 | |
| KSDD006 | 249 | 250 | Diorite | 0.01 | KSDD006 | 294 | 295 | Diorite | 0.01 | |
| KSDD006 | 250 | 251 | Diorite | 0.01 | KSDD006 | 295 | 296 | Diorite | 0.01 | |
| KSDD006 | 251 | 252 | Diorite | 0.01 | KSDD006 | 296 | 297 | Diorite | 0.02 | |
| KSDD006 | 252 | 253 | Diorite | 0.01 | KSDD006 | 297 | 298 | Diorite | 0.01 | |
| KSDD006 | 253 | 254 | Diorite | 0.02 | KSDD006 | 298 | 299 | Diorite | -999 | |
| KSDD006 | 254 | 255 | Diorite | 0.01 | KSDD006 | 299 | 300 | Diorite | -999 | |
| KSDD006 | 255 | 256 | Diorite | 0.01 | KSDD006 | 300 | 301 | Diorite | 0.01 | |
| KSDD006 | 256 | 257 | Diorite | 0.01 | KSDD006 | 301 | 302 | Diorite | 0.01 | |
| KSDD006 | 257 | 258 | Diorite | 0.01 | KSDD006 | 302 | 303 | Diorite | 0.01 | |
| KSDD006 | 258 | 259 | Diorite | 0.01 | KSDD006 | 303 | 304 | Diorite | -999 | |
| KSDD006 | 259 | 260 | Diorite | 0.01 | KSDD006 | 304 | 305 | Diorite | 0.01 | |
| KSDD006 | 260 | 261 | Diorite | -999 | KSDD006 | 305 | 306 | Diorite | 0.01 | |
| KSDD006 | 261 | 262 | Diorite | 0.01 | KSDD006 | 306 | 307 | Diorite | 0.01 | |
| KSDD006 | 262 | 263 | Diorite | 0.01 | KSDD006 | 307 | 308 | Diorite | 0.08 | |
| KSDD006 | 263 | 264 | Diorite | 0.01 | KSDD006 | 308 | 309 | Diorite | 0.17 | |
| KSDD006 | 264 | 265 | Diorite | 0.01 | KSDD006 | 309 | 310 | Diorite | 0.69 | |
| KSDD006 | 265 | 266 | Diorite | 0.01 | KSDD006 | 310 | 311 | Diorite | 0.08 | |
| KSDD006 | 266 | 267 | Diorite | -999 | KSDD006 | 311 | 312 | Diorite | 0.01 | |
| KSDD006 | 267 | 268 | Diorite | 0.02 | KSDD006 | 312 | 313 | Diorite | 0.01 | |
| KSDD006 | 268 | 269 | Diorite | 0.01 | KSDD006 | 313 | 314 | Diorite | -999 | |
| KSDD006 | 269 | 270 | Diorite | 0.01 | KSDD006 | 314 | 315 | Diorite | -999 | |
| KSDD006 | 270 | 271 | Diorite | 0.01 | KSDD006 | 315 | 316 | Diorite | -999 | |
| KSDD006 | 271 | 272 | Diorite | 0.01 | KSDD006 | 316 | 317 | Phyllite | -999 | |
| KSDD006 | 272 | 273 | Diorite | 0.01 | KSDD006 | 317 | 318 | Phyllite | 0.03 | |
| KSDD006 | 273 | 274 | Diorite | 0.01 | KSDD006 | 318 | 319 | Phyllite | 0.01 | |
| KSDD006 | 274 | 275 | Diorite | -999 | KSDD006 | 319 | 320 | Phyllite | 0.01 | |
| KSDD006 | 275 | 276 | Diorite | 0.01 | KSDD006 | 320 | 321 | Phyllite | 0.01 | |
| KSDD006 | 276 | 277 | Diorite | 0.03 | KSDD006 | 321 | 322 | Phyllite | 0.01 | |
| KSDD006 | 277 | 278 | Diorite | 0.02 | KSDD006 | 322 | 323 | Phyllite | -999 | |
| KSDD006 | 278 | 279 | Diorite | 0.02 | KSDD006 | 323 | 324 | Phyllite | 0.01 | |
| KSDD006 | 279 | 280 | Diorite | 0.01 | KSDD006 | 324 | 325 | Phyllite | 0.02 | |
| KSDD006 | 280 | 281 | Diorite | 0.01 | KSDD006 | 325 | 326 | Phyllite | -999 | |
| KSDD006 | 281 | 282 | Diorite | 0.01 | KSDD006 | 326 | 327 | Phyllite | -999 | |
| KSDD006 | 282 | 283 | Diorite | 0.01 | KSDD006 | 327 | 328 | Phyllite | -999 | |
| KSDD006 | 283 | 284 | Diorite | 0.02 | KSDD006 | 328 | 329 | Phyllite | -999 | |
| KSDD006 | 284 | 285 | Diorite | 0.02 | KSDD006 | 329 | 330 | Phyllite | -999 | |
| KSDD006 | 285 | 286 | Diorite | 0.01 | KSDD006 | 330 | 331 | Phyllite | -999 | |
| KSDD006 | 286 | 287 | Diorite | 0.01 | KSDD006 | 331 | 332 | Phyllite | -999 | |
| KSDD006 | 287 | 288 | Diorite | 0.01 | KSDD006 | 332 | 333 | Phyllite | -999 | |
| KSDD006 | 288 | 289 | Diorite | 0.01 | KSDD006 | 333 | 334 | Phyllite | 0.01 | |
| KSDD006 | 289 | 290 | Diorite | 0.01 | KSDD006 | 334 | 335 | Phyllite | -999 |
50
25 November 2022 ASX Announcement
ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD006 | 335 | 336 | Phyllite | -999 | KSDD006 | 380 | 381 | Fault | -999 | |
| KSDD006 | 336 | 337 | Phyllite | -999 | KSDD006 | 381 | 382 | Fault | -999 | |
| KSDD006 | 337 | 338 | Phyllite | 0.01 | KSDD006 | 382 | 383 | Fault | 0.01 | |
| KSDD006 | 338 | 339 | Phyllite | -999 | KSDD006 | 383 | 384 | Fault | 0.03 | |
| KSDD006 | 339 | 340 | Phyllite | 0.01 | KSDD006 | 384 | 385 | Fault | 2.23 | |
| KSDD006 | 340 | 341 | Phyllite | 0.03 | KSDD006 | 385 | 386 | Fault | 0.03 | |
| KSDD006 | 341 | 342 | Phyllite | -999 | KSDD006 | 386 | 387 | Fault | -999 | |
| KSDD006 | 342 | 343 | Phyllite | 0.02 | KSDD006 | 387 | 388 | Fault | -999 | |
| KSDD006 | 343 | 344 | Phyllite | 0.01 | KSDD006 | 388 | 389 | Phyllite | -999 | |
| KSDD006 | 344 | 345 | Phyllite | 0.01 | KSDD006 | 389 | 390 | Phyllite | 0.01 | |
| KSDD006 | 345 | 346 | Phyllite | 0.01 | KSDD006 | 390 | 391 | Phyllite | 0.01 | |
| KSDD006 | 346 | 347 | Phyllite | 0.02 | KSDD006 | 391 | 392 | Diorite | 0.01 | |
| KSDD006 | 347 | 348 | Phyllite | 0.01 | KSDD006 | 392 | 393 | Diorite | 0.03 | |
| KSDD006 | 348 | 349 | Phyllite | -999 | KSDD006 | 393 | 394 | Diorite | 0.01 | |
| KSDD006 | 349 | 350 | Phyllite | -999 | KSDD006 | 394 | 395 | Phyllite | 0.01 | |
| KSDD006 | 350 | 351 | Phyllite | -999 | KSDD006 | 395 | 396 | Phyllite | 0.01 | |
| KSDD006 | 351 | 352 | Phyllite | 0.02 | KSDD006 | 396 | 397 | Phyllite | 0.01 | |
| KSDD006 | 352 | 353 | Phyllite | -999 | KSDD006 | 397 | 398 | Phyllite | 0.01 | |
| KSDD006 | 353 | 354 | Phyllite | 0.01 | KSDD006 | 398 | 399 | Phyllite | 0.01 | |
| KSDD006 | 354 | 355 | Phyllite | 0.01 | KSDD006 | 399 | 400 | Phyllite | 0.01 | |
| KSDD006 | 355 | 356 | Phyllite | 0.01 | KSDD006 | 400 | 401 | Phyllite | 0.01 | |
| KSDD006 | 356 | 357 | Phyllite | 0.01 | KSDD006 | 401 | 402 | Phyllite | -999 | |
| KSDD006 | 357 | 358 | Phyllite | 0.01 | KSDD006 | 402 | 403 | Phyllite | 0.04 | |
| KSDD006 | 358 | 359 | Phyllite | 0.01 | KSDD006 | 403 | 404 | Phyllite | 0.01 | |
| KSDD006 | 359 | 360 | Phyllite | 0.01 | KSDD006 | 404 | 405 | Phyllite | 0.01 | |
| KSDD006 | 360 | 361 | Phyllite | 0.1 | KSDD006 | 405 | 406 | Phyllite | -999 | |
| KSDD006 | 361 | 362 | Phyllite | 0.01 | KSDD006 | 406 | 407 | Phyllite | 0.01 | |
| KSDD006 | 362 | 363 | Phyllite | 0.01 | KSDD006 | 407 | 408 | Phyllite | -999 | |
| KSDD006 | 363 | 364 | Phyllite | 0.01 | KSDD006 | 408 | 409 | Phyllite | 0.01 | |
| KSDD006 | 364 | 365 | Phyllite | 0.2 | KSDD006 | 409 | 410 | Phyllite | 0.01 | |
| KSDD006 | 365 | 366 | Phyllite | 0.02 | KSDD006 | 410 | 411 | Phyllite | 0.01 | |
| KSDD006 | 366 | 367 | Phyllite | 0.02 | KSDD006 | 411 | 412 | Phyllite | 0.01 | |
| KSDD006 | 367 | 368 | Phyllite | 0.01 | KSDD006 | 412 | 413 | Phyllite | 0.01 | |
| KSDD006 | 368 | 369 | Phyllite | -999 | KSDD006 | 413 | 414 | Phyllite | 0.01 | |
| KSDD006 | 369 | 370 | Phyllite | -999 | KSDD006 | 414 | 415 | Phyllite | 0.01 | |
| KSDD006 | 370 | 371 | Phyllite | 0.01 | KSDD006 | 415 | 416 | Phyllite | 0.01 | |
| KSDD006 | 371 | 372 | Phyllite | 0.02 | KSDD006 | 416 | 417 | Phyllite | -999 | |
| KSDD006 | 372 | 373 | Phyllite | 0.04 | KSDD006 | 417 | 418 | Phyllite | 0.01 | |
| KSDD006 | 373 | 374 | Phyllite | 0.02 | KSDD006 | 418 | 419 | Phyllite | 0.02 | |
| KSDD006 | 374 | 375 | Phyllite | -999 | KSDD006 | 419 | 420 | Phyllite | -999 | |
| KSDD006 | 375 | 376 | Phyllite | 0.01 | KSDD006 | 420 | 421 | Phyllite | 0.01 | |
| KSDD006 | 376 | 377 | Fault | 0.03 | KSDD006 | 421 | 422 | Phyllite | 0.02 | |
| KSDD006 | 377 | 378 | Phyllite | -999 | KSDD006 | 422 | 423 | Phyllite | 0.02 | |
| KSDD006 | 378 | 379 | Fault | -999 | KSDD006 | 423 | 424 | Phyllite | 0.01 | |
| KSDD006 | 379 | 380 | Fault | 0.49 | KSDD006 | 424 | 425 | Phyllite | 0.01 |
51
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD006 | 425 | 426 | Phyllite | 0.01 | KSDD007 | 7 | 8 | Phyllite | 0.04 | |
| KSDD006 | 426 | 427 | Phyllite | 0.01 | KSDD007 | 8 | 9 | Phyllite | 0.01 | |
| KSDD006 | 427 | 428 | Phyllite | 0.02 | KSDD007 | 9 | 10 | Phyllite | 0.01 | |
| KSDD006 | 428 | 429 | Phyllite | 0.02 | KSDD007 | 10 | 11 | Phyllite | 0.07 | |
| KSDD006 | 429 | 430 | Phyllite | -999 | KSDD007 | 11 | 12 | Phyllite | 0.08 | |
| KSDD006 | 430 | 431 | Phyllite | 0.01 | KSDD007 | 12 | 13 | Phyllite | -999 | |
| KSDD006 | 431 | 432 | Phyllite | 0.2 | KSDD007 | 13 | 14 | Phyllite | 0.02 | |
| KSDD006 | 432 | 433 | Phyllite | 0.02 | KSDD007 | 14 | 15 | Phyllite | -999 | |
| KSDD006 | 433 | 434 | Phyllite | 0.1 | KSDD007 | 15 | 16 | Phyllite | -999 | |
| KSDD006 | 434 | 435 | Phyllite | 0.01 | KSDD007 | 16 | 17 | Phyllite | 0.01 | |
| KSDD006 | 435 | 436 | Phyllite | 0.01 | KSDD007 | 17 | 18 | Phyllite | 0.02 | |
| KSDD006 | 436 | 437 | Phyllite | 0.01 | KSDD007 | 18 | 19 | Phyllite | 0.01 | |
| KSDD006 | 437 | 438 | Phyllite | 0.01 | KSDD007 | 19 | 20 | Phyllite | 0.01 | |
| KSDD006 | 438 | 439 | Phyllite | -999 | KSDD007 | 20 | 21 | Phyllite | 0.01 | |
| KSDD006 | 439 | 440 | Phyllite | -999 | KSDD007 | 21 | 22 | Phyllite | 0.01 | |
| KSDD006 | 440 | 441 | Phyllite | -999 | KSDD007 | 22 | 23 | Phyllite | 0.01 | |
| KSDD006 | 441 | 442 | Phyllite | -999 | KSDD007 | 23 | 24 | Phyllite | -999 | |
| KSDD006 | 442 | 443 | Phyllite | 0.03 | KSDD007 | 24 | 25 | Phyllite | 0.01 | |
| KSDD006 | 443 | 444 | Phyllite | -999 | KSDD007 | 25 | 26 | Fault | 0.06 | |
| KSDD006 | 444 | 445 | Phyllite | -999 | KSDD007 | 26 | 27 | Fault | 0.02 | |
| KSDD006 | 445 | 446 | Phyllite | -999 | KSDD007 | 27 | 28 | Fault | 0.37 | |
| KSDD006 | 446 | 447 | Phyllite | -999 | KSDD007 | 28 | 29 | Fault | 0.06 | |
| KSDD006 | 447 | 448 | Phyllite | 0.02 | KSDD007 | 29 | 30 | Fault | -999 | |
| KSDD006 | 448 | 449 | Phyllite | -999 | KSDD007 | 30 | 31 | Fault | 0.01 | |
| KSDD006 | 449 | 450 | Phyllite | 0.08 | KSDD007 | 31 | 32 | Fault | 0.01 | |
| KSDD006 | 450 | 451 | Phyllite | 0.01 | KSDD007 | 32 | 33 | Fault | 0.01 | |
| KSDD006 | 451 | 452 | Phyllite | -999 | KSDD007 | 33 | 34 | Fault | -999 | |
| KSDD006 | 452 | 453 | Fault | 0.33 | KSDD007 | 34 | 35 | Fault | 0.2 | |
| KSDD006 | 453 | 454 | Phyllite | 0.08 | KSDD007 | 35 | 36 | Fault | 0.07 | |
| KSDD006 | 454 | 455 | Phyllite | 0.02 | KSDD007 | 36 | 37 | Fault | 0.12 | |
| KSDD006 | 455 | 456 | Phyllite | 0.01 | KSDD007 | 37 | 38 | Fault | 0.01 | |
| KSDD006 | 456 | 457 | Phyllite | 0.01 | KSDD007 | 38 | 39 | Fault | 0.01 | |
| KSDD006 | 457 | 458 | Phyllite | -999 | KSDD007 | 39 | 40 | Fault | -999 | |
| KSDD006 | 458 | 459 | Phyllite | 0.28 | KSDD007 | 40 | 41 | Fault | 0.03 | |
| KSDD007 | 0 | 1 | Pad Fill | 0.04 | KSDD007 | 41 | 42 | Fault | 0.01 | |
| KSDD007 | 1 | 1.4 | Pad Fill | -999 | KSDD007 | 42 | 43 | Fault | 0.01 | |
| KSDD007 | 1.4 | 2 | Pad Fill | 0.08 | KSDD007 | 43 | 44 | Fault | -999 | |
| KSDD007 | 2 | 3 | Pad Fill | -999 | KSDD007 | 44 | 45 | Fault | -999 | |
| KSDD007 | 3 | 3.3 | Pad Fill | 0.07 | KSDD007 | 45 | 46 | Fault | -999 | |
| KSDD007 | 3.3 | 3.8 | Pad Fill | -999 | KSDD007 | 46 | 47 | Fault | -999 | |
| KSDD007 | 3.8 | 4 | Saprock | 0.05 | KSDD007 | 47 | 48 | Fault | -999 | |
| KSDD007 | 4 | 4.4 | Saprock | -999 | KSDD007 | 48 | 49 | Fault | -999 | |
| KSDD007 | 4.4 | 5 | Saprock | 0.31 | KSDD007 | 49 | 50 | Fault | 0.3 | |
| KSDD007 | 5 | 6 | Phyllite | 0.14 | KSDD007 | 50 | 51 | Fault | 0.15 | |
| KSDD007 | 6 | 7 | Phyllite | 0.03 | KSDD007 | 51 | 52 | Fault | 0.06 |
52
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD007 | 52 | 53 | Fault | 0.01 | KSDD007 | 96 | 97 | Diorite | 0.06 | |
| KSDD007 | 53 | 54 | Fault | 0.02 | KSDD007 | 97 | 98 | Diorite | 0.04 | |
| KSDD007 | 54 | 55 | Fault | 0.02 | KSDD007 | 98 | 99 | Diorite | 0.06 | |
| KSDD007 | 55 | 56 | Fault | 0.02 | KSDD007 | 99 | 100 | Fault | 0.08 | |
| KSDD007 | 56 | 57 | Fault | 0.06 | KSDD007 | 100 | 101 | Fault | 0.05 | |
| KSDD007 | 57 | 58 | Diorite | 0.04 | KSDD007 | 101 | 102 | Fault | 0.08 | |
| KSDD007 | 58 | 59 | Diorite | 0.11 | KSDD007 | 102 | 103 | Fault | 0.05 | |
| KSDD007 | 59 | 60 | Diorite | 0.09 | KSDD007 | 103 | 104 | Fault | 0.3 | |
| KSDD007 | 60 | 61 | Diorite | 0.33 | KSDD007 | 104 | 105 | Fault | 0.09 | |
| KSDD007 | 61 | 62 | Diorite | 0.18 | KSDD007 | 105 | 106 | Phyllite | 0.06 | |
| KSDD007 | 62 | 63 | Diorite | 0.16 | KSDD007 | 106 | 107 | Phyllite | 0.07 | |
| KSDD007 | 63 | 63 | Fault | -999 | KSDD007 | 107 | 108 | Phyllite | 0.06 | |
| KSDD007 | 63 | 64 | Fault | 0.2 | KSDD007 | 108 | 109 | Phyllite | 0.05 | |
| KSDD007 | 64 | 65 | Fault | -999 | KSDD007 | 109 | 110 | Phyllite | 0.15 | |
| KSDD007 | 65 | 66 | Fault | 0.18 | KSDD007 | 110 | 111 | Phyllite | 0.16 | |
| KSDD007 | 66 | 67 | Fault | 0.09 | KSDD007 | 111 | 112 | Phyllite | 0.23 | |
| KSDD007 | 67 | 68 | Fault | 0.1 | KSDD007 | 112 | 113 | Phyllite | 0.14 | |
| KSDD007 | 68 | 69 | Fault | 0.08 | KSDD007 | 113 | 114 | Phyllite | 0.16 | |
| KSDD007 | 69 | 70 | Fault | 0.17 | KSDD007 | 114 | 115 | Phyllite | 0.2 | |
| KSDD007 | 70 | 71 | Fault | 0.13 | KSDD007 | 115 | 116 | Diorite | 0.11 | |
| KSDD007 | 71 | 72 | Fault | 0.05 | KSDD007 | 116 | 117 | Fault | 0.14 | |
| KSDD007 | 72 | 73 | Fault | 0.07 | KSDD007 | 117 | 118 | Fault | 0.17 | |
| KSDD007 | 73 | 74 | Fault | 0.08 | KSDD007 | 118 | 119 | Fault | 0.1 | |
| KSDD007 | 74 | 75 | Fault | 0.11 | KSDD007 | 119 | 120 | Phyllite | 0.11 | |
| KSDD007 | 75 | 76 | Fault | 0.1 | KSDD007 | 120 | 121 | Phyllite | 0.11 | |
| KSDD007 | 76 | 77 | Fault | 0.05 | KSDD007 | 121 | 122 | Phyllite | 0.09 | |
| KSDD007 | 77 | 78 | Fault | 0.04 | KSDD007 | 122 | 123 | Phyllite | 0.13 | |
| KSDD007 | 78 | 79 | Fault | 0.62 | KSDD007 | 123 | 124 | Phyllite | 0.14 | |
| KSDD007 | 79 | 80 | Fault | 0.38 | KSDD007 | 124 | 125 | Phyllite | 0.11 | |
| KSDD007 | 80 | 81 | Fault | 0.08 | KSDD007 | 125 | 126 | Phyllite | 0.13 | |
| KSDD007 | 81 | 82 | Fault | 0.05 | KSDD007 | 126 | 127 | Phyllite | 0.29 | |
| KSDD007 | 82 | 83 | Fault | 0.07 | KSDD007 | 127 | 128 | Phyllite | 0.13 | |
| KSDD007 | 83 | 84 | Fault | 0.05 | KSDD007 | 128 | 129 | Phyllite | 0.15 | |
| KSDD007 | 84 | 85 | Fault | 0.06 | KSDD007 | 129 | 130 | Phyllite | 0.09 | |
| KSDD007 | 85 | 86 | Fault | 0.05 | KSDD007 | 130 | 131 | Phyllite | 0.12 | |
| KSDD007 | 86 | 87 | Fault | 0.06 | KSDD007 | 131 | 132 | Phyllite | 0.08 | |
| KSDD007 | 87 | 88 | Fault | 0.04 | KSDD007 | 132 | 133 | Phyllite | 0.09 | |
| KSDD007 | 88 | 89 | Fault | 0.08 | KSDD007 | 133 | 134 | Phyllite | 0.1 | |
| KSDD007 | 89 | 90 | Fault | 0.05 | KSDD007 | 134 | 135 | Phyllite | 0.27 | |
| KSDD007 | 90 | 91 | Fault | 0.06 | KSDD007 | 135 | 136 | Diorite | 0.17 | |
| KSDD007 | 91 | 92 | Fault | 0.06 | KSDD007 | 136 | 137 | Fault | 0.35 | |
| KSDD007 | 92 | 93 | Fault | 0.09 | KSDD007 | 137 | 138 | Fault | 2.88 | |
| KSDD007 | 93 | 94 | Fault | 0.05 | KSDD007 | 138 | 139 | Fault | 1 | |
| KSDD007 | 94 | 95 | Diorite | 0.04 | KSDD007 | 139 | 140 | Fault | 2.13 | |
| KSDD007 | 95 | 96 | Diorite | 0.06 | KSDD007 | 140 | 141 | Fault | 1.07 |
53
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD007 | 141 | 142 | Fault | 0.48 | KSDD007 | 185 | 186 | Marble | 0.4 | |
| KSDD007 | 142 | 143 | Fault | 0.39 | KSDD007 | 186 | 187 | Marble | 0.43 | |
| KSDD007 | 143 | 144 | Fault | 0.24 | KSDD007 | 187 | 188 | Marble | 0.06 | |
| KSDD007 | 144 | 145 | Fault | 0.18 | KSDD007 | 188 | 189 | Marble | 0.03 | |
| KSDD007 | 145 | 146 | Fault | 0.16 | KSDD007 | 189 | 190 | Marble | 0.03 | |
| KSDD007 | 146 | 147 | Fault | 1.71 | KSDD007 | 190 | 191 | Marble | 0.05 | |
| KSDD007 | 147 | 148 | Fault | 0.7 | KSDD007 | 191 | 192 | Marble | 0.06 | |
| KSDD007 | 148 | 149 | Fault | 0.31 | KSDD007 | 192 | 193 | Marble | 0.03 | |
| KSDD007 | 149 | 150 | Fault | 0.34 | KSDD007 | 193 | 194 | Marble | 0.05 | |
| KSDD007 | 150 | 151 | Fault | 0.38 | KSDD007 | 194 | 195 | Marble | 0.13 | |
| KSDD007 | 151 | 152 | Fault | 0.14 | KSDD007 | 195 | 196 | Marble | 0.03 | |
| KSDD007 | 152 | 153 | Fault | 0.38 | KSDD007 | 196 | 197 | Marble | 0.78 | |
| KSDD007 | 153 | 154 | Fault | 0.65 | KSDD007 | 197 | 198 | Fault | 2.37 | |
| KSDD007 | 154 | 155 | Fault | 0.21 | KSDD007 | 198 | 199 | Marble | 0.79 | |
| KSDD007 | 155 | 156 | Fault | 0.23 | KSDD007 | 199 | 200 | Marble | 0.15 | |
| KSDD007 | 156 | 157 | Fault | 0.37 | KSDD007 | 200 | 201 | Marble | 7.95 | |
| KSDD007 | 157 | 158 | Fault | 0.43 | KSDD007 | 201 | 202 | Fault | 0.28 | |
| KSDD007 | 158 | 159 | Fault | 0.53 | KSDD007 | 202 | 203 | Fault | -999 | |
| KSDD007 | 159 | 160 | Fault | 0.64 | KSDD007 | 203 | 204 | Fault | 4.97 | |
| KSDD007 | 160 | 161 | Fault | 10.8 | KSDD007 | 204 | 205 | Skarn | 0.55 | |
| KSDD007 | 161 | 162 | Fault | 4.12 | KSDD007 | 205 | 206 | Skarn | 0.8 | |
| KSDD007 | 162 | 163 | Fault | 4.06 | KSDD007 | 206 | 207 | Skarn | 1.03 | |
| KSDD007 | 163 | 164 | Marble | 56 | KSDD007 | 207 | 208 | Skarn | 2.74 | |
| KSDD007 | 164 | 165 | Marble | 0.47 | KSDD007 | 208 | 209 | Skarn | 1.08 | |
| KSDD007 | 165 | 166 | Marble | 0.48 | KSDD007 | 209 | 210 | Skarn | 2.25 | |
| KSDD007 | 166 | 167 | Marble | 0.52 | KSDD007 | 210 | 211 | Skarn | 0.22 | |
| KSDD007 | 167 | 168 | Marble | 0.13 | KSDD007 | 211 | 212 | Skarn | 0.2 | |
| KSDD007 | 168 | 169 | Marble | 0.08 | KSDD007 | 212 | 213 | Skarn | 0.17 | |
| KSDD007 | 169 | 170 | Marble | 0.06 | KSDD007 | 213 | 214 | Skarn | 0.16 | |
| KSDD007 | 170 | 171 | Marble | 13.9 | KSDD007 | 214 | 215 | Skarn | 0.1 | |
| KSDD007 | 171 | 172 | Marble | 0.03 | KSDD007 | 215 | 216 | Phyllite | 0.04 | |
| KSDD007 | 172 | 173 | Marble | 0.12 | KSDD007 | 216 | 217 | Phyllite | 0.04 | |
| KSDD007 | 173 | 174 | Marble | 0.07 | KSDD007 | 217 | 218 | Phyllite | 0.02 | |
| KSDD007 | 174 | 175 | Marble | -999 | KSDD007 | 218 | 219 | Phyllite | 0.02 | |
| KSDD007 | 175 | 175 | Marble | 0.03 | KSDD007 | 219 | 220 | Phyllite | 0.03 | |
| KSDD007 | 175 | 176 | Marble | 0.11 | KSDD007 | 220 | 221 | Phyllite | 0.02 | |
| KSDD007 | 176 | 177 | Marble | 0.03 | KSDD007 | 221 | 222 | Phyllite | 0.03 | |
| KSDD007 | 177 | 178 | Marble | 0.04 | KSDD007 | 222 | 223 | Phyllite | 0.02 | |
| KSDD007 | 178 | 179 | Marble | 0.12 | KSDD007 | 223 | 224 | Phyllite | 0.03 | |
| KSDD007 | 179 | 180 | Marble | 0.03 | KSDD007 | 224 | 225 | Phyllite | 0.02 | |
| KSDD007 | 180 | 181 | Marble | 0.06 | KSDD007 | 225 | 226 | Phyllite | 0.03 | |
| KSDD007 | 181 | 182 | Marble | 0.19 | KSDD007 | 226 | 227 | Phyllite | 0.03 | |
| KSDD007 | 182 | 183 | Marble | 0.04 | KSDD007 | 227 | 228 | Phyllite | 0.04 | |
| KSDD007 | 183 | 184 | Marble | 0.16 | KSDD007 | 228 | 229 | Phyllite | 0.04 | |
| KSDD007 | 184 | 185 | Marble | 0.05 | KSDD007 | 229 | 230 | Phyllite | 0.03 |
54
25 November 2022 ASX Announcement ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD007 | 230 | 231 | Phyllite | 0.03 | KSDD007 | 275 | 276 | Phyllite | 0.04 | |
| KSDD007 | 231 | 232 | Phyllite | 0.03 | KSDD007 | 276 | 277 | Phyllite | 0.05 | |
| KSDD007 | 232 | 233 | Phyllite | 0.03 | KSDD007 | 277 | 278 | Phyllite | 0.09 | |
| KSDD007 | 233 | 234 | Phyllite | 0.05 | KSDD007 | 278 | 279 | Phyllite | 0.07 | |
| KSDD007 | 234 | 235 | Phyllite | 0.02 | KSDD007 | 279 | 280 | Phyllite | 0.03 | |
| KSDD007 | 235 | 236 | Phyllite | 0.03 | KSDD007 | 280 | 281 | Phyllite | 0.04 | |
| KSDD007 | 236 | 237 | Phyllite | 0.03 | KSDD007 | 281 | 282 | Phyllite | 0.14 | |
| KSDD007 | 237 | 238 | Phyllite | 0.1 | KSDD007 | 282 | 283 | Phyllite | 0.13 | |
| KSDD007 | 238 | 239 | Phyllite | 0.21 | KSDD007 | 283 | 284 | Phyllite | 0.03 | |
| KSDD007 | 239 | 240 | Phyllite | 0.26 | KSDD007 | 284 | 285 | Phyllite | 0.05 | |
| KSDD007 | 240 | 241 | Phyllite | 0.12 | KSDD007 | 285 | 286 | Phyllite | 0.05 | |
| KSDD007 | 241 | 242 | Phyllite | 0.03 | KSDD007 | 286 | 287 | Phyllite | 0.1 | |
| KSDD007 | 242 | 243 | Phyllite | 0.02 | KSDD007 | 287 | 288 | Phyllite | 0.06 | |
| KSDD007 | 243 | 244 | Phyllite | 0.03 | KSDD007 | 288 | 289 | Phyllite | 0.18 | |
| KSDD007 | 244 | 245 | Phyllite | 0.02 | KSDD007 | 289 | 290 | Phyllite | 0.04 | |
| KSDD007 | 245 | 246 | Phyllite | 0.02 | KSDD007 | 290 | 291 | Phyllite | 0.04 | |
| KSDD007 | 246 | 247 | Phyllite | 0.07 | KSDD007 | 291 | 292 | Phyllite | 0.05 | |
| KSDD007 | 247 | 248 | Phyllite | 0.03 | KSDD007 | 292 | 292 | Phyllite | -999 | |
| KSDD007 | 248 | 249 | Phyllite | 0.02 | KSDD007 | 292 | 293 | Phyllite | 0.06 | |
| KSDD007 | 249 | 250 | Phyllite | 0.02 | KSDD007 | 293 | 294 | Breccia | 0.04 | |
| KSDD007 | 250 | 251 | Phyllite | 0.04 | KSDD007 | 294 | 295 | Phyllite | 0.03 | |
| KSDD007 | 251 | 252 | Phyllite | 0.02 | KSDD007 | 295 | 296 | Phyllite | 0.03 | |
| KSDD007 | 252 | 253 | Phyllite | 0.04 | KSDD007 | 296 | 297 | Phyllite | 0.09 | |
| KSDD007 | 253 | 254 | Phyllite | 0.01 | KSDD007 | 297 | 298 | Phyllite | 0.02 | |
| KSDD007 | 254 | 255 | Phyllite | 0.02 | KSDD007 | 298 | 299 | Phyllite | 0.04 | |
| KSDD007 | 255 | 256 | Phyllite | 0.04 | KSDD007 | 299 | 300 | Phyllite | 0.06 | |
| KSDD007 | 256 | 257 | Phyllite | 0.03 | KSDD007 | 300 | 301 | Phyllite | 0.06 | |
| KSDD007 | 257 | 258 | Phyllite | 0.05 | KSDD007 | 301 | 302 | Phyllite | 0.05 | |
| KSDD007 | 258 | 259 | Phyllite | 0.09 | KSDD007 | 302 | 303 | Phyllite | 0.05 | |
| KSDD007 | 259 | 260 | Phyllite | 0.02 | KSDD007 | 303 | 304 | Phyllite | 0.07 | |
| KSDD007 | 260 | 261 | Phyllite | 0.05 | KSDD007 | 304 | 305 | Phyllite | 0.03 | |
| KSDD007 | 261 | 262 | Phyllite | 0.06 | KSDD007 | 305 | 306 | Phyllite | 0.03 | |
| KSDD007 | 262 | 263 | Phyllite | 0.04 | KSDD007 | 306 | 307 | Phyllite | 0.04 | |
| KSDD007 | 263 | 264 | Phyllite | 0.02 | KSDD007 | 307 | 308 | Phyllite | 0.04 | |
| KSDD007 | 264 | 265 | Phyllite | 0.03 | KSDD007 | 308 | 309 | Phyllite | 0.05 | |
| KSDD007 | 265 | 266 | Phyllite | 0.04 | KSDD007 | 309 | 310 | Phyllite | 0.05 | |
| KSDD007 | 266 | 267 | Phyllite | 0.03 | KSDD007 | 310 | 311 | Phyllite | 0.05 | |
| KSDD007 | 267 | 268 | Phyllite | 0.02 | KSDD007 | 311 | 312 | Phyllite | 0.03 | |
| KSDD007 | 268 | 269 | Phyllite | 0.06 | KSDD007 | 312 | 313 | Diorite | 0.03 | |
| KSDD007 | 269 | 270 | Phyllite | 0.02 | KSDD007 | 313 | 314 | Diorite | 0.03 | |
| KSDD007 | 270 | 271 | Phyllite | 0.02 | KSDD007 | 314 | 315 | Phyllite | 0.02 | |
| KSDD007 | 271 | 272 | Phyllite | 0.05 | KSDD007 | 315 | 316 | Phyllite | 0.03 | |
| KSDD007 | 272 | 273 | Phyllite | 0.05 | KSDD007 | 316 | 317 | Phyllite | 0.04 | |
| KSDD007 | 273 | 274 | Phyllite | 0.06 | KSDD007 | 317 | 318 | Phyllite | 0.03 | |
| KSDD007 | 274 | 275 | Phyllite | 0.03 | KSDD007 | 318 | 319 | Phyllite | 0.02 |
55
25 November 2022 ASX Announcement
ASX: LCL
==> picture [103 x 68] intentionally omitted <==
| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD007 | 319 | 320 | Phyllite | 0.02 | KSDD007 | 364 | 365 | Diorite | 0.01 | |
| KSDD007 | 320 | 321 | Phyllite | 0.03 | KSDD007 | 365 | 366 | Phyllite | 0.03 | |
| KSDD007 | 321 | 322 | Phyllite | 0.05 | KSDD007 | 366 | 367 | Phyllite | 0.05 | |
| KSDD007 | 322 | 323 | Phyllite | 0.04 | KSDD007 | 367 | 368 | Phyllite | 0.04 | |
| KSDD007 | 323 | 324 | Phyllite | 0.04 | KSDD007 | 368 | 369 | Phyllite | 0.05 | |
| KSDD007 | 324 | 325 | Phyllite | 0.04 | KSDD007 | 369 | 370 | Phyllite | 0.04 | |
| KSDD007 | 325 | 326 | Diorite | 0.05 | KSDD007 | 370 | 371 | Phyllite | 0.04 | |
| KSDD007 | 326 | 327 | Diorite | 0.07 | KSDD007 | 371 | 372 | Phyllite | 0.07 | |
| KSDD007 | 327 | 328 | Diorite | 0.23 | KSDD007 | 372 | 373 | Phyllite | 0.07 | |
| KSDD007 | 328 | 329 | Diorite | 0.79 | KSDD007 | 373 | 374 | Phyllite | 0.04 | |
| KSDD007 | 329 | 330 | Diorite | 0.09 | KSDD007 | 374 | 375 | Phyllite | 0.02 | |
| KSDD007 | 330 | 331 | Fault | 0.03 | KSDD007 | 375 | 376 | Phyllite | 0.09 | |
| KSDD007 | 331 | 332 | Fault | 0.02 | KSDD007 | 376 | 377 | Phyllite | 0.02 | |
| KSDD007 | 332 | 333 | Diorite | 0.02 | KSDD007 | 377 | 378 | Phyllite | 0.04 | |
| KSDD007 | 333 | 334 | Diorite | 0.04 | KSDD007 | 378 | 379 | Phyllite | 0.07 | |
| KSDD007 | 334 | 335 | Diorite | 0.07 | KSDD007 | 379 | 380 | Phyllite | 0.1 | |
| KSDD007 | 335 | 336 | Phyllite | 0.08 | KSDD007 | 380 | 381 | Phyllite | 0.05 | |
| KSDD007 | 336 | 337 | Phyllite | 0.07 | KSDD007 | 381 | 382 | Phyllite | 0.03 | |
| KSDD007 | 337 | 338 | Phyllite | 0.08 | KSDD007 | 382 | 383 | Phyllite | 0.03 | |
| KSDD007 | 338 | 339 | Phyllite | 0.3 | KSDD007 | 383 | 384 | Phyllite | 0.03 | |
| KSDD007 | 339 | 340 | Phyllite | 0.1 | KSDD007 | 384 | 385 | Phyllite | 0.04 | |
| KSDD007 | 340 | 341 | Phyllite | 0.09 | KSDD007 | 385 | 386 | Phyllite | 0.05 | |
| KSDD007 | 341 | 342 | Phyllite | 0.09 | KSDD007 | 386 | 387 | Phyllite | 0.05 | |
| KSDD007 | 342 | 343 | Phyllite | 0.06 | KSDD007 | 387 | 388 | Phyllite | 0.05 | |
| KSDD007 | 343 | 344 | Phyllite | 0.07 | KSDD007 | 388 | 389 | Phyllite | 0.06 | |
| KSDD007 | 344 | 345 | Phyllite | 0.11 | KSDD007 | 389 | 390 | Phyllite | 0.04 | |
| KSDD007 | 345 | 346 | Phyllite | 0.17 | KSDD007 | 390 | 391 | Phyllite | 0.21 | |
| KSDD007 | 346 | 347 | Phyllite | 0.1 | KSDD007 | 391 | 392 | Phyllite | 0.14 | |
| KSDD007 | 347 | 348 | Phyllite | 0.06 | KSDD007 | 392 | 393 | Phyllite | 0.07 | |
| KSDD007 | 348 | 349 | Phyllite | 0.07 | KSDD007 | 393 | 394 | Phyllite | 0.03 | |
| KSDD007 | 349 | 350 | Phyllite | 0.06 | KSDD007 | 394 | 395 | Phyllite | 0.03 | |
| KSDD007 | 350 | 351 | Phyllite | 0.13 | KSDD007 | 395 | 396 | Phyllite | 0.02 | |
| KSDD007 | 351 | 352 | Phyllite | 0.12 | KSDD007 | 396 | 397 | Phyllite | 0.03 | |
| KSDD007 | 352 | 353 | Phyllite | 0.12 | KSDD007 | 397 | 398 | Phyllite | 0.03 | |
| KSDD007 | 353 | 354 | Phyllite | 0.08 | KSDD007 | 398 | 399 | Phyllite | 0.06 | |
| KSDD007 | 354 | 355 | Phyllite | 0.04 | KSDD007 | 399 | 400 | Phyllite | 0.05 | |
| KSDD007 | 355 | 356 | Phyllite | 0.06 | KSDD007 | 400 | 401 | Phyllite | 0.07 | |
| KSDD007 | 356 | 357 | Phyllite | 0.04 | KSDD007 | 401 | 402 | Phyllite | 0.09 | |
| KSDD007 | 357 | 358 | Phyllite | 0.08 | KSDD007 | 402 | 403 | Phyllite | 0.13 | |
| KSDD007 | 358 | 359 | Phyllite | 0.06 | KSDD007 | 403 | 404 | Phyllite | 0.24 | |
| KSDD007 | 359 | 360 | Phyllite | 0.03 | KSDD007 | 404 | 405 | Phyllite | 0.14 | |
| KSDD007 | 360 | 361 | Diorite | 0.01 | KSDD007 | 405 | 406 | Phyllite | 0.14 | |
| KSDD007 | 361 | 362 | Diorite | 0.01 | KSDD007 | 406 | 407 | Phyllite | 0.08 | |
| KSDD007 | 362 | 363 | Diorite | 0.02 | KSDD007 | 407 | 408 | Phyllite | 0.06 | |
| KSDD007 | 363 | 364 | Diorite | 0.02 | KSDD007 | 408 | 409 | Phyllite | 0.05 |
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| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD007 | 409 | 410 | Phyllite | 0.21 | KSDD007 | 454 | 455 | Phyllite | 0.01 | |
| KSDD007 | 410 | 411 | Phyllite | 0.05 | KSDD007 | 455 | 456 | Phyllite | 0.01 | |
| KSDD007 | 411 | 412 | Phyllite | 0.07 | KSDD007 | 456 | 457 | Phyllite | 0.01 | |
| KSDD007 | 412 | 413 | Phyllite | 0.05 | KSDD007 | 457 | 458 | Phyllite | 0.02 | |
| KSDD007 | 413 | 414 | Phyllite | 0.03 | KSDD007 | 458 | 459 | Phyllite | 0.01 | |
| KSDD007 | 414 | 415 | Phyllite | 0.06 | KSDD007 | 459 | 460 | Phyllite | 0.01 | |
| KSDD007 | 415 | 416 | Phyllite | 0.1 | KSDD007 | 460 | 461 | Phyllite | 0.06 | |
| KSDD007 | 416 | 417 | Phyllite | 0.11 | KSDD008 | 0 | 5 | Colluvium | 0.01 | |
| KSDD007 | 417 | 418 | Phyllite | 0.07 | KSDD008 | 5 | 8.2 | Colluvium | 0.04 | |
| KSDD007 | 418 | 419 | Phyllite | 0.08 | KSDD008 | 8.2 | 9 | Gossan | 0.63 | |
| KSDD007 | 419 | 420 | Phyllite | 0.08 | KSDD008 | 9 | 10 | Gossan | 1.29 | |
| KSDD007 | 420 | 421 | Phyllite | 0.08 | KSDD008 | 10 | 11 | Marble | 0.46 | |
| KSDD007 | 421 | 422 | Phyllite | 0.16 | KSDD008 | 11 | 12 | Marble | 0.34 | |
| KSDD007 | 422 | 423 | Phyllite | 0.46 | KSDD008 | 12 | 14 | Marble | 0.35 | |
| KSDD007 | 423 | 424 | Phyllite | 1.95 | KSDD008 | 14 | 14 | Marble | 0.45 | |
| KSDD007 | 424 | 425 | Phyllite | 4.42 | KSDD008 | 14 | 15 | Phyllite | 0.25 | |
| KSDD007 | 425 | 426 | Phyllite | 1.12 | KSDD008 | 15 | 16 | Phyllite | 0.17 | |
| KSDD007 | 426 | 427 | Phyllite | 0.1 | KSDD008 | 16 | 17 | Phyllite | 0.19 | |
| KSDD007 | 427 | 428 | Phyllite | 0.12 | KSDD008 | 17 | 18 | Phyllite | 0.14 | |
| KSDD007 | 428 | 429 | Phyllite | 0.05 | KSDD008 | 18 | 19 | Phyllite | 0.2 | |
| KSDD007 | 429 | 430 | Phyllite | 0.15 | KSDD008 | 19 | 20 | Phyllite | 0.13 | |
| KSDD007 | 430 | 431 | Phyllite | 0.05 | KSDD008 | 20 | 21 | Phyllite | 0.05 | |
| KSDD007 | 431 | 432 | Fault | 1.8 | KSDD008 | 21 | 22 | Phyllite | 0.07 | |
| KSDD007 | 432 | 433 | Phyllite | 0.41 | KSDD008 | 22 | 23 | Phyllite | 0.1 | |
| KSDD007 | 433 | 434 | Phyllite | 0.25 | KSDD008 | 23 | 24 | Phyllite | 0.04 | |
| KSDD007 | 434 | 435 | Phyllite | 0.06 | KSDD008 | 24 | 25 | Phyllite | 0.05 | |
| KSDD007 | 435 | 436 | Phyllite | 0.07 | KSDD008 | 25 | 26 | Phyllite | 0.08 | |
| KSDD007 | 436 | 437 | Phyllite | 0.1 | KSDD008 | 26 | 27 | Phyllite | 0.04 | |
| KSDD007 | 437 | 438 | Phyllite | 0.18 | KSDD008 | 27 | 28 | Mylonite | 0.15 | |
| KSDD007 | 438 | 439 | Phyllite | 0.06 | KSDD008 | 28 | 29 | Mylonite | 0.09 | |
| KSDD007 | 439 | 440 | Phyllite | 0.1 | KSDD008 | 29 | 30 | Mylonite | 0.16 | |
| KSDD007 | 440 | 441 | Phyllite | 0.05 | KSDD008 | 30 | 31 | Mylonite | 0.1 | |
| KSDD007 | 441 | 442 | Phyllite | 0.1 | KSDD008 | 31 | 32 | Mylonite | 0.17 | |
| KSDD007 | 442 | 443 | Phyllite | 0.05 | KSDD008 | 32 | 33 | Mylonite | 0.17 | |
| KSDD007 | 443 | 444 | Phyllite | 0.15 | KSDD008 | 33 | 34 | Mylonite | 0.79 | |
| KSDD007 | 444 | 445 | Phyllite | 0.02 | KSDD008 | 34 | 35 | Mylonite | 0.16 | |
| KSDD007 | 445 | 446 | Phyllite | 0.01 | KSDD008 | 35 | 36 | Mylonite | 0.16 | |
| KSDD007 | 446 | 447 | Phyllite | 0.01 | KSDD008 | 36 | 37 | Mylonite | 0.16 | |
| KSDD007 | 447 | 448 | Phyllite | 0.02 | KSDD008 | 37 | 38 | Mylonite | 0.04 | |
| KSDD007 | 448 | 449 | Phyllite | 0.02 | KSDD008 | 38 | 39 | Mylonite | 0.14 | |
| KSDD007 | 449 | 450 | Phyllite | 0.01 | KSDD008 | 39 | 40 | Mylonite | 0.08 | |
| KSDD007 | 450 | 451 | Phyllite | 0.01 | KSDD008 | 40 | 41 | Mylonite | 0.09 | |
| KSDD007 | 451 | 452 | Phyllite | 0.1 | KSDD008 | 41 | 42 | Mylonite | 0.1 | |
| KSDD007 | 452 | 453 | Phyllite | 0.01 | KSDD008 | 42 | 43 | Mylonite | 0.12 | |
| KSDD007 | 453 | 454 | Phyllite | 0.02 | KSDD008 | 43 | 44 | Mylonite | 0.12 |
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| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD008 | 44 | 45 | Mylonite | 0.09 | KSDD008 | 89 | 90 | Phyllite | 0.02 | |
| KSDD008 | 45 | 46 | Fault | 0.25 | KSDD008 | 90 | 91 | Phyllite | 0.02 | |
| KSDD008 | 46 | 47 | Fault | 0.14 | KSDD008 | 91 | 92 | Phyllite | 0.61 | |
| KSDD008 | 47 | 48 | Fault | 0.4 | KSDD008 | 92 | 93 | Phyllite | 0.04 | |
| KSDD008 | 48 | 49 | Fault | 0.14 | KSDD008 | 93 | 94 | Phyllite | 0.02 | |
| KSDD008 | 49 | 50 | Fault | 0.17 | KSDD008 | 94 | 95 | Phyllite | 0.04 | |
| KSDD008 | 50 | 51 | Phyllite | 0.06 | KSDD008 | 95 | 96 | Phyllite | 0.04 | |
| KSDD008 | 51 | 52 | Phyllite | 0.08 | KSDD008 | 96 | 97 | Phyllite | 0.05 | |
| KSDD008 | 52 | 53 | Phyllite | 0.12 | KSDD008 | 97 | 98 | Fault | 0.03 | |
| KSDD008 | 53 | 54 | Phyllite | 0.12 | KSDD008 | 98 | 99 | Fault | 0.09 | |
| KSDD008 | 54 | 55 | Phyllite | 0.08 | KSDD008 | 99 | 100 | Fault | 0.11 | |
| KSDD008 | 55 | 56 | Phyllite | 0.2 | KSDD008 | 100 | 101 | Fault | 0.09 | |
| KSDD008 | 56 | 57 | Phyllite | 0.09 | KSDD008 | 101 | 102 | Fault | 0.1 | |
| KSDD008 | 57 | 58 | Phyllite | 0.04 | KSDD008 | 102 | 103 | Fault | 0.04 | |
| KSDD008 | 58 | 59 | Phyllite | 0.05 | KSDD008 | 103 | 104 | Fault | 0.03 | |
| KSDD008 | 59 | 60 | Phyllite | 0.26 | KSDD008 | 104 | 105 | Quartzite | 0.03 | |
| KSDD008 | 60 | 61 | Phyllite | 0.06 | KSDD008 | 105 | 106 | Quartzite | 0.01 | |
| KSDD008 | 61 | 62 | Phyllite | 0.18 | KSDD008 | 106 | 107 | Quartzite | 0.04 | |
| KSDD008 | 62 | 63 | Phyllite | 0.05 | KSDD008 | 107 | 108 | Quartzite | 0.02 | |
| KSDD008 | 63 | 64 | Phyllite | 0.08 | KSDD008 | 108 | 109 | Quartzite | 0.02 | |
| KSDD008 | 64 | 65 | Phyllite | 0.07 | KSDD008 | 109 | 110 | Quartzite | 0.03 | |
| KSDD008 | 65 | 66 | Phyllite | 0.08 | KSDD008 | 110 | 111 | Quartzite | 0.03 | |
| KSDD008 | 66 | 67 | Phyllite | 0.13 | KSDD008 | 111 | 112 | Quartzite | 0.02 | |
| KSDD008 | 67 | 68 | Phyllite | 0.04 | KSDD008 | 112 | 113 | Quartzite | 0.01 | |
| KSDD008 | 68 | 69 | Phyllite | 0.11 | KSDD008 | 113 | 114 | Quartzite | 0.02 | |
| KSDD008 | 69 | 70 | Fault | 0.35 | KSDD008 | 114 | 115 | Quartzite | 0.01 | |
| KSDD008 | 70 | 71 | Fault | 0.28 | KSDD008 | 115 | 116 | Quartzite | 0.02 | |
| KSDD008 | 71 | 72 | Phyllite | 0.12 | KSDD008 | 116 | 117 | Quartzite | 0.02 | |
| KSDD008 | 72 | 73 | Phyllite | 0.07 | KSDD008 | 117 | 118 | Quartzite | 0.02 | |
| KSDD008 | 73 | 74 | Phyllite | 0.07 | KSDD008 | 118 | 119 | Quartzite | 0.02 | |
| KSDD008 | 74 | 75 | Phyllite | 0.05 | KSDD008 | 119 | 120 | Fault | 0.05 | |
| KSDD008 | 75 | 76 | Phyllite | 0.07 | KSDD008 | 120 | 121 | Fault | 0.13 | |
| KSDD008 | 76 | 77 | Phyllite | 0.02 | KSDD008 | 121 | 122 | Fault | 0.01 | |
| KSDD008 | 77 | 78 | Phyllite | 0.04 | KSDD008 | 122 | 123 | Fault | 0.06 | |
| KSDD008 | 78 | 79 | Phyllite | 0.05 | KSDD008 | 123 | 124 | Fault | 0.06 | |
| KSDD008 | 79 | 80 | Phyllite | 0.05 | KSDD008 | 124 | 125 | Fault | -999 | |
| KSDD008 | 80 | 81 | Phyllite | 0.03 | KSDD008 | 125 | 126 | Fault | 0.17 | |
| KSDD008 | 81 | 82 | Fault | 0.05 | KSDD008 | 126 | 127 | Fault | 0.04 | |
| KSDD008 | 82 | 83 | Fault | 0.12 | KSDD008 | 127 | 128 | Fault | 0.03 | |
| KSDD008 | 83 | 84 | Fault | 0.13 | KSDD008 | 128 | 129 | Fault | 0.11 | |
| KSDD008 | 84 | 85 | Fault | 0.08 | KSDD008 | 129 | 130 | Fault | 0.07 | |
| KSDD008 | 85 | 86 | Fault | 0.1 | KSDD008 | 130 | 130 | Fault | 0.06 | |
| KSDD008 | 86 | 87 | Phyllite | 0.02 | KSDD008 | 130 | 131 | Fault | 0.2 | |
| KSDD008 | 87 | 88 | Phyllite | 0.02 | KSDD008 | 131 | 132 | Fault | 0.06 | |
| KSDD008 | 88 | 89 | Phyllite | 0.02 | KSDD008 | 132 | 133 | Fault | 0.13 |
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25 November 2022 ASX Announcement ASX: LCL
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| Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
Hole_ID | From (m) |
To (m) |
Lithology | Au (g/t) |
|
|---|---|---|---|---|---|---|---|---|---|---|
| KSDD008 | 133 | 134 | Fault | -999 | KSDD008 | 177 | 178 | Phyllite | 0.01 | |
| KSDD008 | 134 | 135 | Fault | 0.24 | KSDD008 | 178 | 179 | Phyllite | 0.03 | |
| KSDD008 | 135 | 136 | Phyllite | 1.03 | KSDD008 | 179 | 180 | Phyllite | 0.03 | |
| KSDD008 | 136 | 137 | Phyllite | 0.03 | KSDD008 | 180 | 181 | Phyllite | 0.02 | |
| KSDD008 | 137 | 138 | Phyllite | 0.02 | KSDD008 | 181 | 182 | Phyllite | 0.02 | |
| KSDD008 | 138 | 139 | Phyllite | 0.07 | KSDD008 | 182 | 183 | Fault | 0.01 | |
| KSDD008 | 139 | 140 | Phyllite | 0.02 | KSDD008 | 183 | 184 | Fault | 0.02 | |
| KSDD008 | 140 | 141 | Phyllite | 0.02 | KSDD008 | 184 | 185 | Fault | 0.02 | |
| KSDD008 | 141 | 142 | Phyllite | 0.01 | KSDD008 | 185 | 186 | Fault | 0.03 | |
| KSDD008 | 142 | 143 | Phyllite | 0.02 | KSDD008 | 186 | 187 | Fault | 0.03 | |
| KSDD008 | 143 | 144 | Phyllite | 0.01 | KSDD008 | 187 | 188 | Phyllite | 0.02 | |
| KSDD008 | 144 | 145 | Phyllite | 0.01 | KSDD008 | 188 | 189 | Phyllite | 0.01 | |
| KSDD008 | 145 | 146 | Phyllite | 0.02 | KSDD008 | 189 | 190 | Phyllite | 0.02 | |
| KSDD008 | 146 | 147 | Phyllite | 0.02 | KSDD008 | 190 | 191 | Phyllite | 0.03 | |
| KSDD008 | 147 | 148 | Phyllite | 0.02 | KSDD008 | 191 | 192 | Phyllite | 0.02 | |
| KSDD008 | 148 | 149 | Phyllite | 0.02 | KSDD008 | 192 | 193 | Phyllite | 0.05 | |
| KSDD008 | 149 | 150 | Phyllite | 0.02 | KSDD008 | 193 | 194 | Phyllite | 0.03 | |
| KSDD008 | 150 | 151 | Phyllite | 0.01 | KSDD008 | 194 | 195 | Phyllite | 0.03 | |
| KSDD008 | 151 | 152 | Phyllite | 0.01 | KSDD008 | 195 | 196 | Phyllite | 0.04 | |
| KSDD008 | 152 | 153 | Phyllite | 0.03 | KSDD008 | 196 | 197 | Phyllite | 0.08 | |
| KSDD008 | 153 | 154 | Phyllite | 0.01 | KSDD008 | 197 | 198 | Phyllite | 0.05 | |
| KSDD008 | 154 | 155 | Phyllite | 0.01 | KSDD008 | 198 | 199 | Phyllite | 0.04 | |
| KSDD008 | 155 | 156 | Phyllite | 0.01 | KSDD008 | 199 | 200 | Phyllite | 0.07 | |
| KSDD008 | 156 | 157 | Phyllite | 0.01 | KSDD008 | 200 | 201 | Phyllite | 0.02 | |
| KSDD008 | 157 | 158 | Phyllite | 0.02 | KSDD008 | 201 | 202 | Phyllite | 0.05 | |
| KSDD008 | 158 | 159 | Phyllite | 0.01 | KSDD008 | 202 | 203 | Phyllite | 0.03 | |
| KSDD008 | 159 | 160 | Phyllite | 0.02 | KSDD008 | 203 | 204 | Phyllite | 0.03 | |
| KSDD008 | 160 | 161 | Phyllite | 0.01 | KSDD008 | 204 | 205 | Phyllite | 0.1 | |
| KSDD008 | 161 | 162 | Phyllite | 0.02 | KSDD008 | 205 | 206 | Phyllite | 0.02 | |
| KSDD008 | 162 | 163 | Phyllite | 0.01 | KSDD008 | 206 | 207 | Phyllite | 0.01 | |
| KSDD008 | 163 | 164 | Phyllite | 0.01 | KSDD008 | 207 | 208 | Phyllite | 0.01 | |
| KSDD008 | 164 | 165 | Phyllite | 0.01 | KSDD008 | 208 | 209 | Phyllite | 0.02 | |
| KSDD008 | 165 | 166 | Phyllite | 0.02 | KSDD008 | 209 | 210 | Phyllite | 0.03 | |
| KSDD008 | 166 | 167 | Phyllite | 0.01 | KSDD008 | 210 | 211 | Phyllite | 0.02 | |
| KSDD008 | 167 | 168 | Phyllite | 0.01 | KSDD008 | 211 | 212 | Phyllite | 0.01 | |
| KSDD008 | 168 | 169 | Phyllite | 0.01 | KSDD008 | 212 | 213 | Phyllite | 0.02 | |
| KSDD008 | 169 | 170 | Phyllite | 0.01 | ||||||
| KSDD008 | 170 | 171 | Phyllite | 0.02 | ||||||
| KSDD008 | 171 | 172 | Phyllite | 0.01 | ||||||
| KSDD008 | 172 | 173 | Phyllite | 0.01 | ||||||
| KSDD008 | 173 | 174 | Phyllite | 0.01 | ||||||
| KSDD008 | 174 | 175 | Phyllite | 0.01 | ||||||
| KSDD008 | 175 | 176 | Phyllite | 0.01 | ||||||
| KSDD008 | 176 | 177 | Phyllite | 0.01 |
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25 November 2022 ASX Announcement ASX: LCL
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JORC Code, 2012 Edition – Table 1- Footprint Resources projects PNG. Imou Licence EL2548
Section 1 Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections.)
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Sampling | • Nature and quality of sampling (eg cut channels, random | •Diamond drilling is carried out to produce PQ, HQ and NQ core. |
| techniques | chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling. |
•Following verification of the integrity of stored core boxes and the core within them at the Company’s core shed in Imou, the core is logged by a Geologist and marked for sampling. Following the marking of the cutting line and allocation of sample numbers, allowing for insertion of QAQC samples, the core is cut by employees in the Company’s facility within the core-shed. |
| • Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. |
•Nominally core is cut in half and sampled on 2m intervals, however the interval may be reduced by the Geologist. |
|
| • Aspects of the determination of mineralisation that are Material to the Public Report. |
•Samples are bagged in numbered calico sacks with a sample tag. Groups of 5 samples are bagged in a heavy-duty plastic bag, labelled, weighed and sealed, for transport. |
|
| • In cases where ‘industry standard’ work has been done this would be relatively simple (eg ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other |
•Transport is via helicopter to a commercial airport, where the samples are couriered with a commercial transport group to the Intertek (ITS) Laboratory in Lae, PNG. |
|
| cases more explanation may be required, such as where | •IM19DD001 - Sample preparation (PB05) is carried out by ITS Laboratory in | |
| there is coarse gold that has inherent sampling problems. | Lae, PNG where the whole sample is dried (105°C), crushed, pulverise | |
| Unusual commodities or mineralisation types (eg submarine | (95%,106µm). Splits are then generated for fire assay (FA50/AAS). | |
| nodules) may warrant disclosure of detailed information. | •Pulp samples (30g) are shipped by ITS to the ITS Laboratory in Townsville, | |
| Australia where the samples are analysed for an additional 48 elements using | ||
| Four Acid ICP-OES & MS package 4A/OM10. | ||
| •Soil samples are collected from C horizon from pits dug with hand tools. | ||
| •Allsoilandrockchip samples are bagged and taggedwithunique sample |
60
==> picture [102 x 68] intentionally omitted <==
25 November 2022 ASX Announcement ASX: LCL
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| identity numbers. | ||
| •Rockchip samples, where possible, are taken from outcrops or saprock | ||
| however during reconnaissance mapping samples from float material may also | ||
| be taken if it is considered to be important to the exploration targeting. | ||
| •Continuous rockchip channel samples were obtained along the length of | ||
| channels dug to C horizon and weathered rock. Channel sample intervals within | ||
| the porphyry style mineralisation are 2m lengths, but may be 1m at the | ||
| geologists discretion. | ||
| •All channel, rock chip grab samples and soil samples are approximately 2kg | ||
| weight. | ||
| Drilling | • Drill type (eg core, reverse circulation, open-hole hammer, | •The drilling program is a diamond drilling program using PQ, HQ, and NQ |
| techniques | rotary air blast, auger, Bangka, sonic, etc) and details (eg | diameter core. All drilling was triple tube and was orientated via the Reflex tool |
| core diameter, triple or standard tube, depth of diamond | and surveys undertaken every 30m using a multi-shot camera. | |
| tails, face-sampling bit or other type, whether core is | ||
| oriented and if so, by what method, etc). | ||
| Drill sample | • Method of recording and assessing core and chip sample | •The drillers are required to meet a minimum recovery rate of 95%. Recoveries |
| recovery | recoveries and results assessed. | in M19DD001 were satisfactory. |
| • Measures taken to maximise sample recovery and ensure | •On site, a Drill Contractor employee is responsible for labelling core blocks the | |
| representative nature of the samples. | beginning and end depth of each drill run plus actual and expected recovery in | |
| • Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to |
meters. This and other field processes are audited on a daily basis by a Company employee during drill core mark up. |
|
| preferential loss/gain of fine/coarse material. | •On receipt the core is visually verified for inconsistencies including depth | |
| labels, degree of fracturing (core breakage versus natural), lithology | ||
| progression etc. If the core meets the required conditions it is cleaned, core | ||
| pieces are orientated and joined, lengths and labelling are verified, and | ||
| geotechnical observations made. The core box is then photographed. | ||
| •Orientated sections of core are aligned and structural measurements taken. | ||
| •Following logging, sample intervals are determined and marked up and the | ||
| cutting line transferred to the core. |
61
==> picture [102 x 68] intentionally omitted <==
25 November 2022 ASX Announcement ASX: LCL
| Criteria | JORC Code explanation | Commentary | Commentary |
|---|---|---|---|
| Logging | • Whether core and chip samples have been geologically and | • | Logging is carried out visually by the Project Geologists focusing on lithology, |
| geotechnically logged to a level of detail to support | structure, alteration, veining, recovery RQD and mineralization characteristics. | ||
| appropriate Mineral Resource estimation, mining studies | The level of logging is appropriate for exploration and initial resource | ||
| and metallurgical studies. | estimation evaluation. | ||
| • Whether logging is qualitative or quantitative in nature. Core | • | All core is photographed following the core “mark up” stage. | |
| (or costean, channel, etc) photography. | • | All core is logged and sampled, nominally on 2m intervals respectively but in | |
| • The total length and percentage of the relevant intersections | areas of interest more dense logging and sampling may be undertaken. | ||
| logged. | • | No sample interval is ever less than 30cm of diamond core. | |
| • | On receipt of the multi-element geochemical data this is interpreted for | ||
| consistency with the geologic logging. | |||
| Sub-sampling | • If core, whether cut or sawn and whether quarter, half or all |
• | After logging and definition of sample intervals by the geologist, the marked |
| techniques | core taken. | core is cut in half using a diamond saw in a specially designed facility on site. | |
| and sample preparation |
• If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. |
All core is cut and sampled. The standard sample interval is 2m but may be varied by the geologist to reflect lithology, alteration or mineralization variations. |
|
| • For all sample types, the nature, quality and appropriateness of the sample preparation technique. |
• | As appropriate, all half or quarter core generated for a specific sample interval is collected and bagged. The other half of the core remains in the core box as |
|
| • Quality control procedures adopted for all sub-sampling | a physical archive. | ||
| stages to maximise representivity of samples. | • | The large size (4-8kg) of individual drill samples and continuous sampling of | |
| • Measures taken to ensure that the sampling is | the drill hole, provides representative samples for exploration activities. | ||
| representative of the in situ material collected, including for instance results for field duplicate/second-half sampling. |
• | Field duplicates were taken to test the geological homogeneity of the mineralization and the sample sizes and procedures. Duplicate samples of drill |
|
| • Whether sample sizes are appropriate to the grain size of | core were obtained by cutting the reference half of the core in half again with a | ||
| the material being sampled. | diamond saw, and taking one of the quarter core samples as the field duplicate | ||
| sample, while leaving the other quarter core for reference. This method may | |||
| introduce a certain amount of additional variance due to the difference in | |||
| sample weights, and is a measure of the geological variability of the | |||
| mineralization and the sample size. | |||
| • | Soil samples are collected from C horizon from pits dug with hand tools. | ||
| • | Allsoilandrockchip samples are bagged and taggedwithunique sample |
62
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25 November 2022 ASX Announcement ASX: LCL
| Criteria | JORC Code explanation | Commentary | Commentary |
|---|---|---|---|
| identity numbers. | |||
| • | Rockchip samples, where possible, are taken from outcrops or saprock | ||
| however during reconnaissance mapping samples from float material may also | |||
| be taken if it is considered to be important to the exploration targeting. | |||
| • | Continuous rockchip channel samples were obtained along the length of | ||
| channels dug to C horizon and weathered rock. Channel sample intervals are | |||
| measured with a tape, and within the porphyry style mineralisation are 2m | |||
| lengths, but may be 1m at the geologists discretion. Geologists log each sample | |||
| interval for geology, alteration, veining, and mineralisation. Continuous rockchip | |||
| sampling is an accepted exploration methodology to obtain a representative | |||
| sample. | |||
| • | All channel, rock chip grab samples and soil samples are approximately 2kg. | ||
| Quality of | • The nature, quality and appropriateness of the assaying and | • |
All sample mediums were submitted to Intertek (ITS) laboratory in Lae for |
| assay data | laboratory procedures used and whether the technique is | sample preparation and Au assay. Pulps are sent to ITS laboratory in | |
| and | considered partial or total. | Townsville, Australia for multi-element assays. ITS are ISO accredited. | |
| laboratory tests |
• For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the |
• | Drill samples: Gold assays were obtained using a lead collection fire assay technique (FA50/AAS) and analyses for an additional 48 elements obtained via |
| analysis including instrument make and model, reading | Four Acid ICP-OES & MS package 4A/OM10. Fire assay for gold is considered | ||
| times, calibrations factors applied and their derivation, etc. | a “total” assay technique. An acid (4 acid) digest is considered a total digestion | ||
| • Nature of quality control procedures adopted (eg standards, blanks, duplicates, external laboratory checks) and whether |
technique. However, for some resistant minerals, not considered of economic value at this time, the digestion may be partial e.g. Zr, Ti etc. |
||
| acceptable levels of accuracy (ie lack of bias) and precision | • | No field non-assay analysis instruments were used in the analyses reported. | |
| have been established. | • | Footprint used certified reference material (OREAS) for drilling QAQC control. | |
| Sample blanks and field duplicates are also inserted into the sample sequence. | |||
| QAQC reference samples make up 15% of a sample batch, made up from | |||
| standards, blanks and duplicates. | |||
| • | Geochemistry results are reviewed by the Company for indications of any | ||
| significant analytical bias or preparation errors in the reported analyses. | |||
| • | Internal laboratory QAQC checks are also reported by the laboratory and are | ||
| reviewed as part of the Company’s QAQC analysis. The geochemical data is |
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| ASX Announcement | |||||
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| Criteria | JORC Code explanation | Commentary | |||
| only accepted where the analyses are performed within acceptable limits. | |||||
| • | Soil samples: The soil samples are prepared using PT01. Gold assays are | ||||
| undertaken in Lae using fire assay (FA25/OE02), while the pulps are sent to | |||||
| ITS Townsville Laboratory for 48 multi-element 4 acid digest 4A/MS.Fire assay | |||||
| for gold is considered a “total” assay technique. An acid (4 acid) digest is | |||||
| considered a total digestion technique. However, for some resistant minerals, | |||||
| not considered of economic value at this time, the digestion may be partial e.g. | |||||
| Zr, Ti etc. | |||||
| • | Footprint Rock Chip Procedures: Rock chip samples are approximately 2kg | ||||
| and collected in calico bags with unique sample ticket, and then placed in thick | |||||
| plastic bags, weighed, labelled, and sealed for shipment to ITS Laboratory in | |||||
| Lae, PNG. The rock samples are prepared via drying, crushing and pulverizing | |||||
| using PT01/PF01. Gold is assayed via lead fire assay using FA50/AAS, while | |||||
| the pulps are sent to ITS Townsville Laboratory for 48 multi-element 4 acid | |||||
| digest 4A/MS. | |||||
| • | No QAQC data (field duplicates, standards, blanks) were undertaken on | ||||
| Footprint trenches/channel samples/soils. The data is reliant on the ITS internal | |||||
| laboratory checks. | |||||
| • | Internal laboratory QA/QC checks are reported by the laboratory and a review | ||||
| of the QA/QC reports suggest the laboratory performed within acceptable | |||||
| limits. | |||||
| Verification of | • The verification of significant intersections by either |
• | All digital data received is verified and validated by Footprint Management | ||
| sampling and | independent or alternative company personnel. | before loading into the assay database. | |||
| assaying | • The use of twinned holes. | • | Reported results are compiled by the Company’s geologists and verified by the | ||
| • Documentation of primary data, data entry procedures, data | Company’s database administrator and exploration manager. | ||||
| verification, data storage (physical and electronic) protocols. | • |
No adjustments to assay data were made. | |||
| • Discuss any adjustment to assay data. | • | All data is stored digitally in a database which has restricted access to | |||
| Footprint database personnel. | |||||
| • | Pulps from the ITS Laboratory for all drilling, trenching and rock chips, are | ||||
| returned toFootprint after3months. Footprint thenstore the samplesina |
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25 November 2022 ASX Announcement ASX: LCL
| Criteria | JORC Code explanation | Commentary | Commentary |
|---|---|---|---|
| secure lock storage container in Lae, PNG. | |||
| Location of | • Accuracy and quality of surveys used to locate drill holes | • | The drill hole is located using a handheld GPS using the averaging function for |
| data points | (collar and down-hole surveys), trenches, mine workings | a minimum of 10 minutes. This has an approximate accuracy of 3-5m | |
| and other locations used in Mineral Resource estimation. | considered sufficient at this stage of exploration. | ||
| • Specification of the grid system used. | • | Downhole deviations of the drill hole are evaluated on a regular basis (30m) | |
| • Quality and adequacy of topographic control. | and recorded in a drill hole survey file to allow plotting in 3D. | ||
| • | Channel samples, soils and rock chips are all located with handheld GPS. | ||
| • | The grid system is WGS84 UTM zones Z54S | ||
| Data spacing | • Data spacing for reporting of Exploration Results. | • | Drill spacing is variable due to topography access. |
| and distribution |
• Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity |
• | The sampling of porphyry Cu-Au mineralisation is undertaken on 2m composites. Vein or structurally controlled styles of mineralisation are sampled |
| appropriate for the Mineral Resource and Ore Reserve | routinely at 1m intervals, but depending on the geologists logging, may be | ||
| estimation procedure(s) and classifications applied. | down to no less than 30cm of NQ half core. | ||
| • Whether sample compositing has been applied. | • | Continuous rock chip channel samples nominally have a length of 2m, which is | |
| sufficient for porphyry style mineralisation, but may be varied to 1m based on | |||
| the Geologists discretion. | |||
| Orientation of | • Whether the orientation of sampling achieves unbiased | • | Drill holes are preferentially located in prospective area. |
| data in relation to geological structure |
sampling of possible structures and the extent to which this is known, considering the deposit type. • If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material. |
• • |
All drillholes are planned to best test the lithologies, mineralisation and structures as known, taking into account that steep topography limits alternatives for locating holes. Drill holes discussed within this announcement are oriented to intercept major mineralised structures approximately perpendicular to strike where such information is known or suspected. |
| • | The nature and extent of the soil geochemical sampling achieves an unbiased | ||
| representation of the distribution of the elements assayed. | |||
| • | The nature and extent of the rockchip channel samples is limited to the channel. | ||
| The sample results were accompanied by mapping to indicate the orientation of | |||
| the key mineralized structures. |
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| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| •Exploration is at an early stage and, as such, knowledge on exact locations of | ||
| mineralisation and its relation to structural boundaries is not accurately known. | ||
| However, the sampling pattern is considered appropriate for the program to | ||
| reasonably assess the prospectivity of known features interpreted from other | ||
| data sources. | ||
| Sample | • The measures taken to ensure sample security. | •All core boxes are stored on concrete platforms with lids and strapped down in |
| security | a timber and wire frame. | |
| •On receipt at the core shed the core boxes are examined for integrity. If there | ||
| are no signs of damage or violation of the boxes, they are opened, and the | ||
| core is evaluated for consistency and integrity. | ||
| •The core shed and all core boxes, samples and pulps are secured in the | ||
| Company core yard facility. | ||
| •All sample dispatches are secured and labelled on site. Groups of 5 samples | ||
| are bagged in a heavy-duty plastic bag, labelled, weighed and sealed, for | ||
| transport. | ||
| •Transport is via helicopter to a commercial airport, where the samples are | ||
| couriered with a commercial transport group to the Intertek (ITS) Laboratory in | ||
| Lae, PNG. | ||
| Audits or | • The results of any audits or reviews of sampling techniques | •At this stage no audits have been undertaken. |
| reviews | and data. |
Section 2 Reporting of Exploration Results – Footprint Resources projects PNG. Imou Licence EL2548
(Criteria listed in the preceding section also apply to this section.)
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Mineral | • Type, reference name/number, location and | •The Exploration Titles were validly issued as Exploration Licences pursuant to the 1992 |
| tenement and | ownership including agreements or material |
Mining Act. |
| land tenure status |
issues with third parties such as joint ventures, partnerships, overriding royalties, native title |
•The Exploration Licence grants its holders the exclusive right to carrying out exploration for minerals onthatland. There areno outstanding encumbrances orchargesregistered |
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| Criteria | JORC Code explanation | Commentary | ||
|---|---|---|---|---|
| interests, historical sites, wilderness or national | against the Exploration Title at the National Registry. | |||
| park and environmental settings. | ||||
| • The security of the tenure held at the time of | ||||
| reporting along with any known impediments to | ||||
| obtaining a licence to operate in the area. | ||||
| Exploration | • Acknowledgment and appraisal of exploration | •Imou Project: Previous explorers of the Imou Project area include: | 1971-74 US Steel, | |
| done by other | by other parties. |
regional stream sediment sampling. 1982-1991 Kennecott-Niugini | Mining JV, regional | |
| parties | sampling, soils, rock chips. 1993-2004 Highlands Pacific-Cyprus Amax JV, mapping, soils, | |||
| rock chips, 2 DDH for 409.9m. | ||||
| Geology | • Deposit type, geological setting and style of | •The Imou Project in centred on a porphyry Cu-Au system that spans 3km x 1km area. The | ||
| mineralisation. | mineralisation is associated with a multi-phase Miocene intrusive complex of intermediate | |||
| composition. The Cu-Au mineralisation is dominated by porphyry style veining | hosted within | |||
| pre-mineral diorite, and then a series of intra-mineral porphyries have been identified. Other | ||||
| prospects within the Imou region range from skarn (High Creek), to Intermediate | ||||
| Sulphidation veins (Michael’s Creek). | ||||
| Drill hole | • A summary of all information material to the | |||
| Information | understanding of the exploration results including a tabulation of the following |
HOLE EASTING NORTHING RL (m) EOH (m) |
AZIMUTH | DIP |
| information for all Material drill holes: | IM19DD001 700118 9452966 817 599.6 |
134 | 50 | |
o easting and northing of the drill hole collar |
||||
o elevation or RL (Reduced Level – elevation |
||||
| above sea level in metres) of the drill hole | •During the 2019-2020 drill programme, Footprint drilled a total of 12 diamond holes for | |||
| collar | 4530.6m. Two historical holes were drilling by Niugini Mining Ltd & | Cyprus-Amax JV in 1999 | ||
o dip and azimuth of the hole |
for 409.9m. Hole IM19DD001 is the only material hole drilled by Footprint. | |||
o down hole length and interception depth |
||||
o hole length. |
||||
| • If the exclusion of this information is justified on | ||||
| the basis that the information is not Material and | ||||
| this exclusion does not detract from the | ||||
| understanding of the report, the Competent |
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| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Person should clearly explain why this is the | ||
| case. | ||
| Data | • In reporting Exploration Results, weighting | •No metal equivalent values have been stated. |
| aggregation methods |
averaging techniques, maximum and/or minimum grade truncations (eg cutting of high grades) and cut-off grades are usually Material |
•Quoted drill intervals use a weighted average compositing method of all assays within the interval. Uncut intervals include values below 0.1 g/t Au. |
| and should be stated. | •No cut of high grades has been done. | |
| • Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some |
•All widths quoted are intercept widths, not true widths, as there is insufficient information at this stage of exploration to know the geometries within the system. •The summary metrics for the soil and rockchip channel sample results have been averaged and reported as uncut values. |
|
| typical examples of such aggregations should | ||
| be shown in detail. | ||
| • The assumptions used for any reporting of | ||
| metal equivalent values should be clearly | ||
| stated. | ||
| Relationship | • These relationships are particularly important in | •Drill holes discussed within this announcement are oriented to intercept major mineralised |
| between | the reporting of Exploration Results. | structures approximately perpendicular to strike where known or suspected. Efforts were |
| mineralisation widths and intercept lengths |
• If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported. |
made to intercept the mineralization as perpendicular as possible to derive a best estimate of the true thickness of the mineralization. |
| • If it is not known and only the down hole lengths | ||
| are reported, there should be a clear statement | ||
| to this effect (eg ‘down hole length, true width | ||
| not known’). | ||
| Diagrams | • Appropriate maps and sections (with scales) | •Tabulations of IM19DD001 assays provided as Table 7. Detailed supporting maps and |
| and tabulations of intercepts should be included | sections are not provided in this ASX release as the Company does not view the drill assays |
|
| for any significant discovery being reported | as a significant discovery at this stage. | |
| These should include, but not be limited to a | ||
| plan view of drill hole collar locations and | ||
| appropriate sectional views. |
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| Criteria | JORC Code explanation | Commentary | ||||||
|---|---|---|---|---|---|---|---|---|
| Balanced | • Where comprehensive reporting of all | •Reporting is considered balanced. | ||||||
| reporting | Exploration Results is not practicable, | |||||||
| representative reporting of both low and high | ||||||||
| grades and/or widths should be practiced to | ||||||||
| avoid misleading reporting of Exploration | ||||||||
| Results. | ||||||||
| Other | • Other exploration data, if meaningful and | •No QAQC data (field duplicates, standards, blanks) were | undertaken on Footprint trenches. | |||||
| substantive | material, should be reported including (but not | The data is reliant on the ITS internal | laboratory checks. | |||||
| exploration data |
limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock |
•Logs of soil, rock chip and trenches are generated in the field and material data later transferred by a Geologist to the Company’s database. When available and after review, QA/QC compliant assay data is also transferred to the Company’s database by a qualified database manager. |
||||||
| characteristics; potential deleterious or | Sample specifically referenced in text | |||||||
| contaminating substances. | Sample ID EASTING WGS84 Z54S |
NORTHING WGS84 Z54S |
Lithology | Au g/t | ||||
| Qtz-sulphide | ||||||||
| FT1647 693317 |
9452651 | vein | 58.5 | |||||
| •All pulps are collected from the Laboratory after 3 months and stored in a locked container | ||||||||
| with security. | ||||||||
| Further work | • The nature and scale of planned further work | •Further trenching of the high grade Cu-Au breccia intersected in IM19DD001 is | proposed. | |||||
| (eg tests for lateral extensions or depth | ||||||||
| extensions or large-scale step-out drilling). | ||||||||
| • Diagrams clearly highlighting the areas of | ||||||||
| possible extensions, including the main | ||||||||
| geological interpretations and future drilling | ||||||||
| areas, provided this information is not | ||||||||
| commercially sensitive. |
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JORC Code, 2012 Edition – Table 1- Footprint Resources projects PNG. Ono Licence EL2665
Section 1 Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections.)
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Sampling | • Nature and quality of sampling (eg cut channels, random | •Diamond Drilling completed by Pacific Nuigini Limited(ASX:PNR)see ASX |
| techniques | chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling. |
release 29th January 2014.All drilling undertaken at the Kusi Prospect has been completed using diamond trilling techniques. Holes were drilled commencing in PQ with size reducing to HQ and NQ as required for satisfactory hole advance, core recovery maximisation and hole stability. All drilling was undertaken using triple tube techniques to maximise core recovery. |
| • Include reference to measures taken to ensure sample representivity and the appropriate calibration of any |
This core was geologically logged in 1m or less intervals, and subsequently halved on site for sampling. |
|
| measurement tools or systems used. | •Lower Limestone Trench completed by CRA (Rio Tinto), Trench KSTC45A | |
| • Aspects of the determination of mineralisation that are Material to the Public Report. |
completed by Pacific Niugini Limited (ASX:PNR). Data sourced from PNG Minerals Authority public database. Specific sampling, handling and lab techniques are not recorded. |
|
| • In cases where ‘industry standard’ work has been done this would be relatively simple (eg ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other |
•Trench Ssamples are bagged in numbered calico sacks with a unique sample tag. Groups of 5 samples are bagged in a heavy duty plastic bag, labelled, weighed and sealed, for transport. |
|
| cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (eg submarine |
•Transport is via helicopter to Lae, where the samples are transported in a secure vehicle to the Intertek (ITS) Laboratory. |
|
| nodules) may warrant disclosure of detailed information. | •Rockchip samples, where possible, are taken from outcrops or saprock | |
| however during reconnaissance mapping samples from float material may also | ||
| be taken if it is considered to be important to the exploration targeting. | ||
| •Continuous rockchip channel samples were obtained along the length of | ||
| channels dug to C horizon and weathered rock. Channel sample intervals within | ||
| the porphyry style mineralisation are 2m lengths, but may be 1m at the | ||
| geologists discretion. | ||
| •Allchannel,rockchip grab samples and soilsamples are approximately2kgin |
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| Criteria | JORC Code explanation | Commentary | Commentary |
|---|---|---|---|
| weight. | |||
| Drilling | • Drill type (eg core, reverse circulation, open-hole hammer, | • | All drilling undertaken at the Kusi Prospect has been completed using diamond |
| techniques | rotary air blast, auger, Bangka, sonic, etc) and details (eg | trilling techniques. Holes are drilled commencing in PQ with size reducing to | |
| core diameter, triple or standard tube, depth of diamond | HQ and NQ as required for satisfactory hole advance, core recovery | ||
| tails, face-sampling bit or other type, whether core is | maximisation and hole stability. All drilling is undertaken using triple tube | ||
| oriented and if so, by what method, etc). | techniques to maximise core recovery | ||
| Drill sample | • Method of recording and assessing core and chip sample | • | All geology input was logged and validated by the relevant area geologists. No |
| recovery | recoveries and results assessed. | defined relationship exists between sample recovery and grade. Nor has | |
| • Measures taken to maximise sample recovery and ensure representative nature of the samples. |
sample bias due to preferential loss or gain of fine or coarse material been noted. |
||
| • Whether a relationship exists between sample recovery and | |||
| grade and whether sample bias may have occurred due to | |||
| preferential loss/gain of fine/coarse material. | |||
| Logging | • Whether core and chip samples have been geologically and | • | Drill core was logged geologically by the project geologist to accepted industry |
| geotechnically logged to a level of detail to support | standards capturing lithology, mineralology and structural measurements. All | ||
| appropriate Mineral Resource estimation, mining studies | core was photographed for future reference. | ||
| and metallurgical studies. | |||
| • Whether logging is qualitative or quantitative in nature. Core | |||
| (or costean, channel, etc) photography. | |||
| • The total length and percentage of the relevant intersections | |||
| logged. | |||
| Sub-sampling | • If core, whether cut or sawn and whether quarter, half or all |
• | Diamond Drilling - Half-core samples, sub-set via geological features as |
| techniques | core taken. | appropriate. | |
| and sample preparation |
• If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. |
• • |
Samples undergo fine pulverisation of the entire sample in accordance with the independent certified laboratory's procedures.• QA/QC was ensured during the sub-sampling stages process via the use of the |
| • For all sample types, the nature, quality and | systems of an independent NATA / ISO accredited laboratory contractor.• | ||
| appropriateness of the sample preparation technique. | • | Drill core sample size is considered appropriate for the grain size of the | |
| • Quality control procedures adopted for all sub-sampling | • | material being sampled.• The un-sampledhalfofdiamond corewasretainedforchecksampling/logging |
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| Criteria | JORC Code explanation | Commentary | Commentary |
|---|---|---|---|
| stages to maximise representivity of samples. | if required. | ||
| • Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second-half sampling. |
• • |
All soil and rockchip samples are bagged and tagged with unique sample identity numbers. Rockchip samples, where possible, are taken from outcrops or saprock however during reconnaissance mapping samples from float material may also |
|
| • Whether sample sizes are appropriate to the grain size of | be taken if it is considered to be important to the exploration targeting. | ||
| the material being sampled. | • | Continuous rockchip channel samples were obtained along the length of | |
| channels dug to C horizon and weathered rock. Channel sample intervals are | |||
| measured with a tape, and within the porphyry style mineralisation are 2m | |||
| lengths, but may be 1m at the geologist’s discretion. Geologists log each sample | |||
| interval for geology, alteration, veining and mineralisation. Continuous rockchip | |||
| sampling is an accepted exploration methodology to obtain a representative | |||
| sample. No QAQC data (field duplicates, standards, blanks) were undertaken on | |||
| Footprint trenches. The data is reliant on the ITS internal laboratory checks | |||
| which involves insertion of duplicates, blanks and standards. ITS are ISO | |||
| accredited and part of Intertek. | |||
| • | All channel, rock chip grab samples and soil samples are approximately 2kg. | ||
| Quality of | • The nature, quality and appropriateness of the assaying and | • |
Drilling was analysed by fire assay. A 50g sample undergoes fire assay lead |
| assay data | laboratory procedures used and whether the technique is | collection followed by flame atomic adsorption spectrometry. Quality control is | |
| and | considered partial or total. | ensured via the use of standards, blanks and duplicates. ICP samples are | |
| laboratory tests |
• For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading |
assayed in an independent certified laboratory using validly calibrated equipment. No significant QA/QC issues have arisen in drilling results. These assay methodologies are appropriate for the resource in question. |
|
| times, calibrations factors applied and their derivation, etc. | • | All surface samples were submitted to Intertek (ITS) laboratory in Lae for | |
| • Nature of quality control procedures adopted (eg standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (ie lack of bias) and precision have been established. |
sample preparation and Au assay. Pulps are sent to ITS laboratory in Townsville, Australia for multi-element assays. Gold assays were obtained using a lead collection fire assay technique (FA50/AAS) and analyses for an additional 48 elements obtained via Four Acid ICP-OES & MS package 4A/OM10 |
||
| • | Fire assay for gold is considered a “total” assay technique. | ||
| • | An acid (4 acid) digest is considered a total digestion technique. However, for | ||
| some resistant minerals, not considered of economic value at this time, the |
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| Criteria | JORC Code explanation | Commentary | Commentary |
|---|---|---|---|
| digestion may be partial e.g. Zr, Ti etc. | |||
| • | No field non-assay analysis instruments were used in the analyses reported. | ||
| • | Geochemistry results are reviewed by the Company for indications of any | ||
| significant analytical bias or preparation errors in the reported analyses. | |||
| • | Internal laboratory QAQC checks are also reported by the laboratory and are | ||
| reviewed as part of the Company’s QAQC analysis. The geochemical data is | |||
| only accepted where the analyses are performed within acceptable limits. | |||
| Verification of | • The verification of significant intersections by either |
• | Anomalous drill core intervals as well as random intervals were routinely |
| sampling and | independent or alternative company personnel. | checked assayed as part of the internal QA/QC process. Blanks and laboratory | |
| assaying | • The use of twinned holes. | standards were routinely assayed in accordance with laboratory procedure and primary data was loaded into the drillhole database system and then archived |
|
| • Documentation of primary data, data entry procedures, data | for reference.• | ||
| verification, data storage (physical and electronic) protocols. | • |
No primary drill assays data was modified in any way | |
| • Discuss any adjustment to assay data. | • | All digital data received is verified and validated by Footprint Management | |
| before loading into the assay database. | |||
| • | Reported results are compiled by the Company’s geologists and verified by the | ||
| Company’s database administrator and exploration manager. | |||
| • | No adjustments to surface assay data were made. | ||
| • | All data is stored digitally in a database which has restricted access to | ||
| Footprint database personnel. | |||
| • | Pulps from the ITS Laboratory for all drilling, are returned to Footprint after 3 | ||
| months. Footprint then store the samples in a secure lock storage container in | |||
| Lae, PNG. | |||
| Location of | • Accuracy and quality of surveys used to locate drill holes | • | All drill data was spatially oriented by survey controls via initial GPS |
| data points | (collar and down-hole surveys), trenches, mine workings | positioning, followed by certified surveyor pick-ups. Drillholes were all surveyed | |
| and other locations used in Mineral Resource estimation. | downhole, with single / multishot cameras | ||
| • Specification of the grid system used. | • | The trenches are located using a handheld GPS using the averaging function | |
| for a minimum of 10 minutes. This has an approximate accuracy of 3-5m |
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| Criteria | JORC Code explanation | Commentary | Commentary |
|---|---|---|---|
| • Quality and adequacy of topographic control. | considered sufficient at this stage of exploration. | ||
| • | The grid system is WGS84 UTM zones Z55S. | ||
| Data spacing | • Data spacing for reporting of Exploration Results. | • | No standard spacing currently exists for drill holes |
| and distribution |
• Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity |
• | Continuous rock chip channel samples nominally have a length of 2m, but may be varied to 1m based on the Geologists discretion. |
| appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied. |
• | Trenching of skarn mineralisation that has an underlying stratigraphic control, is undertaken where possible or known, perpendicular (across) to the |
|
| • Whether sample compositing has been applied. | stratigraphy, to try and achieve true thickness intervals. | ||
| Orientation of | • Whether the orientation of sampling achieves unbiased | • | Where possible holes were drilled to return true widths of |
| data in | sampling of possible structures and the extent to which this | interpreted/postulated ore zones. It is not considered that drilling orientation | |
| relation to | is known, considering the deposit type. | has introduced an appreciable sampling bias | |
| geological structure |
• If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to |
• | Trenching of skarn mineralisation that has an underlying stratigraphic control, is undertaken where possible or known, perpendicular (across) to the |
| have introduced a sampling bias, this should be assessed | stratigraphy, to try and achieve true thickness intervals. | ||
| and reported if material. | |||
| Sample | • The measures taken to ensure sample security. | • | Drill core samples were delivered directly to the independent laboratory |
| security | contractor under the company’s supervision using company employees. | ||
| Samples were stored securely until they leave site. | |||
| • | All surface sample dispatches are secured and labelled on site. Groups of 5 | ||
| samples are bagged in a heavy duty plastic bag, labelled, weighed and sealed, | |||
| for transport. | |||
| • | Transport is via helicopter to a commercial airport, where the samples are | ||
| couriered with a commercial transport group to the Intertek (ITS) Laboratory in | |||
| Lae, PNG. | |||
| Audits or | • The results of any audits or reviews of sampling techniques | • | Drill core site sampling techniques and data bases were routinely verified by |
| reviews | and data. | senior geologists and the company’s executive director. |
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Section 2 Reporting of Exploration Results – Footprint Resources projects PNG. Ono Licence EL2665
(Criteria listed in the preceding section also apply to this section.)
| Criteria JORC Code explanation |
Commentary | Commentary | Commentary | Commentary | Commentary | Commentary | Commentary |
|---|---|---|---|---|---|---|---|
| Mineral tenement and land tenure status • Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings. • The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area. |
• The Exploration Titles were validly issued as Exploration Licences pursuant to the 1992 Mining Act. •The Exploration Licence grants its holders the exclusive right to carrying out exploration for minerals on that land. There are no outstanding encumbrances or charges registered against the Exploration Title at the National Registry. |
||||||
| Exploration done by other parties • Acknowledgment and appraisal of exploration by other parties. |
•Kusi Project: Pacific Niugini Limited (PNR) 2010-2020. Stream sampling, soils, rock chips, trenching, aeromagnetics, 8 diamond holes for 2466.7m at Kusi Project. |
||||||
| Geology • Deposit type, geological setting and style of mineralisation. |
•Kusi Project: The Kusi Project is dominated by skarn mineralisation hosted in multiple limestone units within the Owen Stanley metamorphics. Numerous intermediate to felsic dykes transect the project area. Minor Intermediate Sulphidation veins have also been noted. |
||||||
| Drill hole Information • A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes: o easting and northing of the drill hole collaro elevation or RL (Reduced Level – elevation above sealevel in metres) of the drill hole collar o dip and azimuth of the holeo down hole length and interception deptho hole length.• If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does |
Down holes lengths and intercepts are reported in the announcement Hole ID East North RL Azi(True) Dip EOH (m) KSDD001 494157 9134794 1930 6.67 -55 268.6 KSDD002 494157 9134794 1930 6.67 -75 224.6 KSDD003 494006 9134412 1865 71.67 -60 364.6 KSDD004 493580 9134400 2021 231.67 -75 376.8 KSDD005 493850 9134840 2035 156.67 -60 98.8 KSDD006 493850 9134843 2038 156.67 -70 459.3 KSDD007 493631 9134558 2064 196.67 -70 461 KSDD008 494148 9134881 1909 197 -60 213 |
||||||
| Hole ID | East | North | RL | Azi(True) | Dip | EOH (m) | |
| KSDD001 | 494157 | 9134794 | 1930 | 6.67 | -55 | 268.6 | |
| KSDD002 | 494157 | 9134794 | 1930 | 6.67 | -75 | 224.6 | |
| KSDD003 | 494006 | 9134412 | 1865 | 71.67 | -60 | 364.6 | |
| KSDD004 | 493580 | 9134400 | 2021 | 231.67 | -75 | 376.8 | |
| KSDD005 | 493850 | 9134840 | 2035 | 156.67 | -60 | 98.8 | |
| KSDD006 | 493850 | 9134843 | 2038 | 156.67 | -70 | 459.3 | |
| KSDD007 | 493631 | 9134558 | 2064 | 196.67 | -70 | 461 | |
| KSDD008 | 494148 | 9134881 | 1909 | 197 | -60 | 213 | |
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| Criteria | JORC Code explanation | Commentary | |
|---|---|---|---|
| not detract from the understanding of the report, the | |||
| Competent Person should clearly explain why this is the | |||
| case. | |||
| Data | • In reporting Exploration Results, weighting averaging | •No metal equivalent values have been stated. | |
| aggregation methods |
techniques, maximum and/or minimum grade truncations (eg cutting of high grades) and cut-off grades are usually Material and should be stated. |
•No cut of high grades has been done. •All widths quoted are intercept widths. |
|
| •Drill results are generally reported at a cut off of 0.2g/tAu, however lower grade | |||
| • Where aggregate intercepts incorporate short lengths of high | dilution intervals are reported where broad zones of lower grade zones may be |
||
| grade results and longer lengths of low grade results, the | material in exploration for a potential underlying porphyry | ||
| procedure used for such aggregation should be stated and | |||
| some typical examples of such aggregations should be | |||
| shown in detail. | |||
| • The assumptions used for any reporting of metal equivalent | |||
| values should be clearly stated. | |||
| Relationship | • These relationships are particularly important in the reporting | •Drill hole interval widths are downhole width and may not represent true width |
|
| between | of Exploration Results. | unless otherwise stated. | |
| mineralisation widths and intercept lengths |
• If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported. • If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (eg |
•The Kusi trenches reported (Footprint trench 1 and Leah’s Lode trench) are taken perpendicular (across) stratigraphy as the mineralisation is skarn- replacement in style. This gives a more accurate result which is approximately “true thickness” to the mineralisation. |
|
| ‘down hole length, true width not known’). | |||
| Diagrams | • Appropriate maps and sections (with scales) and tabulations | •Geological maps showing the location of drill holes, trenches and exploration | |
| of intercepts should be included for any significant discovery | results are shown in the body of the announcement. | ||
| being reported These should include, but not be limited to a | |||
| plan view of drill hole collar locations and appropriate | |||
| sectional views. | |||
| Balanced | • Where comprehensive reporting of all Exploration Results is | •Reporting is considered balanced. | |
| reporting | not practicable, representative reporting of both low and high | ||
| grades and/or widths should be practiced to avoid | |||
| misleading reporting of Exploration Results. |
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| Criteria | JORC Code explanation | Commentary | |
|---|---|---|---|
| Other | • Other exploration data, if meaningful and material, should be | •No QAQC data (field duplicates, standards, blanks) were undertaken on |
|
| substantive | reported including (but not limited to): geological | Footprint trenches. The data is reliant on the ITS internal laboratory checks. | |
| exploration data |
observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances. |
•Logs of soil, rock chip and trenches are generated in the field and material data later transferred by a Geologist to the Company’s database. When available and after review, QA/QC compliant assay data, based on ITS internal QA/QC procedures, is also transferred to the Company’s database by a qualified database Manager. |
|
| •All pulps are collected from the Laboratory after 3 months and stored in a | |||
| locked container with security. | |||
| Further work | • The nature and scale of planned further work (eg tests for | •Continued trenching, mapping, soils sampling and drilling is planned for the | |
| lateral extensions or depth extensions or large-scale step- | Kusi target. | ||
| out drilling). | |||
| • Diagrams clearly highlighting the areas of possible | |||
| extensions, including the main geological interpretations and | |||
| future drilling areas, provided this information is not | |||
| commercially sensitive. |
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JORC Code, 2012 Edition – Table 1- Footprint Resources projects PNG. Liamu/Veri Veri Project Licence EL2432 (Liamu), EL2706 (Awala)
Section 1 Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections.)
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Sampling | • Nature and quality of sampling (eg cut channels, random | •Very Veri rock chip samples 611751 and GMXR901 were completed by |
| techniques | chips, or specific specialised industry standard | Goldminex (ASX:GMX) see release 9 April 2008 with assays conducted at SGS |
| measurement tools appropriate to the minerals under | Townsville. Specific sampling, handling and laboratory techniques are | |
| investigation, such as down hole gamma sondes, or | unknown. | |
| handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling. |
•Samples are bagged in numbered calico sacks with a unique sample tag. Groups of 5 samples are bagged in a heavy duty plastic bag, labelled, weighed |
|
| • Include reference to measures taken to ensure sample | and sealed, for transport. | |
| representivity and the appropriate calibration of any measurement tools or systems used. |
•Transport is via helicopter to a secure Footprint laydown yard, where the samples are transported in a secure vehicle to Port Moresby for commercial air |
|
| • Aspects of the determination of mineralisation that are | freight to the Intertek (ITS) Laboratory in Lae. | |
| Material to the Public Report. | •Rockchip samples, where possible, are taken from outcrops or saprock | |
| • In cases where ‘industry standard’ work has been done this | however during reconnaissance mapping samples from float material may also | |
| would be relatively simple (eg ‘reverse circulation drilling | be taken if it is considered to be important to the exploration targeting. | |
| was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (eg submarine |
•Continuous rockchip channel samples were obtained along the length of channels dug to C horizon and weathered rock. Channel sample intervals within the porphyry style mineralisation are 2m lengths, but may be 1m at the geologists discretion. |
|
| nodules) may warrant disclosure of detailed information. | •All channel, rock chip grab samples and soil samples are approximately 2kg in | |
| weight. | ||
| •Soil samples are collected from C horizon from pits dug with hand tools, or via a | ||
| hand held or mechanical auger. |
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| Criteria | JORC Code explanation | Commentary | Commentary |
|---|---|---|---|
| Drilling | • Drill type (eg core, reverse circulation, open-hole hammer, | • | NA |
| techniques | rotary air blast, auger, Bangka, sonic, etc) and details (eg | ||
| core diameter, triple or standard tube, depth of diamond | |||
| tails, face-sampling bit or other type, whether core is | |||
| oriented and if so, by what method, etc). | |||
| Drill sample | • Method of recording and assessing core and chip sample | • | NA |
| recovery | recoveries and results assessed. | ||
| • Measures taken to maximise sample recovery and ensure | |||
| representative nature of the samples. | |||
| • Whether a relationship exists between sample recovery and | |||
| grade and whether sample bias may have occurred due to | |||
| preferential loss/gain of fine/coarse material. | |||
| Logging | • Whether core and chip samples have been geologically and | • | NA |
| geotechnically logged to a level of detail to support | |||
| appropriate Mineral Resource estimation, mining studies | |||
| and metallurgical studies. | |||
| • Whether logging is qualitative or quantitative in nature. Core | |||
| (or costean, channel, etc) photography. | |||
| • The total length and percentage of the relevant intersections | |||
| logged. | |||
| Sub-sampling | • If core, whether cut or sawn and whether quarter, half or all |
• | All soil and rockchip samples are bagged and tagged with unique sample |
| techniques | core taken. | identity numbers. | |
| and sample preparation |
• If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. |
• | Rockchip samples, where possible, are taken from outcrops or saprock however during reconnaissance mapping samples from float material may also be taken if it is considered to be important to the exploration targeting. |
| • For all sample types, the nature, quality and appropriateness of the sample preparation technique. |
• | Continuous rockchip channel samples were obtained along the length of channels dug to C horizon and weathered rock. Channel sample intervals are |
|
| • Quality control procedures adopted for all sub-sampling | measured with a tape, and within the porphyry style mineralisation are 2m | ||
| stages to maximise representivity of samples. | lengths, but may be 1m at the geologist’s discretion. Geologists log each sample | ||
| • Measures taken to ensure that the sampling is | interval for geology, alteration, veining, and mineralisation. Continuous rockchip |
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| Criteria | JORC Code explanation | Commentary | Commentary |
|---|---|---|---|
| representative of the in situ material collected, including for | sampling is an accepted exploration methodology to obtain a representative | ||
| instance results for field duplicate/second-half sampling. | sample. No QAQC data (field duplicates, standards, blanks) were undertaken on | ||
| • Whether sample sizes are appropriate to the grain size of the material being sampled. |
Footprint trenches. The data is reliant on the ITS internal laboratory checks which involves insertion of duplicates, blanks and standards. ITS are ISO accredited and part of Intertek. |
||
| • | All channel, rock chip grab samples and soil samples are approximately 2kg. | ||
| Quality of | • The nature, quality and appropriateness of the assaying and | • |
All samples were submitted to Intertek (ITS) laboratory in Lae for sample |
| assay data | laboratory procedures used and whether the technique is | preparation and Au assay. Pulps are sent to ITS laboratory in Townsville, | |
| and | considered partial or total. | Australia for multi-element assays. Gold assays were obtained using a lead | |
| laboratory tests |
• For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the |
collection fire assay technique (FA50/AAS) and analyses for an additional 48 elements obtained via Four Acid ICP-OES & MS package 4A/OM10 |
|
| analysis including instrument make and model, reading | • | Fire assay for gold is considered a “total” assay technique. | |
| times, calibrations factors applied and their derivation, etc. | • | An acid (4 acid) digest is considered a total digestion technique. However, for | |
| • Nature of quality control procedures adopted (eg standards, | some resistant minerals, not considered of economic value at this time, the | ||
| blanks, duplicates, external laboratory checks) and whether | digestion may be partial e.g. Zr, Ti etc. | ||
| acceptable levels of accuracy (ie lack of bias) and precision have been established. |
• | No field non-assay analysis instruments were used in the analyses reported. | |
| • | Geochemistry results are reviewed by the Company for indications of any | ||
| significant analytical bias or preparation errors in the reported analyses. | |||
| • | Internal laboratory QAQC checks are also reported by the laboratory and are | ||
| reviewed as part of the Company’s QAQC analysis. The geochemical data is | |||
| only accepted where the analyses are performed within acceptable limits. | |||
| Verification of | • The verification of significant intersections by either |
• | All digital data received is verified and validated by Footprint Management |
| sampling and | independent or alternative company personnel. | before loading into the assay database. | |
| assaying | • The use of twinned holes. | • | Reported results are compiled by the Company’s geologists and verified by the |
| • Documentation of primary data, data entry procedures, data | Company’s database administrator and exploration manager. | ||
| verification, data storage (physical and electronic) protocols. | • |
No adjustments to assay data were made. | |
| • Discuss any adjustment to assay data. | • | All data is stored digitally in a database which has restricted access to | |
| Footprint database personnel. |
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| Criteria | JORC Code explanation | Commentary | Commentary |
|---|---|---|---|
| • | Pulps from the ITS Laboratory for all drilling are returned to Footprint after 3 | ||
| months. Footprint then store the samples in a secure lock storage container in | |||
| Lae, PNG. | |||
| Location of | • Accuracy and quality of surveys used to locate drill holes | • | The trenches are located using a handheld GPS using the averaging function |
| data points | (collar and down-hole surveys), trenches, mine workings | for a minimum of 10 minutes. This has an approximate accuracy of 3-5m | |
| and other locations used in Mineral Resource estimation. | considered sufficient at this stage of exploration. | ||
| • Specification of the grid system used. | • | The grid system is WGS84 UTM zones Z55S. | |
| • Quality and adequacy of topographic control. | |||
| Data spacing | • Data spacing for reporting of Exploration Results. | • | Continuous rock chip channel samples nominally have a length of 2m, but may |
| and distribution |
• Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity |
• | be varied to 1m based on the Geologists discretion. Trenching of porphyry style mineralisation (Dada) is undertaken at 2m |
| appropriate for the Mineral Resource and Ore Reserve | intervals, and is considered an acceptable sample density for the style of | ||
| estimation procedure(s) and classifications applied. | mineralisation. | ||
| • Whether sample compositing has been applied. | |||
| Orientation of | • Whether the orientation of sampling achieves unbiased | • | Trenching of porphyry style mineralisation (Dada) is undertaken at 2m |
| data in | sampling of possible structures and the extent to which this | intervals, and is considered an acceptable sample density for the style of | |
| relation to | is known, considering the deposit type. | mineralisation. Mapping of the porphyry veins and orientation assist with | |
| geological structure |
• If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to |
defining trench orientation to avoid any geological bias. | |
| have introduced a sampling bias, this should be assessed | |||
| and reported if material. | |||
| Sample | • The measures taken to ensure sample security. | • | All sample dispatches are secured and labelled on site. Groups of 5 samples |
| security | are bagged in a heavy duty plastic bag, labelled, weighed and sealed, for | ||
| transport. | |||
| • | Transport is via helicopter to a secure Footprint laydown yard, where the | ||
| samples are transported in a secure vehicle to Port Moresby for commercial air | |||
| freight to the Intertek (ITS) Laboratory in Lae. |
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| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Audits or | • The results of any audits or reviews of sampling techniques | •At this stage no audits have been undertaken. |
| reviews | and data. |
Section 2 Reporting of Exploration Results – Footprint Resources projects PNG. Liamu/Veri Veri Project Licence EL2432 (Liamu), EL2706 (Awala)
(Criteria listed in the preceding section also apply to this section.)
| Criteria | JORC Code explanation | Commentary | |
|---|---|---|---|
| Mineral | • Type, reference name/number, location and ownership | •The Exploration Titles were validly issued as Exploration Licences pursuant to | |
| tenement and | including agreements or material issues with third parties |
the 1992 Mining Act. | |
| land tenure status |
such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings. |
•The Exploration Licence grants its holders the exclusive right to carrying out exploration for minerals on that land. There are no outstanding encumbrances or charges registered against the Exploration Title at the National Registry. |
|
| • The security of the tenure held at the time of reporting along | |||
| with any known impediments to obtaining a licence to | |||
| operate in the area. | |||
| Exploration | • Acknowledgment and appraisal of exploration by other | •The Liamu licence areas have seen ongoing exploration including BHP, CRA, | |
| done by other | parties. |
Elders, AOG Minerals Highlands Pacific and Goldminex. | |
| parties | •The bulk of the targeted work that continued to drilling testing was undertaken | ||
| by Goldminex (GMX) from 2007- 2014. This work included 23 holes for 7195m | |||
| across multiple project areas. | |||
| •Reginal scale geophysics (magnetics, VTEM, ZTEM) was undertaken during | |||
| the GMX period. | |||
| Geology | • Deposit type, geological setting and style of mineralisation. | •Liamu Project: The main target style at Liamu is porphyry Cu-Au mineralisation, | |
| although GMX did explore for Intermediate Sulphidation style vein | |||
| mineralisation. | |||
| •Ubei Project: The main target style at Ubei is Intermediate Sulphidation style | |||
| vein mineralisation and porphyry Cu-Au. |
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| Criteria | JORC Code explanation | Commentary | |
|---|---|---|---|
| •Veri Veri: The main target style at Veri Veri is serpentinite hosted nickel | |||
| sulphides and nickel laterites associated with weathered ultramafic rocks. | |||
| Drill hole | • A summary of all information material to the understanding | •NA | |
| Information | of the exploration results including a tabulation of the | ||
| following information for all Material drill holes: | |||
o easting and northing of the drill hole collar |
|||
o elevation or RL (Reduced Level – elevation above sea |
|||
| level in metres) of the drill hole collar | |||
o dip and azimuth of the hole |
|||
o down hole length and interception depth |
|||
o hole length. |
|||
| • If the exclusion of this information is justified on the basis | |||
| that the information is not Material and this exclusion does | |||
| not detract from the understanding of the report, the | |||
| Competent Person should clearly explain why this is the | |||
| case. | |||
| Data | • In reporting Exploration Results, weighting averaging | •No metal equivalent values have been stated. | |
| aggregation methods |
techniques, maximum and/or minimum grade truncations (eg cutting of high grades) and cut-off grades are usually Material and should be stated. |
•No cut of high grades has been done. •All widths quoted are intercept widths. |
|
| • Where aggregate intercepts incorporate short lengths of high | |||
| grade results and longer lengths of low grade results, the | |||
| procedure used for such aggregation should be stated and | |||
| some typical examples of such aggregations should be | |||
| shown in detail. | |||
| • The assumptions used for any reporting of metal equivalent | |||
| values should be clearly stated. | |||
| Relationship | • These relationships are particularly important in the reporting | •Trench sampling at Dada is considered representative of the stockwork style |
|
| between | mineralisation associated with porphyry Cu-Au mineralisation, and is |
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| Criteria | JORC Code explanation | Commentary | |
|---|---|---|---|
| mineralisation | of Exploration Results. |
perpendicular to the dominant vein orientation. | |
| widths and intercept lengths |
• If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported. |
||
| • If it is not known and only the down hole lengths are | |||
| reported, there should be a clear statement to this effect (eg | |||
| ‘down hole length, true width not known’). | |||
| Diagrams | • Appropriate maps and sections (with scales) and tabulations | •Geological maps showing the location of trenches and exploration results are | |
| of intercepts should be included for any significant discovery | shown in the body of the announcement. | ||
| being reported These should include, but not be limited to a | |||
| plan view of drill hole collar locations and appropriate | |||
| sectional views. | |||
| Balanced | • Where comprehensive reporting of all Exploration Results is | •Reporting is considered balanced. | |
| reporting | not practicable, representative reporting of both low and high | ||
| grades and/or widths should be practiced to avoid | |||
| misleading reporting of Exploration Results. | |||
| Other | • Other exploration data, if meaningful and material, should be | •No QAQC data (field duplicates, standards, blanks) were undertaken on |
|
| substantive | reported including (but not limited to): geological | Footprint trenches. The data is reliant on the ITS internal laboratory checks. | |
| exploration data |
observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances. |
•Logs of soil, rock chip and trenches are generated in field and material data later transferred by a Geologist to the Company’s database. When available and after review, QA/QC compliant assay data is also transferred to the Company’s database by a qualified database Manager. |
|
| •All pulps are collected from the Laboratory after 3 months and stored in a | |||
| locked container with security. | |||
| •Ground EM geophysics has been conducted by Footprint over the Ubei | |||
| prospects of Lion, Tiger, Cheetah, and Puma. | |||
| •Footprint completed 10 diamond holes for 1814m in the Liamu and Ubei project | |||
| areas. These targets have since been downgraded and not of current interest. | |||
| Further work | • The nature and scale of planned further work (eg tests for | •Continued trenching, mapping, soils sampling and electrical testing ahead of | |
| lateral extensions or depth extensions or large-scale step- | potential drilling is planned for the Veri Veri Ni-Au target. |
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| Criteria | JORC Code explanation | Commentary | |
|---|---|---|---|
| out drilling). | |||
| • Diagrams clearly highlighting the areas of possible | |||
| extensions, including the main geological interpretations and | |||
| future drilling areas, provided this information is not | |||
| commercially sensitive. |
85