AI assistant
WA1 RESOURCES LTD — Capital/Financing Update 2023
Sep 25, 2023
66031_rns_2023-09-25_c25ac016-be50-4c3a-823e-1296c3b7c040.pdf
Capital/Financing Update
Open in viewerOpens in your device viewer
==> picture [595 x 91] intentionally omitted <==
26 SEPTEMBER 2023
WEST ARUNTA PROJECT
LUNI ASSAYS CONTINUE TO DELIVER SIGNIFICANT HIGH-GRADE EXPANSION
Highlights
- Assays received from drillholes 400m west of previous results, including:
LURC23-013 from 51m: 16m at 2.0% Nb2O5
LURC23-012 from 52m: 8m at 1.6% Nb2O5
LURC23-011 from 45m: 10m at 1.9% Nb2O5
-
These drillholes confirm further continuity of the shallow, high-grade blanket of mineralisation which remains open and now extends over 2km east-west
-
Assays from 200m step-out drilling in the southeast also extends mineralisation:
LURC23-043 from 50m: 8m at 2.1% Nb2O5
and from 62m: 6m at 2.0% Nb2O5
-
LURC23-042 drilled in the southeast has identified deeper mineralisation interpreted to be in a fault offset position, with 1m at 3.7% Nb2O5 at end of hole
-
First 100m spaced infill drillhole assays received demonstrating short-range continuity of the shallow high-grade zone, including:
LURC23-110 from 40m: 7m at 3.1% Nb2O5
▪ Over 20,000m of drilling has now been completed at Luni with a further 10,000m planned for the remainder of the year
WA1 Resources Ltd (ASX: WA1) ( WA1 or the Company ) is pleased to announce further exploration results from drilling at the 100% owned West Arunta Project in Western Australia.
WA1’s Managing Director, Paul Savich, commented:
“It is remarkable that we are able to continue broad reconnaissance drilling at Luni and consistently return very high-grade, shallow niobium mineralisation. In addition, infill drilling is now beginning to establish internal continuity between the initial broad step-out holes.
“Meanwhile the results from LURC23-042 drilled in the southeast of Luni has provided an exciting new high-grade target zone from ~120m depth which appears to be in a similar offset position to that seen in the south-central area from previously reported holes LURC23-015 and 078. Further drilling will be completed in this area to test the potential for deeper mineralisation.”
==> picture [595 x 66] intentionally omitted <==
==> picture [594 x 93] intentionally omitted <==
==> picture [483 x 299] intentionally omitted <==
Figure 1: Luni plan view with drill collar locations and key new intersections
Geological Discussion - Luni Carbonatite (Sambhar Prospect Area)
Results within this release relate to further reverse circulation ( RC ) drillholes (refer to Table 2) completed at the Luni carbonatite. A total of 140 RC and 18 diamond drillholes have now been drilled at Luni, with 47 holes now reported.
High-grade niobium mineralisation identified 400m west of previously released drillholes
New significant intersections have been reported in this announcement relating to holes drilled 400m west of previously reported assay results.
The assay results highlight an extension of the shallow, high-grade niobium mineralisation into the west of the carbonatite, well beyond the known high-grade northeast trending corridor which has been the subject of significant infill drilling.
The high-grade mineralisation in western drillholes LURC23-011, 012 and 013 is occurring coincident with the upper saprolite-lower saprolite interface, a common characteristic that has been observed more broadly across the weathered horizon at Luni.
Further assay results from drillholes within the western portion of the interpreted carbonatite will be received in the coming weeks. In addition, further infill drilling is being planned in this new western zone to better define the mineralisation.
New target zone in the south-east of Luni
An additional significant niobium intersection was returned from ongoing broad 200m step-out drilling, with LURC23-043 intersecting high-grade mineralisation in the south-east of Luni.
==> picture [595 x 64] intentionally omitted <==
==> picture [594 x 93] intentionally omitted <==
Furthermore LURC23-042, a reconnaissance drillhole located 200m south of 043, ended in highgrade mineralisation with the final metre returning 1m at 3.7% Nb2O5. This drillhole was terminated at 120m due to drilling conditions and was unable to adequately test the vertical extent of this mineralisation.
==> picture [483 x 353] intentionally omitted <==
Figure 2: Luni plan view with drill collar locations and passive seismic inset Refer to ASX Announcement dated 1 March 2023 for full passive seismic details
The mineralised interval occurs deeper than that generally intersected elsewhere at Luni. The passive seismic model potentially provides an explanation through the occurrence of two vertically offset horizons (see Figure 2).
The mechanism for the offset is interpreted to be an east-west trending fault and drillhole 042 only just intersects the top of the deeper horizon. Holes LURC23-030, 031 and 041 which are also located over the deeper acoustic impedance boundary did not reach this deeper horizon.
A similar deeper horizon is observed in drillholes LURC23-015 and 078. It is currently interpreted that a similar offset regime may be occurring in the southeast of Luni.
The Company is completing further RC and diamond drilling in the southeastern area to test the potential for enriched mineralisation in this deeper target zone.
==> picture [595 x 64] intentionally omitted <==
==> picture [594 x 93] intentionally omitted <==
Assays from the first infill drillhole demonstrate continuity of the high-grade oxide blanket
Assay results from hole LURC23-110 have been received and includes 7m at 3.1% Nb2O5 from 40m.
This hole was drilled between 2022 discovery hole LURC003 and the first hole drilled in the 2023 field season, LURC23-022. This early infill hole was completed to better understand continuity of the enriched blanket of mineralisation between the broad 200m step-out holes.
Indications from this first infill hole is that continuity is strong between discovery hole LURC003 (7m at 3.5% Nb2O5 from 40m) and LURC23-022 (12m at 3.2% Nb2O5 from 47m).
For full details of key intersections refer to the annotated images and Tables 1 and 2. The orientation of enriched, oxide mineralisation (true width) is interpreted to be sub-horizontal and coincident with the flat lying transition between intensely and moderately weathered carbonatite.
==> picture [595 x 64] intentionally omitted <==
==> picture [595 x 93] intentionally omitted <==
==> picture [626 x 416] intentionally omitted <==
Figure 3: Luni carbonatite plan view of completed and planned drilling with significant intersections to date For previously released results refer to ASX announcements dated 6 February, 1 May, 5 June, 29 June, 21 August and 28 August 2023 F
==> picture [594 x 93] intentionally omitted <==
Niobium Overview
==> picture [276 x 235] intentionally omitted <==
Niobium is a critical metal with unique properties that make it essential as the world transitions to a low carbon economy.
The primary niobium product is Ferroniobium (FeNb, ~65% Nb) which accounts for approximately 90% of a 100,000tpa[1] market. Ferroniobium is utilised as a micro alloy in the steel industry to improve the mechanical properties of steel.
Niobium pentoxide (Nb2O5) represents a key growth market, with significant recent developments in lithium-ion battery technology to utilise niobium to substantially reduce charge times down to six minutes while enhancing battery life by up to 20,000 cycles, an increase of up to 10x compared to existing technologies[2] .
Figure 4: Key Niobium Resources Globally Source: See table 3 for full details
Whilst global supply is concentrated in Brazil (90% of global production), global demand for niobium products is widespread. There are many end users and a growing number of applications.
==> picture [483 x 241] intentionally omitted <==
Figure 5: Major suppliers and consumers of global niobium
Source: Adapted from CBMM data and Australian critical mineral list (2023)
Note 1. Mordor Intelligence: Global Niobium Market Report 2023 2 https://www.batterydesign.net/niobium-in-batteries/ accessed on 18 August 2023
==> picture [594 x 93] intentionally omitted <==
ENDS
This Announcement has been authorised for market release by the Board of WA1 Resources Ltd.
For further information, please contact:
Media
Investors Media Paul Savich Michael Vaughan Managing Director Fivemark Partners T: +61 8 6478 7866 T: +61 422 602 720 E: [email protected] E: [email protected]
Or visit our website at www.wa1.com.au
Competent Person Statements
The information in this announcement that relates to Exploration Results is based on information compiled by Ms. Stephanie Wray who is a Member of the Australian Institute of Geoscientists. Ms. Wray is a full-time employee of WA1 Resources Ltd and has sufficient experience which is relevant to the style of mineralisation under consideration to qualify as a Competent Person as defined in the 2012 Edition of the “Australian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”. Ms. Wray consents to the inclusion in the announcement of the matters based on her information in the form and context in which it appears.
Disclaimer: No representation or warranty, express or implied, is made by the Company that the material contained in this announcement will be achieved or proved correct. Except for statutory liability which cannot be excluded, each of the Company, its directors, officers, employees, advisors and agents expressly disclaims any responsibility for the accuracy, fairness, sufficiency or completeness of the material contained in this presentation and excludes all liability whatsoever (including in negligence) for any loss or damage which may be suffered by any person as a consequence of any information in this presentation or any effort or omission therefrom. The Company will not update or keep current the information contained in this presentation or to correct any inaccuracy or omission which may become apparent, or to furnish any person with any further information. Any opinions expressed in the presentation are subject to change without notice.
==> picture [595 x 64] intentionally omitted <==
==> picture [594 x 93] intentionally omitted <==
About WA1
WA1 Resources Ltd is based in Perth, Western Australia and was admitted to the official list of the Australian Securities Exchange (ASX) in February 2022. WA1’s shares are traded under the code WA1.
WA1’s objective is to discover Tier 1 deposits in Western Australia’s underexplored regions and create value for all stakeholders. We believe we can have a positive impact on the remote communities within the lands on which we operate. We will execute our exploration using a proven leadership team which has a successful track record of exploring in WA’s most remote regions.
Forward-Looking Statements
This ASX Release may contain certain “forward-looking statements” which may be based on forward-looking information that are subject to a number of known and unknown risks, uncertainties, and other factors that may cause actual results to differ materially from those presented here. Where the Company expresses or implies an
==> picture [376 x 301] intentionally omitted <==
expectation or belief as to future events or results, such expectation or belief is expressed in good faith and believed to have a reasonable basis. For a more detailed discussion of such risks and other factors, see the Company’s Prospectus and Annual Reports, as well as the Company’s other ASX Releases. Readers should not place undue reliance on forward-looking information. The Company does not undertake any obligation to release publicly any revisions to any forwardlooking statement to reflect events or circumstances after the date of this ASX Release, or to reflect the occurrence of unanticipated events, except as may be required under applicable securities laws.
==> picture [595 x 64] intentionally omitted <==
==> picture [595 x 93] intentionally omitted <==
Table 1: RC Drilling Results - Significant Intercepts
| Hole ID | From (m) |
To (m) |
Interval (m) |
Nb2O5 (%) |
TREO (%) |
Nd+Pr (ppm) |
NdPr:TREO (%) |
Sc2O3 (ppm) |
Ta2O5 (ppm) |
SrO (%) |
Th (ppm) |
U (ppm) |
P2O5 (%) |
TiO2 (%) |
|
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| LURC23011 | incl | 45 | 79 | 34 | 0.84 | 0.65 | 1,458 | 23% | 14 | 11 | 0.7 | 13 | 19 | 9.9 | 0.4 |
| 45 | 55 | 10 | 1.90 | 1.71 | 3,833 | 22% | 39 | 19 | 1.9 | 33 | 50 | 18.9 | 0.9 | ||
| LURC23012 | incl | 51 | 79 | 28 | 0.68 | 0.25 | 580 | 23% | 33 | 27 | 0.4 | 26 | 29 | 3.6 | 0.6 |
| 52 | 60 | 8 | 1.56 | 0.57 | 1,328 | 23% | 90 | 36 | 1.0 | 53 | 63 | 6.1 | 0.7 | ||
| LURC23013 | incl | 37 | 76 | 39 | 1.15 | 0.67 | 1,476 | 22% | 22 | 52 | 0.8 | 61 | 88 | 13.6 | 1.1 |
| 51 | 67 | 16 | 1.98 | 0.94 | 2,080 | 22% | 28 | 31 | 1.2 | 72 | 153 | 18.4 | 0.6 | ||
| LURC23042 | 119 | 120 | 1 | 3.68 | 1.35 | 2,855 | 21% | 88 | 0 | 2.0 | 50 | 63 | 23.8 | 0.2 | |
| LURC23043 | incl and and |
40 | 96 | 56 | 0.99 | 0.74 | 1,463 | 20% | 24 | 9 | 0.8 | 28 | 12 | 12.8 | 0.2 |
| 50 | 58 | 8 | 2.12 | 2.57 | 4,753 | 18% | 45 | 10 | 1.5 | 78 | 22 | 18.3 | 0.4 | ||
| 62 | 68 | 6 | 1.98 | 0.97 | 2,156 | 22% | 39 | 7 | 1.2 | 34 | 21 | 24.8 | 0.2 | ||
| 76 | 80 | 4 | 1.31 | 0.77 | 1,626 | 21% | 29 | 13 | 1.0 | 29 | 16 | 24.3 | 0.1 | ||
| LURC23044 | 40 | 49 | 9 | 0.32 | 0.66 | 1,500 | 23% | 26 | 5 | 1.1 | 20 | 19 | 17.7 | 0.2 | |
| LURC23046 | incl and |
38 | 59 | 21 | 0.48 | 0.17 | 383 | 22% | 57 | 38 | 0.2 | 23 | 31 | 4.2 | 0.8 |
| 55 | 57 | 2 | 1.66 | 0.23 | 510 | 22% | 89 | 128 | 0.3 | 47 | 107 | 7.8 | 0.3 | ||
| 97 | 105 | 8 | 0.41 | 0.06 | 139 | 22% | 32 | 19 | 0.2 | 7 | 14 | 0.9 | 1.1 | ||
| LURC23110 | incl and |
38 | 97 | 59 | 0.69 | 0.30 | 670 | 22% | 13 | 35 | 0.2 | 39 | 21 | 4.2 | 0.3 |
| 40 | 47 | 7 | 3.08 | 1.22 | 2,671 | 22% | 57 | 83 | 1.0 | 124 | 102 | 15.2 | 1.3 | ||
| 94 | 95 | 1 | 1.80 | 0.37 | 787 | 21% | 15 | 74 | 0.2 | 42 | 39 | 3.6 | 0.4 |
Note: 1: Results not displayed above are considered to contain no significant anomalism. Note 2: 'TREO’ is an abbreviation of Total Rare Earth Oxides, representing a combined group of 16 elements (La, Ce, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu, Y, Sc).
==> picture [595 x 64] intentionally omitted <==
==> picture [594 x 93] intentionally omitted <==
Table 2: RC collar locations and intervals for drillhole results within this release
| Hole ID | Easting | Northing | RL | Dip | Azimuth | Depth |
|---|---|---|---|---|---|---|
| (m) | (Degrees) | (Degrees) | (m) | |||
| LURC23011 | 436002 | 7540398 | 385 | -60 | 180 | 150 |
| LURC23012 | 436002 | 7540598 | 385 | -60 | 180 | 120 |
| LURC23013 | 436002 | 7540798 | 385 | -60 | 180 | 150 |
| LURC23014 | 436002 | 7540998 | 385 | -60 | 180 | 96 |
| LURC23041 | 437596 | 7540013 | 357 | -60 | 180 | 95 |
| LURC23042 | 437597 | 7540192 | 401 | -60 | 180 | 120 |
| LURC23043 | 437591 | 7540407 | 357 | -60 | 180 | 96 |
| LURC23044 | 437590 | 7540603 | 358 | -60 | 180 | 138 |
| LURC23046 | 437608 | 7540996 | 359 | -60 | 180 | 108 |
| LURC23047 | 437604 | 7541203 | 412 | -60 | 180 | 120 |
| LURC23104 | 438000 | 7541174 | 382 | -60 | 180 | 120 |
| LURC23110 | 436801 | 7540496 | 385 | -60 | 180 | 120 |
==> picture [595 x 64] intentionally omitted <==
==> picture [594 x 93] intentionally omitted <==
Table 3: Key niobium resources globally
| Deposit Size | Nb2O5 | Contained Nb2O5 | |
|---|---|---|---|
| CBMM (Araxa) | (Mt) | (%) | (kt) |
| Measured Indicated Inferred |
Unknown Unknown Unknown* |
Unknown Unknown Unknown* |
Unknown Unknown Unknown* |
| Total | 462 | 2.48% | 11,458 |
| Source: US Geological Survey published 2017 available at https://pubs.usgs.gov/pp/1802/m/pp1802m.pdf *Measured, Indicated and Inferred resource notpublicly available to due CBMMprivate ownership |
|||
| Lynas Rare Earths (Mt Weld) | (Mt) | (%) | (kt) |
| Measured Indicated Inferred |
0 2 36 |
0 1.40% 1.06% |
0 21 384 |
| Total | 38 | 1.07% | 405 |
| Source: Lynas Corporation Ltd ASX announcement 5/10/2015, https://wcsecure.weblink.com.au/pdf/LYC/01668856.pdf Resource as at 31 August 2015(JORC 2012 Compliant) |
|||
| Magris Resources (Niobec) | (Mt) | (%) | (kt) |
| Measured Indicated Inferred |
286 344 68 |
0.44% 0.40% 0.37% |
1,252 1,379 252 |
| Total | 698 | 0.41% | 2,883 |
| Source: IAMGOLD NI 43-101 Report available at https://www.miningdataonline.com/reports/Niobec_12102013_TR.pdf Resource as at 31 December 2012(NI 43-101 Compliant) |
|||
| CMOC (Catalao II) | (Mt) | (%) | (kt) |
| Oxide Measured Indicated Inferred |
0.3 0.1 1.3 |
0.86% 0.74% 0.83% |
2 1 11 |
| Total | 1.7 | 0.83% | 14 |
| Fresh Rock (Open Pit) Measured Indicated Inferred |
0 27 13 |
0.00% 0.95% 1.06% |
0 258 138 |
| Total | 40 | 0.99% | 396 |
| Fresh Rock (Underground) Measured Indicated Inferred |
0.0 0.2 6.3 |
0.00% 0.89% 1.24% |
0 2 78 |
| Total | 6.5 | 1.23% | 80 |
| Total (All) | 48.4 | 1.01% | 490 |
| Source: China Molybdenum Co. Ltd: Major Transaction Acquisition of Anglo American PLC's Niobium and Phosphate Businesses available at https://www1.hkexnews.hk/listedco/listconews/sehk/2016/0908/ltn20160908840.pdf Resource as at 30 June 2016(JORC 2012 Compliant) |
==> picture [595 x 64] intentionally omitted <==
==> picture [594 x 93] intentionally omitted <==
JORC Code, 2012 Edition – Table 1
Section 1 Sampling Techniques and Data
| CRITERIA | COMMENTARY |
|---|---|
| Sampling techniques |
▪ All geological information referred to in this ASX Announcement was derived from a Reverse Circulation (RC) drill program. ▪ From every metre drilled a 2-3kg sample (split) was sampled into a calico bag via the rig mounted cone splitter. Samples submitted to the laboratory were determined by the rig geologist. ▪ Every metre interval was analysed with an Evident Vanta handheld XRF (pXRF) to aid in identifying zones of interest. ▪ All samples were submitted to ALS Laboratories in Perth for elemental analyses via Lithium Borate Fusion (ME-MS81D) with overlimit determination via ALS method ME-XRF30. |
| Drilling techniques | ▪ RC drillingwas completed at all holes with a diameter of 146mm. |
| Drill sample recovery |
▪ Sample recoveries are visually estimated for each metre with poor or wet samples recorded in the sample table. ▪ The sample cyclone was routinely cleaned at the end of each 6m rod and when deemed necessary. ▪ No relationship has been determined between sample recovery and the mineralisation returned. ▪ Samples were dry and recovery was high through the significant intervals reported. |
| Logging | ▪ The RC rock chips were logged for geology, alteration, and mineralisation by the Company’s geological personnel. Drill logs were recorded digitally and have been verified. ▪ Logging of drill chips is qualitative and based on the presentation of representative chips retained for all 1m sample intervals in the chip trays. ▪ The metre intervals were analysed on the drill pad by pXRF, magnetic susceptibility and scintillometer to assist with logging and the identification of mineralisation. |
| Sub-sampling techniques and sample preparation |
▪ RC samples were collected from the drill rig splitter into calico bags. ▪ In all holes the 1m samples within the tertiary cover were composited into 4m intervals from spoil piles using a scoop by the site geologist. ▪ Single metre samples were collected and assayed from approx. 16m or as determined bythe sitegeologist. |
| Quality of assay data and laboratory tests |
▪ All samples were submitted to ALS Laboratories in Perth for select element analyses via Lithium Borate Fusion (ME-MS81D) with overlimit determination via ALS method ME-XRF30. ▪ Standard laboratory QAQC was undertaken and monitored by the laboratory and then by WA1 geologists upon receipt of assay results. ▪ Certified Reference Materials (CRMs) were inserted at a rate of one every 20 samples. The CRM results have passed an internal QAQC review. ▪ The laboratory standards have been reviewed by the company and havepassed internalQAQC checks. |
==> picture [595 x 64] intentionally omitted <==
==> picture [594 x 93] intentionally omitted <==
| CRITERIA | COMMENTARY |
|---|---|
| Verification of sampling and assaying |
▪ Analytical QC is monitored by the laboratory using standards and repeat assays. ▪ Mineralised intersections have been verified against the downhole geology. ▪ Logging and sampling data was recorded digitally in the field. ▪ Significant intersections are inspected by senior Company geologists. ▪ Select samples have been sent to Intertek for umpire laboratory analysis with results showing a strong correlation to the primary laboratory. ▪ No twinned holes have received assayresults at this time. |
| Location of data points |
▪ Drill hole collars were surveyed and recorded using a handheld GPS. Drill collars will be surveyed with DGPS at appropriate stages of the program. ▪ All co-ordinates are provided in the MGA94 UTM Zone 52 co- ordinate system with an estimated accuracy of +/-5m. ▪ Azimuth and dip of the drill holes was recorded after completion of the hole using a gyro. A reading was taken every 30m with an accuracyof +/-1 degree azimuth and +/-0.3 degree dip. |
| Data spacing and distribution |
▪ See drill hole table for hole position and details. ▪ Data spacing at this stage is not considered suitable for Mineral Resource Estimation. |
| Orientation of data in relation to geological structure |
▪ The orientation of the oxide-enriched mineralisation is interpreted to be sub-horizontal. The orientation of primary mineralisation is poorly constrained due to the limited number of drill holes that have penetrated to depth. ▪ See drill hole table for hole details and the text of this announcement for discussion regarding the orientation of holes. ▪ See drill hole table for hole details and the text of this announcement for discussion regarding the orientation of holes. ▪ Drill holes were designed based on interpretation from modelled geophysical data and the discovery drillholes. ▪ Mineralisation is currently interpreted as a sub horizontal oxide unit. Modelling of the mineralisation is underway to constraint the true and apparent width of the enriched zone. |
| Sample security | ▪ Sample security is not considered a significant risk with WA1 staff present during collection. ▪ All geochemical samples were collected, bagged and sealed by WA1 staff, and delivered to ALS Laboratories in Perth. ▪ 1m splits were stored in a secure location. |
| Audits or reviews | ▪ The program and data is reviewed on an ongoing basis by senior WA1personnel. |
==> picture [595 x 64] intentionally omitted <==
==> picture [594 x 93] intentionally omitted <==
Section 2 Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this section.)
| Criteria | Commentary |
|---|---|
| Mineral tenement and land tenure status |
▪ All work completed and reported in this ASX Announcement was completed on E80/5173 which is 100% owned by WA1 Resources Ltd. ▪ The Company also currently holds two further granted Exploration Licences and nine Exploration Licence Applications within the area of the West Arunta Project. |
| Exploration done by other parties |
▪ The West Arunta Project has had limited historic work completed within the Project area, with the broader area having exploration focused on gold, base metals, diamonds and potash. ▪ Significant previous explorers of the Project area include Beadell Resources and Meteoric Resources. Only one drill hole (RDD01) had been completed within the tenement area by Meteoric in 2009, and more recently a second hole proximate to the Project by Encounter Resources Ltd in 2020. ▪ Most of the historic work was focused on the Urmia and Sambhar Prospects with historic exploration (other than RDD01) being limited to geophysical surveys and surface sampling. ▪ Historical exploration reports are referenced within the WA1 Resources Ltd Prospectus dated 29 November 2021 which was released byASX on 4 February2022. |
| Geology | ▪ The West Arunta Project is located within the West Arunta Orogen, representing the western-most part of the Arunta Orogen which straddles the Western Australia-Northern Territory border. ▪ Outcrop in the area is generally poor, with bedrock largely covered by Tertiary sand dunes and spinifex country of the Gibson Desert. As a result, geological studies in the area have been limited, and a broader understanding of the geological setting is interpreted from early mapping as presented on the MacDonald (Wells, 1968) and Webb (Blake, 1977 (First Edition) and Spaggiari et al., 2016 (Second Edition)) 1:250k scale geological map sheets. ▪ The West Arunta Orogen is considered to be the portion of the Arunta Orogen commencing at, and west of, the Western Australia- Northern Territory border. It is characterised by the dominant west- north-west trending Central Australian Suture, which defines the boundary between the Aileron Province to the north and the Warumpi Province to the south. ▪ The broader Arunta Orogen itself includes both basement and overlying basin sequences, with a complex stratigraphic, structural and metamorphic history extending from the Paleoproterozoic to the Paleozoic(Jolyet al.,2013). |
| Drill hole Information |
▪ Refer to Table 2 for drill hole details. |
| Data aggregation methods |
▪ Selected significant intercepts are weight averaged by length and calculated using a 0.2% lower cut off, with a maximum of 3m of consecutive internal dilution. ▪ No metal equivalents have been reported. |
| Relationship between |
▪ The true thickness of the mineralisation intersected in the drill holes has not been estimated due to limited data. |
==> picture [595 x 64] intentionally omitted <==
==> picture [594 x 93] intentionally omitted <==
| Criteria | Commentary |
|---|---|
| mineralisation widths and intercept lengths |
|
| Diagrams | ▪ Refer to figuresprovided within this ASX Announcement. |
| Balanced reporting |
▪ All meaningful information has been included in the body of the text. |
| Other substantive exploration data |
▪ All data and information considered material has been included in the body of this ASX Announcement. ▪ A preliminary mineralogical assessment has been undertaken on a select number of samples. Refer to bodyof text for further details. |
| Further work | ▪ Further interpretation of drill data and assay results will be completed over the coming months, including detailed petrographic and mineralogical analysis. ▪ Additional exploration drillingand analysis is ongoing. |
==> picture [595 x 64] intentionally omitted <==