AI assistant
LIGHTNING MINERALS LTD — Capital/Financing Update 2025
Jan 16, 2025
65212_rns_2025-01-16_7ee436f3-d1fb-4e4f-949c-ed8bc75609b3.pdf
Capital/Financing Update
Open in viewerOpens in your device viewer
==> picture [596 x 53] intentionally omitted <==
Confirmation of Spodumene and Additional Strong Lithium Soil Sampling Results in Brazil Supports Drill Program for Q1 2025
ASX Announcement 1 7 Ja n u a r y 2 0 2 5
Lightning Minerals (L1M or the Company) is pleased to announce the confirmation of spodumene minerals discovered within pegmatites at the Esperança Project in Brazil’s Lithium Valley region of Minas Gerais. Additionally, the highest tenor lithium assays to date from its soil sampling programs at the Caraíbas and Esperança projects, also located in the Lithium Valley have been received. Peak soil assays of up to 429ppm Lithium have been returned at Caraíbas and 320ppm Lithium at Canabrava.
The confirmation of spodumene as the lithium bearing mineral via Raman spectrographic analysis further demonstrates the significance of the recent discovery at Esperança (ASX Announcement 18[th] November 2024) and the upcoming 2,000m drill program. Drill contractor engagement is now being finalised.
HIGHLIGHTS
-
Spodumene Minerals confirmed via Raman Spectroscopy at Esperança project
-
Highest tenor lithium results to date returned from Caraíbas and Canabrava with results up to 429ppm Lithium and 320ppm Lithium respectively
-
Procurement of drilling contractors and logistics progressing well for inaugural drilling campaign of up to 2,000m diamond drilling at Esperança due to begin during Q1 2025
Lightning Minerals Managing Director Alex Biggs said , “Further excellent results across our projects in Brazil provide even greater confidence in the potential prospectivity of both project areas and the region. The past 6-months have been significant for the Company in providing strong drill targets and allowing us to both develop an exploration thesis and drill target priorities. As we move towards our first drill campaign in Brazil el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806 at Esperança we look ahead to another busy and productive year that has the potential to deliver significant results and a step change for the Company. I have always believed in being aggressive in our exploration strategy and with the results and targets we have generated so far in Brazil believe in the potential this region holds for us.”.
Spodumene Confirmation through Raman Spectroscopy at Esperança Project
During geological mapping fieldwork conducted in mid-November 2024 field geologists encountered a previously unknown historical artisanal mine within the Esperança project area. Pegmatitic lithologies were present in the walls of the excavations which displayed elongate crystals up to 50cm of suspected spodumene. Selective mineral specimen grab samples were collected and analysed via a SciAps Z-903 handheld LIBS (Laser-Induced Breakdown Spectroscopy) device which returned a qualitative lithium endowment of up to 4.04% Li2O. While the lithium content analyses using the LIBS device was considered positive, the mineral species containing the lithium had not yet been confirmed.
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806
==> picture [596 x 53] intentionally omitted <==
Selectively sampled mineral specimens were sent to Perth for analyses using a Bruker BRAVO Raman spectrometer. The results confirm the presence of spodumene as the lithium bearing mineral with 5 samples returning positive spectral responses consistent with the mineral data library for spodumene (Table 1 and Figure 2).
Table 1: Raman analyses results for spodumene within selective sampling of mineral specimens at Esperança Project
| Sample ID | Raman SpectroscopyIdentified Minerals |
|---|---|
| LMBR0005 | Kaolinite |
| LMBR0006 | Albite + Kaolinite |
| LMBR0007 | Kaolinite |
| LMBR0008 | Kaolinite |
| LMBR0009 | Spodumene + Kaolinite |
| LMBR0010 | Albite + Kaolinite |
| LMBR0011 | Albite + Kaolinite |
| LMBR0012 | Muscovite + Albite |
| LMBR0013 | Spodumene + Kaolinite |
| LMBR0014 | Spodumene + Kaolinite |
| LMBR0015 | Spodumene + Kaolinite |
| LMBR0016 | Spodumene + Kaolinite + Wodginite |
The Raman test work has also confirmed the high degree of weathering of the mineral specimens, with all but one sample returning spectral response consistent with kaolin for samples that retain a crystal habit. This result suggests the weathering profile of the sampled horizon is high, where precursor minerals have been substantially weathered.
Mineral specimen LMBR0016 contained an accessory opaque mineral which was not readily identified by field geologists. The Raman test work has returned a strong spectral response consistent with Wodginite, which is a Manganese-Tin-Tantalum oxide.
To avoid the highly weathered supergene profile present at the Esperança spodumene occurrence the upcoming proposed drill program will be targeting depths greater than 30m below surface which is the interpreted base of complete oxidation in the local area. Whole rock laboratory sample analysis supports the el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806 degree of weathering of the pegmatite samples with lithium content peaking at 0.38% Li2O for sample VLM207. The full suite of analytical data and spatial locations for all whole rock samples is available within (Appendix 1, Table 2, and Figure 4).
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806
==> picture [596 x 53] intentionally omitted <==
Figure 1: (Left) Photograph of highly weathered spodumene sample LMBR0009, ( Right ) Photograph of highly weathered spodumene sample LMBR0016 showing accessory wodginite in left crystal face (dark mineral)
==> picture [196 x 210] intentionally omitted <==
==> picture [217 x 209] intentionally omitted <==
Figure 2: (A) Example of Spodumene spectral response of sample LMBR0009, ( B ) Sample LMBR0009 also presents strong Kaolin spectral response which supports weathered interpretation, (C) Example of Spodumene response of sample LMBR0016, (D) Accessory Wodginite mineral in sample LMBR0016
==> picture [537 x 389] intentionally omitted <==
----- Start of picture text -----
el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
----- End of picture text -----
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806
==> picture [596 x 53] intentionally omitted <==
Phase 1 Soil Sampling Campaign Completion – All Projects
Final analytical results for the remaining 1,061 Soil Samples completed across the Caraíbas, Canabrava and Esperança projects are now available. Results are positive with the highest lithium tenor anomalism returned to date occurring at the Caraíbas and Canabrava project areas of 429ppm Lithium and 320ppm Lithium respectively.
Esperança Soil Results
The soil sampling program at Esperança was primarily designed to test for lithium at a tenement scale with collection of 465 samples planned along 400m spaced N-S orientated sample lines. The discovery of a spodumene bearing pegmatites in the northwest corner of the tenement during the beginning of the sampling program resulted in the addition of further 191 samples at a closer line spacing at 100m.
The results for the program are shown in Figure 3. The majority of anomalous results occur within the infilled area in the northwest, with results above 60ppm lithium clustered around the spodumene occurrence, and the target for the Company’s inaugural drill program. An isolated peak result of 144ppm lithium is recorded in sample SOLM1315 which will receive follow up investigation.
Figure 3: Soil sampling (lithium) results at the Esperança project (labelled samples over 100ppm Lithium)
==> picture [512 x 353] intentionally omitted <==
----- Start of picture text -----
el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
----- End of picture text -----
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806
==> picture [596 x 53] intentionally omitted <==
Figure 4: Soil sampling and rock chip sampling locations (lithium) at the Esperança project
==> picture [507 x 350] intentionally omitted <==
Drill targeting will continue to focus on the spodumene occurrence at Esperança with the thesis that the spodumene bearing pegmatite dips toward to the southeast toward the centre of the tenement.
Caraíbas Soil Results
Soil results for the remaining 213 samples taken at the Caraíbas project show high tenor soil responses for lithium. Sampling proximal to an artisanal mine with known lithium mineral occurrences of lepidolite (ASX Announcement 22 April 2024) has returned elevations up to 429ppm Lithium, with several adjacent samples el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806 returning values over 200ppm Lithium which is considered a high response for residual soils of Salinas Formation in the region (Figure 5).
The results are currently being investigated with follow up site visits underway to ascertain if outcropping geology at the sites can explain the magnitude of the lithium response. The results of field investigations will feed into the ongoing drill targeting and prioritisation exercise with a view to potentially developing new high priority targets post completion of the Esperança drilling campaign. This will be targeted at the identified lithium in soil anomaly extending approximately 2km with peak results up to 239ppm Lithium (ASX Announcement 02 December 2024).
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806
==> picture [596 x 53] intentionally omitted <==
Figure 5: Soil sampling (lithium) results at the Caraíbas project. Previously reported soil results within western most tenement 831424/2013 are shaded
==> picture [508 x 352] intentionally omitted <==
Canabrava Soil Results
Soil results for 59 infill samples, and 78 new primary samples are now available for the Canabrava project. The infill soil sampling program was designed to follow up previous results where samples on 400m spaced sample lines returned results up to 113ppm Lithium (ASX Announcement 03 October 2024). The infill samples have been collected on a reduced line spacing of 100m and show consistent lithium anomalism el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806 >80ppm which coincides with mapped pegmatites over a 700m strike length (Figure 6). The ability to sample further east into the tenement is truncated by the transition from residual sediments of the Salinas Formation into tertiary depositional sediments which are considered a poor proxy for targeting lithium.
A small 78 sample program was also completed in the south-eastern areas of the Canabrava project in residual Salinas Formation sediments. Results are shown in Figure 7. The two easternmost sample lines have consistent lithium values above 200ppm with a peak result of 320ppm. Infill sampling at this location is being considered as part of the drill targeting and prioritisation exercise.
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806
==> picture [596 x 53] intentionally omitted <==
Figure 6: Infill Soil sampling (lithium) results at the Canabrava project
==> picture [465 x 321] intentionally omitted <==
Figure 7: Soil sampling (lithium) results and updated geological mapping at the Canabrava project
==> picture [470 x 326] intentionally omitted <==
----- Start of picture text -----
el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
----- End of picture text -----
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806
==> picture [596 x 53] intentionally omitted <==
Ongoing Works in Brazil
Drill contractor engagement is now underway for the Company’s inaugural 2,000m drill campaign at Esperança due to begin in Q1 2025. Plans are also underway for drilling at Caraíbas which will be targeted at the identified lithium in soil anomaly extending approximately 2km with peak results up to 239ppm Lithium (ASX Announcement 02 December 2024).
Results for the Phase 1 soil sampling campaign have now been returned in full. Further target generation is now underway. Further infill soil programs may be considered where results require further definition prior to moving to drill testing. Prioritisation of the current suite of targets is now being undertaken to ensure the most robust targets and tested via drilling in the first pass.
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806
==> picture [596 x 53] intentionally omitted <==
Figure 8: Lightning Minerals’ Brazilian tenements in regional context of the Lithium Valley region of Minas Gerais
==> picture [451 x 660] intentionally omitted <==
----- Start of picture text -----
el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
----- End of picture text -----
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806
==> picture [596 x 53] intentionally omitted <==
Figure 9: Local project location of Lightning Minerals’ Brazilian lithium projects
==> picture [451 x 466] intentionally omitted <==
Approved for release by the Board of Directors
-END-
More information at www.lightningminerals.com.au
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806
==> picture [596 x 53] intentionally omitted <==
ABOUT LIGHTNING MINERALS
Lightning Minerals is a mineral exploration company, listed on the Australian Securities Exchange (ASX:L1M) and focused on the exploration of critical minerals and lithium at its tenements across Western Australia. The acquisition of the Caraíbas, Canabrava and Esperança lithium projects in Minas Gerais, Brazil are potentially transformational to the Company’s success in the lithium sector. The Company also owns the Dundas project in the prolific Dundas region of Western Australia, the Dalmas and Hiver lithium projects in Quebec, Canada, another significant and evolving lithium region globally . The Company also holds other projects in Western Australia which include Mt Bartle and Mailman Hill which are prospective for base metals and critic al minerals.
FORWARD LOOKING STATEMENTS
Information included in this release constitutes forward-looking statements. Often, but not always, forward looking statements can generally be identified by the use of forward-looking words such as “may”, “will”, “expect”, “intend”, “plan”, “estimate”, “anticipate”, “continue”, and “guidance”, or other similar words and may include, without limitation, statements regarding plans, strategies and objectives of management, anticipated production or construction commencement dates and expected costs or production outputs.
Forward looking statements inherently involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance and achievements to differ materially from any future results, performance or achievements. Relevant factors may include, but are not limited to, changes in commodity prices, foreign exchange fluctuations and general economic conditions, increased costs and demand for production inputs, the speculative nature of exploration and project development, including the risks of obtaining necessary licences and permits and diminishing quantities or grades of reserves, political and social risks, changes to the regulatory framework within which the Company operates or may in the future operate, environmental conditions including extreme weather conditions, recruitment and retention of personnel, industrial relations issues and litigation. Forward looking statements are based on the Company and its management’s good faith assumptions relating to the financial, market, regulatory and other relevant environments that will exist and affect the Company’s business and operations in the future. The Company does not give any assurance that the assumptions on which forward looking statements are based will prove to be correct, or that the Company’s business or operations will not be affected in any material manner by these or oth er factors not foreseen or foreseeable by the Company or management or beyond the Company’s control.
Although the Company attempts and has attempted to identify factors that would cause actual actions, events or results to dif fer materially from those disclosed in forward looking statements, there may be other factors that could cause actual results, performance, achievements or events not to be as anticipated, estimated or intended, and many events are beyond the reasonable control of the Company. Accordingly, readers are cautioned not to place undue reliance on forward looking statements. Forward looking statements in these materials speak only at the date of issue. Subject to any continuing obligations under applicable law or any relevant stock exchange listing rules, in providing this information the Company does not undertake any obligation to publicly update or revise any of the forward-looking statements or to advise of any change in events, conditions or circumstances on which any such statement is based.
COMPETENT PERSONS STATEMENT
The information contained herein that relates to exploration results is based on information compiled or reviewed by Mr Jarrad Woodland, who is a Competent Person and a member of the Australasian Institute of Mining and Metallurgy. Mr Woodland is a full-time employee of the Company. Mr Woodland has sufficient experience which is relevant to the style of mineralisation and types of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Persons as defined in the 2012 Edition of the ‘Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves’. Mr Woodland consents to the inclusion of his name in the matters based on the information in the form and context in which it appears. Mr Woodland holds options in Lightning Minerals.
REFERENCES TO PREVIOUS ANNOUNCEMENTS
The Company confirms that it is not aware of any new information or data that materially affects the information included in the original market announcements, and that all material assumptions and technical parameters have not materially changed. The Company also confirms that the form and context in which the Competent Person’s findings are presented have not been materially modified from the original market announcement.
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806
==> picture [843 x 53] intentionally omitted <==
Appendix 1: Brazilian Projects – JORC Code 2012 Table 1 Criteria
The Table below summarises the assessment and reporting criteria used for exploration results for the Exploration Projects and reflects the guidelines in Table 1 of The Australasian Code for the Reporting of Exploration Results, Mineral Resources and Ore Reserves (The JORC 2012 Code).
Section 1 - Sampling Techniques and Data
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Sampling techniques | Nature and quality of sampling (eg cut channels, random 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. Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. Aspects of the determination of mineralisation that are Material to the Public Report. 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 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 nodules) may warrant disclosure of detailed information. |
• Data in this document relates to Raman Spectroscopy, geochemical soil and rock chip sampling, field visual identification of minerals, and SciAps Z-903 Handheld LIBS (Laser-Induced Breakdown Spectroscopy) • Mineral samples for VLM207 were collected at the discretion of field geologists targeting spodumene minerals to confirm the mineral species. The LIB’s test work on these samples relates only to a fraction of the mineral and does not represent the whole rock lithium content, which is now available and contained within Appendix 1, Table 2 below. • Raman Spectroscopy is a chemical analysis technique which involves illuminating a substance with a laser and analysing the light that is scattered off the surface of the substance. The scattered light can provide a lot of information about the substance and its structure, and can be used to identify, characterize, and quantify many chemical components. • Soil sampling is a reconnaissance stage exploration technique which may indicates the geochemical parameters of the underlying or nearby bedrock geology. Mineralised lithologies of the target commodity may elevate elemental proportions in the soil and provide vectors toward location the mineralised body. • Soil samples were collected using pick and shovel from depths of approximately 30cm below the surface. • Rockchip samples were collected at the discretion of the field geologist, this method is appropriate given the early stage of exploration at the Caraíbas Project • Approximately 200g of material from the deepest sample horizon is passed through a 2mm sieve, with the -2mm retained for assay. • All samples were submitted to SGS Geosol Laboratórios Ltd’ of Belo Horizonte. • Sampling was carried out using Lightning Minerals procedures and QAQC processes as per current industry standard practice. • Sample site locations are recorded using a Garmin Map 62s handheld device and are reported in projection SIRGAS 2000 / UTM 23S |
| Drilling techniques | Drill type (eg core, reverse circulation, open-hole hammer, 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). |
• No drilling is being reported |
| Drill sample recovery | Method of recording and assessing core and chip sample 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. |
• No drilling is being reported |
| Logging | Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. |
• No drilling is being reported |
==> picture [843 x 57] intentionally omitted <==
==> picture [843 x 53] intentionally omitted <==
| Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. The total length andpercentage of the relevant intersections logged. |
||
|---|---|---|
| Sub-sampling techniques and sample preparation |
If core, whether cut or sawn and whether quarter, half or all core taken. If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. For all sample types, the nature, quality and appropriateness of the sample preparation technique. Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples. 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. Whether sample sizes are appropriate to the grain size of the material being sampled. |
• Soil Samples are collected in the field into small kraft cardboard bags and are 200gm per unit. • Rock chip samples are approximately 1-3kg and are collected into pre numbered calico bags. • Industry standard QAQC practices of field duplicates and the appropriate use of laboratory provided Certified Reference Material for low level lithium are used for all laboratory sample submissions. Field Duplicates are utilised by the company at a rate of 1:50 samples. |
| Quality of assay data and laboratory tests |
The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total. For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc. 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. |
• All samples were submitted to SGS Geosol Laboratórios Ltd’ of Belo Horizonte Minas Gerais Brazil. • Analysis procedures are considered appropriate for Lithium and Multi element analysis. • Samples are prepared and analysed using SGS technique PRS80J and are analysed via optical emission spectroscopy analysis using code ICP90A. Determination by Fusion with Sodium Peroxide - ICP OES. • Soil samples - Elements analysed at ppm limits for include Al, As, B, Ba, Be, Ca, Cd, Co, Cr, Cu, Fe, K, La, Li, Mg, Mn, Mo, Nb, Ni, P, Pb, Sb, Sc, Sn, Sr, Ta, Ti, V, W, Y, Zn • Rock Chip - Elements analysed at ppm limits include Ag, Al,As, B,Ba, Be,Bi, Ca,Cd, Ce,Co, Cr, Cs, Cu, Dy, Er, Eu, Fe, Ga, Gd, Ge, Hf, Ho, In, K, La, Li, Lu, Mg, Mn, Mo, Nb, Nd, Ni, P, Pb, Pr, Rb, Sb, Sc, Sm, Sn, Sr, Ta, Tb, Th, Ti, Tl, Tm, U, V, W, Y, Yb, Zn, Zr • Laboratory CRM material has been utilised at this early stage of exploration works. • A SciAps Z-903 LIBS device was been used for spot sample readings of minerals of interest within sample VLM207. The device is calibrated each day, and before analysis is begun. QAQC standards are used every 10-15 readings as consistency checks. Readings times are approximately 3 to 5 seconds and are standard for the device. The device is calibrated to a lithium profile supplied by SciAps prior to use. • Handheld LIBS is expected to differ from laboratory assay results and can read above theoretical maximum values. They should not be used to replace assays or indicate whole rock grade which are now available in Appendix 1, Table 2 below. |
| Verification of sampling and assaying |
The verification of significant intersections by either independent or alternative company personnel. The use of twinned holes. Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols. Discuss any adjustment to assay data. |
• No verification will be undertaken for these initial samples as they will not be used in any resource estimate. • The samples are to determine the levels of Li and other valuable elements in soil samples. |
| Location of data points | Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation. Specification of the grid system used. |
• Handheld Garmin GPS instruments were used to geo locate each sample location, these instruments are understood to be accurate within a ±5m in the horizontal and vertical planes. • The level of topographic control offered by a handheld GPS is considered sufficient for early exploration activities. • All samples were collected in the SIRGAS 2000/UTM zone 23S |
==> picture [843 x 57] intentionally omitted <==
==> picture [843 x 53] intentionally omitted <==
| Data spacing and distribution Orientation of data in relation to geological structure Sample security Audits or reviews |
Quality and adequacy of topographic control. | |
|---|---|---|
| Data spacing for reporting of Exploration Results. Whether the data spacing, and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied. Whether sample compositing has been applied. |
• The soil and rock chip sample spacing is considered appropriate for the reporting of the exploration results. • No Mineral Resource or Ore Reserve Estimates have been completed. |
|
| Whether the orientation of sampling achieves unbiased 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. |
• The collection of soil and rock chip sampling data was targeted as best possible at this early stage of exploration activities. |
|
| The measures taken to ensure sample security. | • The chain of custody for sampling procedures and sample analysis was managed by the contract geological consultants duringcollection |
|
| The results of any audits or reviews of sampling techniques and data. | • No audits or reviews of sampling techniques have been conducted to date. |
Section 2 - Reporting of Exploration Results
| Criteria | JORC Code explanation | 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 Esperança, Canabrava, and Caraíbas Projects are located approximately 18km south-south east of the town of Salinas, Minas Gerais, Brazil. • The Esperança Project area totals ~11.1km2and comprises one exploration licence 301033/2013 • The Caraíbas Project area totals ~17.3km2 and comprises 5 granted exploration licences 831.514/2018, 832.041/2011, 831.424/2013, 832.763/2014, and 830.313/2014 • The Canabrava Project area totals ~16.7km2and comprises two granted exploration licences 830440/2015 and 830439/2015 • The Tenements are considered ingood standingat the time of this report. |
| Exploration done by other parties |
Acknowledgment and appraisal of exploration by other parties. |
• The Projects are at a very early stage of exploration and little to no recorded work has been completed by prior explorers. • Recent exploration has included a small reconnaissance explorationprogram by project vendor Bengal Mining. |
| Geology | Deposit type, geological setting and style of mineralisation. | • No known mineral deposits occur within project tenure. • Project geology comprises Neoproterozoic age sedimentary rocks of Araçuaí Orogen intruded by pegmatites interpreted to originate from the fractionation of magmatic fluids from the peraluminous S-type post tectonic granitoids of Araçuaí Orogen. • The target commodityis hardrock lithium within lithium-caesium-tantalumpegmatites. |
| 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: oeasting and northing of the drill hole collar oelevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar odown hole length and interception depth, ohole length. |
• No drillhole information is reported. • No material information has been excluded from this report, laboratory analytical results have been adequately communicated and described within the body of this report. |
==> picture [843 x 57] intentionally omitted <==
==> picture [843 x 53] intentionally omitted <==
| 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 aggregation methods |
In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (eg cutting of high grades) and cut-off grades are usually Material and should be stated. 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. |
• No levelling of the raw geochemical data was undertaken. • Plan images have been generated using QGIS software. • No metal equivalent values are reported. |
| Relationship between mineralisation widths and intercept lengths |
These relationships are particularly important in the reporting of Exploration Results. 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’). |
• No drillhole information is reported. • There is insufficient data provided by the mapping and geochemical results contained within this report for a relationship between pegmatite and mineral resources to be reported. |
| Diagrams | Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views. |
• Appropriate reporting of results has been included in the body of this announcement; the plans, or lack thereof suitably represent the nature of the results. |
| Balanced reporting | Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should bepracticed to avoid misleading reporting of Exploration Results. |
• Comprehensive reporting of soil and rock chip geochemical results within the Projects has been included in Appendix 1. |
| Other substantive exploration data |
Other exploration data, if meaningful and material, should be reported including (but not 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 characteristics; potential deleterious or contaminating substances. |
• All meaningful data and relevant information have been included in the body of the report. |
| Further work | The nature and scale of planned further work (e.g., 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. |
• Follow up infill soil sampling is currently being planned and is expected to begin imminently, however at the time of reporting the program has not yet begun. |
==> picture [843 x 57] intentionally omitted <==
==> picture [843 x 53] intentionally omitted <==
Appendix 1 - Table 1: Soil Sampling Assays >150ppm lithium
| Sample ID | Project | Easting (UTM 23S) | Northing (UTM 23S) | Be (ppm) | Li (ppm) | Nb (ppm) | Sn (ppm) | Ta (ppm) | W (ppm) | Y (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|
| SOLM0143 | Caraíbas | 800022 | 8195453 | 2.5 | 173 | 22 | 25 | 23 | 25 | 33 |
| SOLM0150 | Caraíbas | 800050 | 8195109 | 6 | 160 | 20 | 25 | 12 | 25 | 29 |
| SOLM0178 | Caraíbas | 800052 | 8193758 | 12 | 154 | 20 | 25 | 12 | 25 | 21 |
| SOLM0191 | Caraíbas | 800450 | 8195453 | 2.5 | 153 | 41 | 25 | 21 | 25 | 41 |
| SOLM0196 | Caraíbas | 800450 | 8195204 | 10 | 239 | 45 | 25 | 5 | 25 | 37 |
| SOLM0197 | Caraíbas | 800432 | 8195154 | 9 | 157 | 41 | 25 | 12 | 25 | 30 |
| SOLM0207 | Caraíbas | 800451 | 8194703 | 9 | 181 | 49 | 25 | 5 | 25 | 33 |
| SOLM0279 | Caraíbas | 800849 | 8194997 | 7 | 160 | 30 | 25 | 5 | 25 | 42 |
| SOLM0299 | Caraíbas | 801252 | 8194095 | 7 | 155 | 14 | 25 | 5 | 25 | 12 |
| SOLM0612 | Caraíbas | 803247 | 8196163 | 16 | 208 | 12 | 25 | 20 | 25 | 37 |
| SOLM0613 | Caraíbas | 803249 | 8196118 | 25 | 277 | 16 | 25 | 26 | 25 | 59 |
| SOLM0615 | Caraíbas | 803254 | 8196017 | 11 | 183 | 18 | 25 | 16 | 25 | 95 |
| SOLM0616 | Caraíbas | 803253 | 8195966 | 7 | 168 | 5 | 25 | 18 | 25 | 80 |
| SOLM0618 | Caraíbas | 803250 | 8195868 | 10 | 156 | 11 | 25 | 17 | 25 | 94 |
| SOLM0677 | Caraíbas | 803687 | 8195535 | 12 | 226 | 5 | 25 | 23 | 25 | 45 |
| SOLM0680 | Caraíbas | 803657 | 8195379 | 12 | 216 | 5 | 25 | 15 | 25 | 36 |
| SOLM0688 | Caraíbas | 803650 | 8195031 | 9 | 159 | 13 | 25 | 27 | 25 | 41 |
| SOLM0724 | Caraíbas | 804053 | 8195110 | 9 | 186 | 5 | 25 | 5 | 25 | 45 |
| SOLM0725 | Caraíbas | 804052 | 8195165 | 10 | 188 | 5 | 25 | 16 | 25 | 50 |
| SOLM0726 | Caraíbas | 804052 | 8195211 | 11 | 229 | 5 | 25 | 5 | 25 | 39 |
| SOLM0727 | Caraíbas | 804051 | 8195257 | 13 | 396 | 5 | 25 | 5 | 25 | 36 |
| SOLM0728 | Caraíbas | 804053 | 8195308 | 13 | 429 | 5 | 25 | 5 | 25 | 34 |
| SOLM0729 | Caraíbas | 804051 | 8195363 | 11 | 227 | 5 | 25 | 13 | 25 | 42 |
| SOLM0730 | Caraíbas | 804047 | 8195412 | 17 | 254 | 12 | 25 | 22 | 25 | 71 |
| SOLM0731 | Caraíbas | 804054 | 8195464 | 12 | 189 | 10 | 25 | 5 | 25 | 37 |
| SOLM0732 | Caraíbas | 804054 | 8195514 | 8 | 202 | 5 | 25 | 10 | 25 | 36 |
| SOLM0733 | Caraíbas | 804056 | 8195566 | 12 | 192 | 5 | 25 | 5 | 25 | 32 |
| SOLM0734 | Caraíbas | 804054 | 8195612 | 14 | 265 | 12 | 25 | 5 | 25 | 33 |
| SOLM0735 | Caraíbas | 804051 | 8195662 | 14 | 286 | 11 | 25 | 5 | 25 | 41 |
==> picture [843 x 53] intentionally omitted <==
| Sample ID | Caraíbas | Easting (UTM 23S) | Northing (UTM 23S) | Be (ppm) | Li (ppm) | Nb (ppm) | Sn (ppm) | Ta (ppm) | W (ppm) | Y (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|
| SOLM0736 | Caraíbas | 804052 | 8195717 | 15 | 268 | 10 | 25 | 11 | 25 | 35 |
| SOLM0737 | Canabrava | 804051 | 8195759 | 11 | 182 | 5 | 25 | 12 | 25 | 28 |
| SOLM1129 | Canabrava | 800590 | 8188995 | 7 | 160 | 13 | 25 | 5 | 25 | 44 |
| SOLM1134 | Canabrava | 800606 | 8189255 | 10 | 164 | 18 | 25 | 20 | 25 | 20 |
| SOLM1149 | Canabrava | 801382 | 8189090 | 8 | 155 | 11 | 25 | 12 | 25 | 38 |
| SOLM1152 | Canabrava | 801380 | 8188939 | 14 | 175 | 5 | 25 | 23 | 25 | 43 |
| SOLM1175 | Canabrava | 802189 | 8188919 | 12 | 187 | 5 | 25 | 11 | 25 | 64 |
| SOLM1186 | Canabrava | 802568 | 8188911 | 10 | 170 | 19 | 25 | 19 | 25 | 54 |
| SOLM1187 | Canabrava | 802984 | 8188883 | 18 | 228 | 20 | 25 | 17 | 25 | 73 |
| SOLM1188 | Canabrava | 802981 | 8188932 | 11 | 264 | 11 | 25 | 13 | 25 | 39 |
| SOLM1189 | Canabrava | 803000 | 8188969 | 13 | 320 | 26 | 25 | 21 | 25 | 62 |
| SOLM1190 | Canabrava | 802958 | 8189027 | 15 | 238 | 23 | 25 | 17 | 25 | 72 |
| SOLM1191 | Canabrava | 802983 | 8189078 | 11 | 230 | 5 | 25 | 10 | 25 | 71 |
| SOLM1192 | Canabrava | 802982 | 8189126 | 8 | 263 | 11 | 25 | 5 | 25 | 47 |
| SOLM1193 | Canabrava | 802981 | 8189179 | 9 | 231 | 5 | 25 | 13 | 25 | 43 |
| SOLM1202 | Canabrava | 803383 | 8189221 | 8 | 220 | 5 | 25 | 5 | 25 | 30 |
| SOLM1203 | Canabrava | 803384 | 8189171 | 14 | 225 | 5 | 25 | 5 | 25 | 42 |
| SOLM1204 | Canabrava | 803380 | 8189126 | 9 | 213 | 5 | 25 | 5 | 25 | 47 |
| SOLM1205 | Canabrava | 803385 | 8189076 | 10 | 203 | 11 | 25 | 5 | 25 | 40 |
| SOLM1206 | Canabrava | 803386 | 8189029 | 15 | 181 | 5 | 25 | 5 | 25 | 41 |
| SOLM1207 | Canabrava | 803385 | 8188979 | 16 | 223 | 5 | 25 | 5 | 25 | 34 |
| SOLM1208 | Canabrava | 803383 | 8188927 | 9 | 215 | 5 | 25 | 5 | 25 | 38 |
| SOLM1209 | Caraíbas | 803383 | 8188879 | 14 | 168 | 5 | 25 | 5 | 25 | 35 |
| SOLM1214 | Caraíbas | 803748 | 8194777 | 11 | 160 | 5 | 25 | 5 | 25 | 37 |
| SOLM1224 | Caraíbas | 803856 | 8194770 | 14 | 381 | 5 | 25 | 5 | 25 | 27 |
==> picture [843 x 53] intentionally omitted <==
Appendix 1 - Table 2: Rock Chip Sampling Assays
| Sample ID | Project | Easting (UTM 23S) | Northing (UTM 23S) | Be (ppm) | Li (ppm) | Nb (ppm) | Sn (ppm) | Ta (ppm) | W (ppm) | Y (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|
| VLM009 | Caraíbas | 803852 | 8194803 | 13 | 36 | 5 | 11 | 5 | 50 | 5.61 |
| VLM022 | Caraíbas | 803896 | 8194826 | 8 | 44 | 12 | 23 | 5 | 50 | 2.99 |
| VLM029 | Caraíbas | 803255 | 8194579 | 7 | 15 | 5 | 7 | 5 | 50 | 2.41 |
| VLM030 | Caraíbas | 803234 | 8194603 | 8 | 33 | 5 | 2.5 | 5 | 50 | 4.9 |
| VLM032 | Caraíbas | 803185 | 8194636 | 7 | 11 | 5 | 2.5 | 5 | 50 | 11.35 |
| VLM039 | Caraíbas | 803451 | 8195112 | 10 | 50 | 5 | 2.5 | 5 | 50 | 1.27 |
| VLM055 | Caraíbas | 803227 | 8195722 | 31 | 28 | 5 | 2.5 | 5 | 50 | 1.04 |
| VLM072 | Caraíbas | 794984 | 8192062 | 218 | 5 | 84 | 43 | 88 | 50 | 20.79 |
| VLM080 | Caraíbas | 794614 | 8192526 | 227 | 5 | 122 | 15 | 57 | 50 | 2.96 |
| VLM107 | Caraíbas | 795258 | 8193586 | 187 | 28 | 97 | 28 | 40 | 50 | 3.24 |
| VLM122 | Canabrava | 794653 | 8192722 | 161 | 27 | 109 | 47 | 40 | 50 | 1.68 |
| VLM138 | Esperança | 792121 | 8187833 | 51 | 23 | 43 | 11 | 15 | 50 | 7.52 |
| VLM149 | Esperança | 791982 | 8187642 | 12 | 15 | 17 | 7 | 5 | 50 | 2.55 |
| VLM157 | Esperança | 792170 | 8187904 | 29 | 15 | 47 | 2.5 | 14 | 50 | 7.1 |
| VLM163 | Esperança | 791996 | 8187840 | 70 | 13 | 89 | 32 | 55 | 50 | 7.64 |
| VLM165 | Esperança | 791937 | 8187715 | 11 | 49 | 29 | 13 | 5 | 50 | 2.96 |
| VLM176 | Esperança | 792478 | 8187543 | 2.5 | 39 | 10 | 6 | 5 | 50 | 1.83 |
| VLM177 | Esperança | 792455 | 8187566 | 8 | 233 | 21 | 19 | 5 | 50 | 3.5 |
| VLM179 | Esperança | 792329 | 8187637 | 24 | 49 | 49 | 30 | 18 | 50 | 6.57 |
| VLM181 | Esperança | 792275 | 8187672 | 6 | 34 | 14 | 6 | 5 | 50 | 3.14 |
| VLM186 | Esperança | 792402 | 8187770 | 20 | 38 | 34 | 11 | 12 | 50 | 4.65 |
| VLM199 | Esperança | 793145 | 8187908 | 10 | 30 | 35 | 70 | 5 | 50 | 55.42 |
| VLM206 | Esperança | 792704 | 8187639 | 21 | 434 | 14 | 551 | 23 | 50 | 5.58 |
| VLM207 | Esperança | 792674 | 8187621 | 26 | 1775 | 43 | 944 | 55 | 50 | 8.45 |
| VLM208 | Esperança | 792674 | 8187624 | 8 | 39 | 18 | 20 | 5 | 50 | 2.16 |
| VLM209 | Esperança | 792676 | 8187623 | 2.5 | 37 | 5 | 19 | 5 | 50 | 1.91 |
| VLM210 | Esperança | 792673 | 8187622 | 24 | 265 | 233 | 539 | 46 | 50 | 1.47 |
| VLM211 | Esperança | 792675 | 8187622 | 53 | 29 | 38 | 11 | 5 | 283 | 49.46 |
| SRL001 | Esperança | 792693 | 8187679 | 7 | 153 | 52 | 18 | 5 | 50 | 10.47 |
==> picture [843 x 53] intentionally omitted <==
| Sample ID | Project | Easting (UTM 23S) | Northing (UTM 23S) | Be (ppm) | Li (ppm) | Nb (ppm) | Sn (ppm) | Ta (ppm) | W (ppm) | Y (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|
| SRL002 | Esperança | 792693 | 8187679 | 2.5 | 39 | 5 | 6 | 5 | 50 | 3.55 |
| SRL003 | Esperança | 792699 | 8187641 | 154 | 1130 | 69 | 1141 | 117 | 50 | 9.12 |
| SRL004 | Esperança | 792699 | 8187641 | 22 | 76 | 85 | 88 | 120 | 50 | 12.81 |
| SRL005 | Esperança | 792254 | 8187678 | 22 | 26 | 39 | 16 | 15 | 50 | 10.85 |
| SRL006 | Esperança | 792449 | 8187561 | 166 | 43 | 75 | 25 | 36 | 50 | 25.74 |
| SRL007 | Canabrava | 794748 | 8192381 | 2.5 | 19 | 5 | 7 | 5 | 50 | 4.1 |
| SRL008 | Esperança | 792536 | 8187475 | 31 | 1325 | 169 | 373 | 30 | 50 | 5.67 |
| SRL009 | Esperança | 792795 | 8187714 | 11 | 34 | 32 | 17 | 5 | 50 | 1.48 |
| SRL010 | Esperança | 792417 | 8187715 | 6 | 51 | 36 | 19 | 5 | 50 | 1.51 |
Appendix 2 - Table 1: Reporting Visual Estimates of Mineralisation
| Project | Sample ID | Geology/Comments |
|---|---|---|
| Esperança | VLM207 | Spodumene mineral species are confirmed for sample VLM207 through laboratory use of a Bruker BRAVO Raman spectrometer. The proportion of spodumene minerals are reported as visual estimates only and mineral percentages are shown in Appendix 2 Table 2 below. Whole Rock lithium content is shown in Appendix 1 Table 2 above. |
Appendix 2 - Table 2: All Pegmatite Field Descriptions Within the Esperança Project
| Sample ID | Easting (UTM 23S) |
Northing (UTM 23S) |
Lithology | Campaign | Primary Minerals (Major >30%) |
Secondary Minerals (Minor >5% and <30%) |
Accessory Minerals (Trace <5%) |
Boulder /In-Situ |
Comments |
|---|---|---|---|---|---|---|---|---|---|
| VLM009 | 803852 | 8194803 | Pegmatite | 2024 | Feldspar | Muscovite, Quartz |
Outcrop | Large pegmatite, rich muscovite, albite, and quartz | |
| VLM022 | 803896 | 8194826 | Pegmatite | 2024 | Muscovite, Feldspar |
Schlorite | Outcrop | Pegmatite with very rich muscovite, schorlite and feldspar |
|
| VLM029 | 803255 | 8194579 | Pegmatite | 2024 | Feldspar | Muscovite, Quartz |
Outcrop | Artisanal digging, composed quartz, albite and muscovite, small tunnel |
|
| VLM030 | 803234 | 8194603 | Pegmatite | 2024 | Feldspar | Muscovite, Quartz |
Outcrop | Old artisanal digging, pegmatite composed by albite, quartz and muscovite |
==> picture [843 x 53] intentionally omitted <==
| Sample ID | Easting (UTM 23S) |
Northing (UTM 23S) |
Lithology | Campaign | Primary Minerals (Major >30%) |
Secondary Minerals (Minor >5% and <30%) |
Accessory Minerals (Trace <5%) |
Boulder /In-Situ |
Comments |
|---|---|---|---|---|---|---|---|---|---|
| VLM032 | 803185 | 8194636 | Pegmatite | 2024 | Quartz | Feldspar | Outcrop | Old Artisanal digging, composed by core quartz and edge feldspar |
|
| VLM039 | 803451 | 8195112 | Pegmatite | 2024 | Quartz | Feldspar | Outcrop | Pegmatite with quartz core and edge feldspar, Old digging |
|
| VLM055 | 803227 | 8195722 | Pegmatite | 2024 | Feldspar | Muscovite, Quartz |
Outcrop | Large block pegmatite with feldspar, muscovite, and quartz |
|
| VLM072 | 794984 | 8192062 | Pegmatite | 2024 | Muscovite, Quartz |
Feldspar, Tourmaline |
Float | Pegmatite fine, with light green muscovite, quartz, feldspar and tourmaline |
|
| VLM080 | 794614 | 8192526 | Pegmatite | 2024 | Feldspar | Outcrop | Pegmatite, coarse feldspar | ||
| VLM107 | 795258 | 8193586 | Pegmatite | 2024 | Feldspar, Quartz |
Tourmaline | Float | Block rolled pegmatite with tourmaline, coarse and fine | |
| VLM122 | 794653 | 8192722 | Pegmatite | 2024 | Quartz, Tourmaline |
Muscovite, Feldspar |
Outcrop | In drainage subcrop pegmatite fine, composed by quartz, tourmaline, muscovite, and albite |
|
| VLM138 | 792121 | 8187833 | Pegmatite | 2024 | Quartz, Tourmaline |
Muscovite, Feldspar |
Outcrop | Pegmatite rich tourmaline, quartz, muscovite, and feldspar |
|
| VLM149 | 791982 | 8187642 | Pegmatite | 2024 | Feldspar, Quartz |
Tourmaline | Outcrop | In drainage subcrop pegmatite coarse tourmaline rich and muscovite |
|
| VLM157 | 792170 | 8187904 | Pegmatite | 2024 | Feldspar, Quartz |
Tourmaline, Muscovite |
Outcrop | Large outcrop pegmatite, composed by tourmaline, feldspar, quartz and muscovite, |
|
| VLM163 | 791996 | 8187840 | Pegmatite | 2024 | Feldspar, Quartz |
Muscovite | Float | Pegmatite composed quartz, albite, and light green muscovite |
|
| VLM165 | 791937 | 8187715 | Pegmatite | 2024 | Feldspar | Quartz | Outcrop | Largepegmatite, concordant with foliation | |
| VLM176 | 792478 | 8187543 | Pegmatite | 2024 | Quartz, Tourmaline |
Muscovite, Feldspar |
Outcrop | Subcrop pegmatite, texture graphic, composed by quartz, tourmaline, feldspar, and muscovite |
|
| VLM177 | 792455 | 8187566 | Pegmatite | 2024 | Quartz, Muscovite |
Feldspar | Outcrop | Old digging in pegmatite, rich quartz, muscovite, and feldspar. |
|
| VLM179 | 792329 | 8187637 | Pegmatite | 2024 | Feldspar, Tourmaline |
Quartz, Muscovite |
Outcrop | Large outcrop pegmatite, composed by tourmaline, feldspar, quartz,and muscovite |
|
| VLM181 | 792275 | 8187672 | Pegmatite | 2024 | Muscovite, Quartz |
Feldspar, Tourmaline |
Outcrop | Large coarse and fine pegmatite outcrop, width 5 meters, composed by quartz, muscovite, feldspar, and tourmaline schorlite |
==> picture [843 x 53] intentionally omitted <==
| Sample ID | Easting (UTM 23S) |
Northing (UTM 23S) |
Lithology | Campaign | Primary Minerals (Major >30%) |
Secondary Minerals (Minor >5% and <30%) |
Accessory Minerals (Trace <5%) |
Boulder /In-Situ |
Comments |
|---|---|---|---|---|---|---|---|---|---|
| VLM186 | 792402 | 8187770 | Pegmatite | 2024 | Feldspar, Tourmaline |
Quartz, Muscovite |
Outcrop | Large coarse and fine pegmatite outcrop rich tourmaline, feldspar, quartz and muscovite. Width 20 meters |
|
| VLM199 | 793145 | 8187908 | Pegmatite | 2024 | Muscovite, Quartz |
Feldspar, Tourmaline |
Outcrop | Subcrop pegmatite rich muscovite light green and small tourmaline |
|
| VLM206 | 792704 | 8187639 | Pegmatite - Spodumene |
2024 | Feldspar | Quartz, Muscovite |
Spodumene | Outcrop | Digging, large pegmatite containing crystals of highly altered spodumene |
| VLM207 | 792674 | 8187621 | Pegmatite - Spodumene |
2024 | Quartz, Spodumene |
Feldspar, Muscovite |
Outcrop | Selective mineral sample selection for analysis from Artisanal mine in zoned pegmatite. Spodumene sampled zone(55%quartz and 35% spodumene) |
|
| VLM208 | 792674 | 8187624 | Pegmatite | 2024 | Feldspar | Quartz, Muscovite, Tourmaline |
Garnet, Spodumene, Tantalite and beryl |
Outcrop | Artisanal mine in zoned pegmatite. Gallery with quartz plus spodumene zone (55% quartz and 5% spodumene) |
| VLM209 | 792676 | 8187623 | Pegmatite | 2024 | Feldspar | Quartz | Float | Feldspar - concentrated, minor quartz | |
| VLM210 | 792673 | 8187622 | Pegmatite | 2024 | Muscovite | Feldspar | Float | Large light green muscovite concentrate | |
| VLM211 | 792675 | 8187622 | Pegmatite | 2024 | Feldspar | Columbite, Tantalite? |
Float | Dark mineral, possible columbite or tantalite | |
| SRL001 | 792693 | 8187679 | Pegmatite | 2024 | Feldspar, Muscovite |
Quartz, Schorlite |
Outcrop | Trench in pegmatite that ended in schist. Kf, radial white mica, qtz, Ox. Mn, schorlite. |
|
| SRL002 | 792693 | 8187679 | Pegmatite | 2024 | Feldspar, Muscovite |
Quartz, Schorlite |
Outcrop | Trench in pegmatite that ended in schist. Kf, radial white mica, qtz, Ox. Mn, schorlite. |
|
| SRL003 | 792699 | 8187641 | Pegmatite - Spodumene |
2024 | Feldspar, Quartz |
Muscovite | Spodumene | Outcrop | Highly weathered spodumene within Feld+Qtz+Musc, two samples taken |
| SRL004 | 792699 | 8187641 | Pegmatite - Spodumene |
2024 | Feldspar, Quartz |
Muscovite | Spodumene | Outcrop | Highly weathered spodumene within Feld+Qtz+Musc, two samples taken |
| SRL005 | 792254 | 8187678 | Pegmatite | 2024 | Feldspar, Quartz |
Tourmaline, Muscovite |
Garnet | Outcrop | Outcrop of pegmatite in the drainage. kf, ab, qtz, schorlite, green mus and garnet. Very similar to Luciano'speg. |
==> picture [843 x 53] intentionally omitted <==
| Sample ID | Easting (UTM 23S) |
Northing (UTM 23S) |
Lithology | Campaign | Primary Minerals (Major >30%) |
Secondary Minerals (Minor >5% and <30%) |
Accessory Minerals (Trace <5%) |
Boulder /In-Situ |
Comments |
|---|---|---|---|---|---|---|---|---|---|
| SRL006 | 792449 | 8187561 | Pegmatite | 2024 | Feldspar, Quartz |
Tourmaline, Muscovite |
Garnet | Outcrop | Old trench that intercepted a robust peg with kf, ab, qtz, green mus, schorlite and garnet. |
| SRL007 | 794748 | 8192381 | Pegmatite | 2024 | Feldspar, Quartz |
Muscovite, Schorlite |
Pyrolusite? | Float | Large peg boulder, with ab, qtz, mus, schorlite, Mn oxide. Moderately weathered. |
| SRL008 | 792536 | 8187475 | Pegmatite | 2024 | Feldspar, Quartz |
Muscovite, Schorlite |
Outcrop | Peg outcrop in drainage with ab, kf, qtz, green mica, shorlite. Thickness 1m and indefinite length. |
|
| SRL009 | 792795 | 8187714 | Pegmatite | 2024 | Feldspar, Quartz |
Muscovite, Schorlite |
Pyrolusite? | Float | Attempted artisanal mine that took floats of peg. Kf, qtz, green mica and Mn oxide. |
| SRL010 | 792417 | 8187715 | Pegmatite | 2024 | Feldspar, Quartz |
Muscovite, Schorlite |
Outcrop | Decimeter scale blocks of peg. Kf, ab, qtz, green mica and schorlite. Coarse and fine texture. |