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LIGHTNING MINERALS LTD — Capital/Financing Update 2025
Feb 5, 2025
65212_rns_2025-02-05_be38843b-040d-42df-b899-7017fee20934.pdf
Capital/Financing Update
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Drill Contractor Appointed for Esperança Project to Test Spodumene Bearing Pegmatites – Mobilisation Underway
ASX Announcement 6 February 2025
Lightning Minerals (L1M or the Company) is pleased to report that Energold Drilling S.A. has been selected as the preferred contractor for drilling at the Esperança project in the Lithium Valley region of Minas Gerais, Brazil. Drilling will be targeting spodumene pegmatites discovered at Esperança project in November 2024 (ASX Announcement 18 November 2024 and ASX Announcement 17 January 2025).
HIGHLIGHTS
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Up to 2,000m of drilling to test spodumene within pegmatites at the Esperança lithium project to begin the week of 15[th] February 2025
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elevated lithium in soil anomalies
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Energold Drilling S.A. has been selected as preferred drill contractor after the completion of a drill tender process and contractor evaluation
Lightning Minerals Managing Director Alex Biggs said, “It’s always exciting to begin a new drill program and with the targets we have generated the next logical step is to begin drill testing at the Esperança project. Our team has worked hard over the past 6-months to define strong lithium targets in a very prospective region. Our inaugural drill program in the Lithium Valley is only the first target of multiple areas that have been identified that demonstrate significant lithium potential across all three project areas: Esperança, Caraíbas and Canabrava. We welcome Energold Drilling S.A. as our Brazilian drilling contractors and wish our team a safe and productive drilling campaign. We look forward to keeping the market updated on our progress”.
Drilling to Begin at Esperança Project
A diamond drill program for up to 2,000m will begin at the Company’s Esperança lithium project the week starting 15[th] February. Mobilisation is currently underway. The program is designed to follow recent priority drill targets identified through regional geochemical sampling and geological mapping campaigns.
The program is designed to test for the potential of fresh pegmatites beneath the currently identified pegmatites at and near surface, which are highly weathered.
The drill program will be conducted utilising Energold’s specialist modular drill rigs which minimise clearing requirements, environmental impacts and allow for flexibility in drilling. This is important as drill plans may change as further information on the target area is understood as the drill program advances.
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08)
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Figure 1: Preliminary Esperança drill plan
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Figure 2: Energold SA modular drill rig
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08)
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Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08)
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Figure 3: Soil sampling and rock chip sampling locations (lithium) at the Esperança project
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Esperança Spodumene Discovery
During the Company’s extensive ground reconnaissance and soil sampling works across its three project areas in the Lithium Valley of Minas Gerais, Brazil: Esperança, Caraíbas and Canabrava artisanal workings were discovered at the Esperanca project (ASX Announcement 18 November 2024).
Mineral sample VLM207 yielded initial LIBS results of 4.04%Li20 with whole rock assays yielding 0.38% Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) Li20. This is to be expected as samples taken from the discovery site were taken from a highly weathered profile. The upcoming drill program will target areas greater than 30m in depth where subcropping, fresh spodumene pegmatites may be present (ASX Announcement 17 January 2025).
Raman analysis has also been completed using a Bruker BRAVO Raman spectrometer which confirmed the presence of spodumene plus the highly weathered nature of the samples (ASX Announcement 17 January 2025).
A summary of lithium is soil results >150ppm Lithium is presented in Appendix 1, Table 1. A summary of rock chip samples is presented in Appendix 1, Table 2. A summary of visual estimates of sample VLM207 is presented in Appendix 2, Table 1. A summary of pegmatite field descriptions is presented in Appendix 2, Table 2.
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08)
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Figure 4a (left): Zoned spodumene bearing pegmatite discovered at the Esperança project Source of selective spodumene sample VLM207. Figure 4b (right): Large elongate spodumene crystals (Spd) up to 50cm in length showing homogeneous growth patterns amongst a quartz (Qtz) and Feldspar (Fdsp) rich matrix. (Rock descriptions for samples presented in Appendix 2, Table 2)
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Ongoing Works in Brazil
In parallel to the Company’s inaugural drill program at the Esperança project ground reconnaissance is continuing at both the Caraíbas and Canabrava projects where lithium in soil anomalism up to 429ppm Lithium and 320ppm Lithium have been identified respectively (ASX Announcement 17 January 2025). Drill targeting is being evaluated across multiple target areas with plans for drilling later in 2025.
Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08)
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08)
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Figure 5: Lightning Minerals’ tenements in in the Lithium Valley region of Minas Gerais (Regional
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location)
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08)
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Figure 6: Lightning Minerals’ Brazilian tenements in in the Lithium Valley region of Minas Gerais
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08)
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Approved for release by the Board of Directors
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More information at www.lightningminerals.com.au
Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08)
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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 critical 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 other 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 differ 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)
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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 results are 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 results are 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 results are reported |
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| Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. The total length andpercentage of the relevant intersections logged. |
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|---|---|---|
| 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 |
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| 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 and 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. |
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| 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. |
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|---|---|---|
| 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. |
• Up to 2,000m of Diamond drilling of the target described in the report above is expected to commence shortly. • 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. |
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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 |
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| 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 [842 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 [842 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 [842 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 | Large pegmatite, 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 [842 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 [842 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. |