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LIGHTNING MINERALS LTD — Capital/Financing Update 2024
Apr 21, 2024
65212_rns_2024-04-21_640ab42b-b071-47b5-9b04-5f7f47a3952c.pdf
Capital/Financing Update
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Acquisition of Bengal Mining - Highly Prospective Lithium Projects in Brazil’s Lithium Valley
ASX Announcement 22 April 2024
Lightning Minerals ( L1M or the Company ) is excited to announce the signing of a binding agreement to acquire Bengal Mining Pty Ltd ( Bengal ) which holds, via its wholly owned subsidiary Tigre Mineracao Ltda ( Tigre ) option agreements over two lithium projects, Caraíbas and Sidrônio (the Projects ) in Brazil’s prolific Lithium Valley district in the state of Minas Gerais ( Proposed Acquisition ).
The Company views the Proposed Acquisition as transformative for its future, leveraging the strategic proximity of the projects to Latin Resources’ (ASX: LRS) Colina project[1] hosting 70.3Mt @ 1.27% Li20 and Sigma Lithium’s (NASDAQ: SGML) Grota do Cirilo project[2] hosting 108.9Mt @ 1.41% Li20. The Projects have been acquired from Bengal, a privately held Australian company which holds exclusive options across all seven (7) tenements totalling 3,372 Ha.
HIGHLIGHTS
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Resources’ (ASX: LRS) Colina project
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chip assay results grading up to 0.53% Li2O (lepidolite)
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assay results are considered positive exploration indicators
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Strong aeromagnetic geophysical trends correlate with regional mineralised trends
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Projects lie within geology of the Salinas Formation which hosts other lithium Resources in the region
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Proposed Transaction based on 5Mt, 10Mt and 20Mt Resource milestones presenting significant upside at both a project and company level demonstrating vendor confidence
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Oversubscribed placement of A$1.5M at A$0.07 per share to facilitate work program
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Field work to commence as soon as deal completion and approval at Company EGM
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fieldwork expertise and insights
Note 1: Further exploration work to verify historically mapped and sampled pegmatites is necessary. The scale of the geological outcrops are unknown and the presence of pegmatitic lithologies does not necessarily indicate the presence of lithium, tantalum or caesium mineralisation. Note 2: The Company is op@mis@c about concluding the transac@on and acquisi@on outlined herein, however at the date of this announcement no assurance that the condi@ons precedent with respect to the transac@on will be met. Accordingly, investors are cau@oned against making investment decisions based on this announcement.
Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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It is with great excitement that Lightning Minerals announces what it considers the transformative Proposed Acquisition of the Projects in the Lithium Valley region of Minas Gerais, Brazil. The Projects are located in the Eastern Brazilian Pegmatite Province which currently hosts two world class lithium deposits: Latin Resources’ (ASX: LRS) Colina project and Sigma Lithium’s (NASDAQ: SGML) Grota do Cirilo project.
The Company is planning to begin on-ground works as soon as the Proposed Acquisition is finalised. Early-stage reconnaissance works indicate presence of lithium bearing minerals (lepidolite) with the immediate strategy to now confirm potential and then test via drilling. The Projects are subject to an exclusive option agreement that allows the Company flexibility in its exploration approach to determine the most prospective opportunities that it sees most value in based on initial work programs.
Lightning Minerals Managing Director Alex Biggs said , “This Proposed Acquisition represents a significant transaction for the Company. We believe in the lithium thematic and see now as a great opportunity to acquire highly prospective projects in known and established lithium regions. Minas Gerais in Brazil has emerged as a proven lithium hub with the acquisition located in close proximity to the world class lithium resources of Latin Resources’ (ASX: LRS) Colina project and Sigma Lithium’s (NASDAQ: SGML) Grota do Cirilo project. The Project presents some excellent early indicators of lithium mineralisation with prospective underlying geology that offers clear exploration targets. As part of the transaction we welcome new key shareholders, to the Company and look forward to the next stage of evolution of the business. It is exciting to see the Company developing and expanding our influence; we now have projects in three of the predominant lithium regions in the world: Dundas in Western Australia, Quebec in Canada and Mina Gerais in Brazil. We look forward to starting our on-ground works in Brazil and also progressing works on our other projects in Western Australia and Canada”.
About the Projects and Minas Gerais as a Lithium Region
The Projects are located in the Lithium Valley region of Minas Gerais, Brazil. The Projects cover 3,372 Ha comprising seven (7) exploration licences and are located approximately 20km south of Latin Resources’ (ASX: LRS) Colina lithium project and 60km north-west of Signa Lithium’s (NASDAQ: SGML) Grota do Cirilo project (Figure 1). The region has emerged as one of the world’s premier lithium districts over the past few years and presents significant exploration potential.
The Company will benefit from access to a seasoned ground team, providing invaluable fieldwork expertise and insights, enhancing the Company's strategic approach to exploration. Relationships the Company already has in the region will help facilitate project growth and advancement.
Minas Gerais is Brazil’s third largest economy with over 300 mines operating in the state with tier-1 operators including Vale, BHP and Rio Tinto. The state boasts a strong mining labour pool and presents a cost competitive jurisdiction for exploration and project development with mature infrastructure, hydro power and road access.
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Figure 1: Location of Caraíbas and Sidrônio projects
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Caraíbas and Sidrônio Projects
The Projects are located in the Eastern Brazilian Pegmatite Province that encompasses approximately 150,000 km[2] , stretching from Bahia state to Rio de Janeiro state. The Caraíbas Project consists of five (5) separate tenements covering 1,733 Ha and the project area contains a series of albite and muscovite rich pegmatites identified by Bengal’s initial reconnaissance works. Aeromagnetic data shows the tenements are located along regional structures and shear zones which are analogous to the trends present at Latin Resources’ (ASX: LRS) Colina deposit. The Caraíbas Project is located approximately 20km to the south in the same Salinas geological formation.
The Sidrônio Project consists of two (2) tenements covering 1,638 Ha, strategically located adjacent and along strike to the south from the Caraíbas Project. Aeromagnetic data shows the tenements are located along similar interpreted structural trends that may potentially be conduits for mineralisation.
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Figure 2: Caraíbas and Sidrônio project location, geology and tenements
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Both Projects cover prospective Salinas Formation geology which is thought to provide adequate rheological conditions suitable for the emplacement of late hydrothermal fluids. In similar geological settings, proximal to S-type granites, the Salinas Formation is known to host fertile lithium mineral bearing pegmatites.
Records from the ‘Project Evaluation of the Potential of Lithium in Brazil’ - Servico Geologico do Brasil (Geological Service of Brazil)[3] indicate that historic prospecting or fossicking may have occurred with the Caraíbas Project. At this location an inactive mine location is recorded as ‘LB-43 Lavra Luís Rocha – Caraíbas’ which is interpreted to be a small-scale prospecting excavation. The area was then targeted by Bengal company geologists in late 2023 as part of a small reconnaissance program to identify lithium prospectivity in the region. Three rock chip samples were taken from the site with peak assay results of 0.53% Li2O, 1,245 ppm tantalum, 1,175 ppm rubidium and 1,455 ppm caesium (Table 1). Geological descriptions of the rock samples are shown in Table 2, and photographs of BLR237 and VLR1269 are shown in Figure 3(a) and Figure 3 (b) respectively.
These results are considered encouraging and support the thesis that pegmatites in the project areas might have favourable geochemistry and fractionation conditions. Elevated tantalum levels are considered a good indicator of potential for adequate fractionation conditions and will form a key part of the Company’s initial reconnaissance works and analysis. These results warrant immediate follow up exploration and will form part of the near-term exploration plan for the Caraíbas project. A full table of results for samples taken from the project areas are included in Appendix 2, Table 1.
Table 1: Assay data associated with samples taken at historic “inactive mine” location
| Field Name |
Target | Easting (UTM 23S) |
Northing | Ta ppm | Li2O % |
K/R b |
||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
(UTM |
Cs ppm | Li ppm | Nb ppm | Rb ppm | Sn ppm | |||||||
| 23S) | ||||||||||||
| BLR238 | Caraibas | 803813 |
8194761 |
704 | 1281 | 801 | 665 | 272 | 1245 | 0.28 | 29 | |
| BLR237 | Caraibas | 803812 | 8194766 | 1455 | 2457 | 64 | 1175 | 103 | 196 | 0.53 | 24 | |
| VLR1269 | Caraibas | 803808 | 8194765 | 124 | 97 | 5 | 574 | 2.5 | 5 | 0.01 | 64 | |
Table 2: Geological descriptions associated with samples taken at historic “inactive mine” location.
| Field Name | Target | Easting (UTM 23S) |
Northing | Geology Description |
|---|---|---|---|---|
(UTM |
||||
| 23S) | ||||
| BLR238 | Caraibas | 803813 |
8194761 |
Gpe (pegmatite) whitish with >> schorlite + lepidolite |
| BLR237 | Caraibas | 803812 | 8194766 | Presence of rubellite and lepidolite. Zoned lepidolite (external halo with Li) |
| VLR1269 | Caraibas | 803808 | 8194765 | Pegmatite rich in Lepidolite (Li) and light green tourmaline(?) |
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Figure 3: (A) Photograph of sample BLR237 showing lepidolite minerals (purple) within pegmatite sample (B) Photograph of sample VLR1269 showing lepidolite minerals (purple) within pegmatite sample (C) Photographic example of workings located within the larger Caraíbas tenement area (805118mE, 8193908mN). Samples collected by Bengal Mining
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Regional Geology, Prospectivity and Trends
The Eastern Brazilian Pegmatite Province is a globally recognised region for hard rock lithium prospectivity. The Colina and Grota do Cirilo Project Lithium resources highlight the potential for the region to host Tier 1 lithium deposits.
Like Caraíbas and Sidrônio, these deposits are located within the Salinas Formation proximal to PostCollisional Magmatism which are of the Type-S granitic geochemistry. S-Type granites are known to be favourable and form part of the genetic model for the creation of lithium-caesium-tantalum (LCT) deposits. The Salinas Formation commonly includes lithologies such as mica-quartz schists and quartzmica schists with localised intercalations of rocks, calcium-silicates, meta conglomerates and micaceous quartzites. Reconnaissance work by Bengal has identified similar rock types at both the Caraibas and Sidronio projects which are considered positive indicators when looking at the projects in a regional context.
Multiple prospective geophysical trends have been identified through interpretation of publicly available aeromagnetic data from the Servico Geologico do Brasil (Geological Service of Brazil) which correlates with the parallel mineralised corridor that hosts Latin Resources’ (ASX: LRS) Colina deposit. These trends will form the basis of further on-ground mapping, reconnaissance, and sampling across the tenements with a view to defining drill targets.
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Figure 4: Caraíbas and Sidrônio projects location and tenements plotted against publicly available analytic signal aeromagnetic image from Servico Geologico do Brasil (Geological Service of Brazil)
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Program of Works and Use of Funds
The option agreements that the Company has acquired via Bengal allows for clear identification of drill targets prior to full acquisition of the Project areas, either in full or in part. The Company has existing relationships with contractors and personnel in the region which will significantly accelerate its work programs and has a strong relationship with other operators in the region.
The following work programs will be completed across all projects. These work plans are subject to change as the Company develops further knowledge of the Project areas.
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Table 3: Initial work program strategy Caraíbas and Sidrônio projects
| Work Program | Timing | Use of Funds (A$) | Notes |
|---|---|---|---|
| Ground reconnaissance – mapping and sampling | 10 weeks | 200,000 | To run concurrently |
| Geophysical drone survey | 8 weeks | 100,000 | |
| Drill target identification | 8 weeks | 50,000 | |
| Phase 1 drilling | 12 weeks | 960,000 | |
Table 4: Initial work program schedule Caraíbas and Sidrônio projects
| Work Program | Jun 24 |
Jul 24 |
Aug 24 |
Sep 24 |
Oct 24 |
Nov 24 |
Dec 24 |
|---|---|---|---|---|---|---|---|
| Ground reconnaissance – mapping and sampling | |||||||
| Geophysical drone survey and interpretation | |||||||
| Drill target identification | |||||||
| Phase 1 drilling |
Proposed Acquisition Terms
The Company has entered into a binding share sale agreement with the majority shareholders of Bengal to acquire all the issued capital of Bengal. Bengal holds exclusive options via its wholly owned subsidiary Tigre, to purchase seven (7) tenements located in Brazil’s Lithium Valley region in the state of Minas Gerais, comprising the Projects.
Subject to obtaining all regulatory and shareholder approvals, the initial consideration payable for the acquisition of 100% of the shares in Bengal is as follows:
Consideration
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a) 22,142,857 fully ordinary paid shares in the Company ( Shares ) to the value of A$1,550,000 based on a deemed issue price of $0.07 per Share ( Consideration Shares );
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b) 6,000,000 L1M options, with an exercise price of $0.105 being a 50% premium to the Share price of $0.07 and an expiry date of three years from the date of issue ( Consideration Options ); and
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c) 39,999,999 performance rights that will convert into Shares on a one-for-one basis, subject to the satisfaction of the milestones outlined below ( Performance Rights ).
The issue of the Consideration Shares, the Performance Rights and the Shares issued on conversion of the Performance Rights will be subject to voluntary escrow for a period of 12 months from the date of issue.
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Milestones
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a) Milestone 1: 14,285,714 Performance Rights to vest into Shares subject to the Company delineating a JORC compliant Mineral Resource Estimate on the Projects of at least 5Mt grading at least 1.0% Li2O within three years from the date of issue;
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b) Milestone 2: 14,285,714 Performance Rights to vest into Shares subject to the Company delineating a JORC compliant Mineral Resource Estimate on the Projects of at least 10Mt grading at least 1.0%Li2O within four years from the date of issue; and
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c) Milestone 3: 11,428,571 Performance Rights to vest into Shares subject to the Company delineating a JORC compliant Mineral Resource Estimate on the Projects of at least 30Mt grading at least 1.0%Li2O within five years from the date of issue.
Exclusive Option Exercise
Bengal (via its wholly owned subsidiary Tigre) has exclusive options across all tenements under the following terms in Table 5. This allows the Company to conduct early-stage exploration quickly and effectively to then determine which of the tenements are appropriate to exercise, minimising the upfront expenditure.
Table 5: Exclusive option agreement terms
| Project | Option Period |
Option Fee |
Monthly Fee (US$) |
Option Exercise (US$) |
Bonus (US$) | Royalty | Status |
|---|---|---|---|---|---|---|---|
| Caraíbas | 24 month |
100K (Paid) |
5K | 1M per tenement |
Nil | Nil | Landowner signed |
| Sidrônio | 12 month |
70K (Paid) | Nil | 200K per tenement |
200K if 10Mt @ 1.3% Li20 or greater |
1% NSR | Landowner signed |
Conditions Precedent
The Proposed Acquisition is subject to the following conditions precedent:
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the minority shareholders of Bengal executing a binding share sale agreement;
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satisfaction of the Company’s due diligence investigations;
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the repayment of loans owed by Tigre;
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the Company obtaining any necessary ASX or shareholder approvals, including issue of the Consideration Shares, Consideration Options, Performance Rights and Tranche 2 Placement Shares and Options (defined below); and
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The parties obtaining any required third party approvals.
Cautionary Statement
The Company is optimistic about concluding the Proposed Acquisition, however, at the date of this announcement there is no assurance that the conditions precedent with respect to the Proposed Acquisition will be met. Accordingly, investors are cautioned against making investment decisions based on this announcement.
Dilutionary Effect of Transaction
The below table shows the potential dilution of existing shareholders as a result of the Proposed Acquisition.
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Table 6: Dilutionary effect of transaction
| Capital Structure | Shares | % | Options | Performance Rights |
|---|---|---|---|---|
| Existing Securities | 49,864,034 | 50.20 | 37,258,543 | 4,800,000 |
| Consideration Securities | 22,142,857 | 22.29 | 6,000,000 | 39,999,999 |
| Placement Securities | 21,428,571 | 21.57 | 10,714,286 | - |
| S3 Consortium Pty Ltd (Stocks Digital) | 5,892,857 | 5.93 | - | - |
| Total Post Completion | 99,328,320 | 100.00 | 53,972,829 | 44,799,999 |
Placement
The Company has received firm commitments in relation to a placement from new and existing professional and sophisticated investors to raise A$1.50 million by the issue of 21,428,571 Shares at an issue price of $0.07 ( Placement Shares ), with attaching quoted options ( L1MO ) exercisable at A$0.25 each and expiring 13 March 2028 ( Placement Options ) on the basis of 1 option for every 2 Placement Shares subscribed for ( Placement ).
The Placement will take place in two tranches as follows:
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(a) 7,479,605 Placement Shares issued on 29 April 2024 utilising the Company’s placement capacity under Listing Rule 7.1, raising a total of A$523,572 (before costs) ( Tranche 1 ); and
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(b) 13,948,966 Placement Shares and 10,714,286 Placement Options subject to shareholder approval pursuant to Listing Rule 7.1 and Listing Rule 10.11 (Listing Rule 10.11 director participation detailed below), to raise a total of A$976,428 before costs ( Tranche 2 ).
The Company engaged PAC Partners Securities Pty Ltd as lead manager and broker to the Placement and will receive a fee of 6%.
Company directors Francesco Cannavo, Alex Biggs and Craig Sharpe will participate in tranche 2 of the placement, subscribing for securities to the value of A$20,000, A$15,000 and A$10,500 respectively. The director’s participation in tranche 2 of the placement is subject to shareholder approval for the purposes of ASX Listing Rule 10.11.
Extraordinary General Meeting (EGM)
The issue of the Consideration Shares, Consideration Options, Performance Rights and the Tranche 2 Placement Shares and Options will be subject to the Company obtaining shareholder approval at an upcoming EGM of its shareholders.
Relevance of Proposed Acquisition
Brazil has emerged in recent years as a significant lithium mining region with Latin Resources (ASX: LRS) Colina lithium project and Signa Lithium’s (NASDAQ: SGML) Grota do Cirilo project being the most advanced and largest scale lithium projects in Brazil. The Eastern Brazilian Pegmatite Province in Minas Gerais, which hosts the Company’s proposed acquisitions, is hole to 100% of Brazil’s official lithium reserves. Also operating in the region is Lithium Ionic Corp. (TSXV: LTH) who have recently been delineating its initial Mineral Resource Estimate at its Bandeira Project 29.5Mt @ 1.37% Li20 (13.72 Mt @ 1.40% Li20 Measured + Indicated), 15.79Mt @ 1.34% Li20 Inferred) further demonstrating the
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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prospectivity of the region. A Pre Economic Assessment (PEA) demonstrated a IRR of 121% and NPV8 post tax of C$1.6 Billion (see TSXV announcement 30 November 2023).
Mining is a key driver of the economy in both Minas Gerais and Brazil. Figure 5 demonstrates the impact that mining has had on Minas Gerais’ Industrial Production Index (IPI) in 2023. In December 2023 Minas Gerais exported US$3.56 Billion of goods. Between December 2022 and December 2023. The exports of Minas Gerais have increased by US$722 Million (25.5%) from US$2.84 Billion to US$3.56 Billion with the dominant commodities being minerals (mainly iron ore and ferro alloys) and raw sugar.
Figure 5: Minas Gerais industrial grow in 2023
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Source: CEIC
The Proposed Acquisition is relevant to the Company as it expands its influence into some of the world’s premier lithium mining regions. Active exploration is key to the Company’s modus operandi and acquisition of projects that sit within proven geological domains is an important step in working towards a discovery. Optionality on a jurisdictional basis also provides additional opportunities and investors that may have a preference for specific jurisdictions and their related commodities.
The Company has existing relationships within the region that can be utilised to ensure efficient deployment of exploration teams to identify drill targets as quickly as possible.
References
1Latin Resources’ (ASX: LRS) Colina project hosting 70.3Mt @ 1.27% Li20 (1.73Mt @ 1.47% Li20 Measured, 39.29 Mt @ 1.36% Li20 Indicated, 29.26Mt @1.13% Li20 Inferred)
2Sigma Lithium’s (NASDAQ: SGML) Grota do Cirilo project hosting 108.9Mt @ 1.41% Li202 (94.3Mt @ 1.40% Li20 Measured and Indicated, 14.6Mt @ 1.37% Li20 Inferred)
3Servico Geologico do Brasil (Geological Service of Brazil): https://rigeo.cprm.gov.br/jspui/handle/doc/17451
Approved for release by the Board of Directors -END-
More information at www.lightnmingminerals.com.au
Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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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 Company’s agship Dundas project is located in the prolic Dundas region of Western Australia. The Company also owns the Dalmas and Hiver lithium projects in Quebec, Canada, another signicant and evolving lithium region globally as well as other projects in Western Australia which include Mt Jewell, 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 identied 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 uctuations 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 nancial, 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 dened 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 conrms 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 conrms that the form and context in which the Competent Person’s ndings are presented have not been materially modied from the original market announcement.
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Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Appendix 1: Caraíbas and Sidrônio Projects – JORC Code 2012 Table 1 Criteria
The Table below summarises the assessment and reporting criteria used for exploration results for the Caraíbas and Sidrônio 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 explana@on | Commentary |
|---|---|---|
| Sampling techniques | Nature and quality of sampling (eg cut channels, random chips, or specifc specialised industry standard measurement tools appropriate to the minerals under inves;ga;on, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limi;ng the broad meaning of sampling. Include reference to measures taken to ensure sample represen;vity and the appropriate calibra;on of any measurement tools or systems used. Aspects of the determina;on of mineralisa;on that are Material to the Public Report. In cases where ‘industry standard’ work has been done this would be rela;vely simple (eg ‘reverse circula;on drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fre assay’). In other cases more explana;on may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodi;es or mineralisa;on types (eg submarine nodules) may warrant disclosure of detailed informa;on. |
• The 2023 rock chip sampling program was completed by Bengal Mining Contract geologists. • The rock chip samples were collected at the natural surface, these have been subdivided into outcrop, Subcrop, foat, and ‘digging’ samples as per Appendix 3 table 1. • Samples submiHed to the analyIcal laboratory are at the discreIon of the representaIve geologist. • The rock chip samples were assayed via ICM90A (fusion by sodium peroxide and fnish with ICP-MS/ICP-OES) for a 56-element suite at the SGS Geosol Laboratorios located at Vespasiano/Minas Gerais, Brazil. • No control samples have been used at this stage. The internal laboratory controls (blanks, duplicates and standards) are considered suitable. • Sample sites are located using a handheld GPS device which is considered accurate to within 6m using Datum SIRGAS 2000, Zone 23 South. |
| Drilling techniques | Drill type (eg core, reverse circula;on, 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 drill 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 representa;ve nature of the samples. Whether a rela;onship exists between sample recovery and grade and whether sample bias may have occurred due to preferen;al loss/gain of fne/coarse material. |
• No drill 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 es;ma;on, mining studies and metallurgical studies. Whether logging is qualita;ve or quan;ta;ve in nature. Core (or costean, channel, etc) photography. The total length and percentage of the relevant intersec;ons logged. |
• All rock chip samples are geologically described by suitably experienced and qualifed in-country geologists. • Rock descripIons are qualitaIve in nature and consider geological aspects such as lithology, mineralisaIon, mineralogy, weathering, and colour. • Photographs are taken of samples for each sample and stored on Bengal Mining IT infrastructure. • The feld lithological descripIons and subsequent reporIng of pegmaItes are not indicaIve of economic pegmaIte hosted mineralisaIon. Further exploraIon work including an assessment of the current rock chip samplingresults will be required to confrm thepresence of anymineralisaIon. |
| Lev Sub-sampling techniques and sample prepara;on |
el 6 505 Little Collins St Melbourne VIC 3000 Australia | ad If core, whether cut or sawn and whether quarter, half or all core taken. |
==> picture [842 x 52] intentionally omitted <==
| If non-core, whether rifed, tube sampled, rotary split, etc and whether sampled wet or dry. For all sample types, the nature, quality and appropriateness of the sample prepara;on technique. Quality control procedures adopted for all sub-sampling stages to maximise represen;vity of samples. Measures taken to ensure that the sampling is representa;ve of the in situ material collected, including for instance results for feld duplicate/second-half sampling. Whether sample sizes are appropriate to the grain size of the material being sampled. |
• The selected sample is considered appropriate for the early stage of exploraIon at the Caraíbas and Sidrônio projects. |
|
|---|---|---|
| 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 par;al or total. For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading ;mes, calibra;ons factors applied and their deriva;on, etc. Nature of quality control procedures adopted (eg standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (ie lack of bias) andprecision have been established. |
• Rock Chip samples were assayed via ICM90A (fusion by sodium peroxide and fnish with ICP-MS/ICP-OES) for a 56-element suite at the SGS Geosol Laboratorios located at Vespasiano/Minas Gerais, Brazil. • No control samples have been used at this early stage of exploraIon. The internal laboratory controls (blanks, duplicates and standards) are considered suitable. |
| Verifca;on of sampling and assaying |
The verifca;on of signifcant intersec;ons by either independent or alterna;ve company personnel. The use of twinned holes. Documenta;on of primary data, data entry procedures, data verifca;on, data storage (physical and electronic) protocols. Discuss any adjustment to assay data. |
• The CP independently verifed sampling, assay and geological results from a externally maintained and stored geological database. • Assay data and results are reported, unadjusted. • Li2O results used in the market are converted from Li results mulIplying it by the industry factor 2.153. |
| Loca;on of data points | Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other loca;ons used in Mineral Resource es;ma;on. Specifca;on of the grid system used. Quality and adequacy of topographic control. |
• Handheld GPS instruments were used to geo locate each drill collar, these instruments are understood to be accurate within a nominal ±6m in the horizontal and verIcal planes. • The level of topographic control ofered by a handheld GPS is considered sufcient for early exploraIon drilling. • All samples were collected in the SIRGAS 2000 Datum,Zone 23 South. |
| Data spacing and distribu;on |
Data spacing for repor;ng of Explora;on Results. Whether the data spacing and distribu;on is sufcient to establish the degree of geological and grade con;nuity appropriate for the Mineral Resource and Ore Reserve es;ma;on procedure(s) and classifca;ons applied. Whether sample composi;ng has been applied. |
• The sample spacing is considered appropriate for the reporIng of the reconnaissance exploraIon results. • No Mineral Resource or Ore Reserve EsImates have been completed. • No sample composiIng has been applied. |
| Orienta;on of data in rela;on to geological structure |
Whether the orienta;on of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type. If the rela;onship between the drilling orienta;on and the orienta;on of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material. |
• Due to the preliminary nature of the reconnaissance sampling campaign, rock samples are designed to test specifc outcropping or sub cropping targets, with no set spacing. |
| Sample security | The measures taken to ensure sample security. | • The chain of custody for sampling procedures and sample analysis was managed by Bengal Company geologists duringreconnaissance works |
==> picture [842 x 52] intentionally omitted <==
Audits or reviews 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 explana@on | Commentary |
|---|---|---|
| Mineral tenement and land tenure status |
Type, reference name/number, loca;on and ownership including agreements or material issues with third par;es such as joint ventures, partnerships, overriding royal;es, na;ve ;tle interests, historical sites, wilderness or na;onal park and environmental se_ngs. The security of the tenure held at the ;me of repor;ng along with any known impediments to obtaining a licence to operate in the area. |
• Bengal Mining Ltd, via its wholly owned subsidiary Tigre Mineracao Ltda, holds exclusive opIons to acquire the Tenements that comprise the Caraíbas and Sidrônio Projects in accordance with opIon agreements. • The Carabias Project includes exploraIon licences 831.514/2018, 832.041/2011, 831.424/2013, 832.763/2014, 830.313/2014. • The Sidrônio Project includes exploraIon licences 830.439/2015, 830.440/2015. • The Caraíbas and Sidrônio Project area totals ~33km2and comprises seven granted Research AuthorisaIon licences and two mining request areas (Appendix 3) • The Tenements are considered ingood standingat the Ime of this report. |
| Explora;on done by other par;es |
Acknowledgment and appraisal of explora;on by other par;es. |
• The Caraíbas and Sidrônio Projects are at a very early stage and liHle work has been explored by prior explorers. • Recent exploraIon has included a small reconnaissance exploraIon program by project vendor Bengal Mining. The informaIon contained within this report references the work Bengal have completed which supports the Lightning Minerals acquisiIon. • State datasets including the ‘Project EvaluaIon of the PotenIal of Lithium in Brazil’ form the Servico Geologico do Brasil (Geological Service of Brazil) are publicly available at Servico Geologico do Brasil (Geological Service of Brazil) hHps://rigeo.cprm.gov.br/jspui/handle/doc/17451 publicaIons. • Review of the historic exploraIon informaIon has been completed. |
| Geology | Deposit type, geological se_ng and style of mineralisa;on. | • No known mineral deposits occur within the project tenure. • The Caraíbas and Sidrônio Lithium Project geology comprises Neoproterozoic age sedimentary rocks of Araçuaí Orogen intruded by pegmaItes interpreted to originate from the fracIonaIon of magmaIc fuids from the peraluminous S-type post tectonic granitoids of Araçuaí Orogen. • The target commodityis hardrock lithium within lithium-caesium-tantalumpegmaItes. |
| Drill hole Informa;on | A summary of all informa;on material to the understanding of the explora;on results including a tabula;on of the following informa;on for all Material drill holes: oeas;ng and northing of the drill hole collar oeleva;on or RL (Reduced Level – eleva;on above sea level in metres) of the drill hole collar odown hole length and intercep;on depth, ohole length. If the exclusion of this informa;on is jus;fed on the basis that the informa;on 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. |
• No drillhole informaIon is reported |
| Data aggrega;on methods |
In repor;ng Explora;on Results, weigh;ng averaging techniques, maximum and/or minimum grade trunca;ons (eg cu_ng of high grades) and cut-of grades are usually Material and should be stated. Where aggregate intercepts incorporate short lengths of high-grade results and longer lengths of lowgrade results, theprocedure usedfor such |
• No levelling of the raw geochemical data was undertaken. • Li2O results used in the market are converted from Li results mulIplying it by the industry factor 2.153. • Plan images have been generated using QGGIS soqware. • No metal equivalent values are reported. |
==> picture [842 x 52] intentionally omitted <==
| aggrega;on should be stated and some typical examples of such aggrega;ons should be shown in detail. |
||
|---|---|---|
| Rela;onship between mineralisa;on widths and intercept lengths |
These rela;onships are par;cularly important in the repor;ng of Explora;on Results. If the geometry of the mineralisa;on 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 efect(eg ‘down hole length, true width not known’). |
• No drillhole informaIon is reported. • There is insufcient data provided by the mapping and rock chip results contained within this report for a relaIonship between pegmaIte and mineral resources to be reported. |
| Diagrams | Appropriate maps and sec;ons (with scales) and tabula;ons of intercepts should be included for any signifcant discovery being reported These should include, but not be limited to a plan view of drill hole collar loca;ons and appropriate sec;onal views. |
• Appropriate reporIng of results has been included in the body of this announcement; the plans, or lack thereof suitably represent the nature of the exploraIon results. |
| Balanced repor;ng | Where comprehensive repor;ng of all Explora;on Results is not prac;cable, representa;ve repor;ng of both low and high grades and/or widths should be prac;ced to avoid misleading repor;ng of Explora;on Results. |
• Comprehensive reporIng of all rock chip samples within the Caraíbas and Sidrônio projects has been included in Appendix 2 - Table 1. • PerInent informaIon has been communicated to ensure balanced and representaIve reporIng of exploraIon results has been achieved. |
| Other substan;ve explora;on data |
Other explora;on data, if meaningful and material, should be reported including (but not limited to): geological observa;ons; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteris;cs; poten;al deleterious or contamina;ng substances. |
• All meaningful data and relevant informaIon have been included in the body of the report. |
| Further work | The nature and scale of planned further work (eg tests for lateral extensions or depth extensions or large-scale step-out drilling). Diagrams clearly highligh;ng the areas of possible extensions, including the main geological interpreta;ons and future drilling areas, provided this informa;on is not commercially sensi;ve. |
• Further work is outlined, budgeted and scheduled in secIon ‘Program of Works and Use of Funds’ contained within the body of the report. • The planning of drilling of the reported pegmaItes is dependent on a further phases of exploraIon providing saIsfactory results to warrant that scale of exploraIon works. |
==> picture [842 x 52] intentionally omitted <==
APPENDIX 2 - TABLE 1 – Analytical results for Bengal Mining reconnaissance program
| Field Name | Project Area |
Easting (UTM 23S) |
Northing (UTM 23S) |
Point Type | Geologic Description | Be ppm |
Cs ppm | K ppm | Li ppm | Nb ppm |
Rb ppm |
Sn ppm |
Ta ppm | Li % ppm |
Li2O% | K/Rb |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| BLR059 | Caraíbas | 801358 | 8194279 | Outcrop | Valley. Peg (Qz+Felds). Coarse tourmaline(indicolite) hosted by fne-grained CST(?)/Bt-schist. PEG 112/58. Sn 136/36 |
8 | 19.6 | 23621 | 41 | 5 | 195 | 2.5 | 5 | 0.00 | 0.01 | 121.13 |
| BLR062 | Caraíbas | 800223 | 8194625 | Subcrop | In situ PEG. | 78 | 17.5 | 30073 | 20 | 19 | 287 | 70 | 5 | 0.00 | 0.00 | 104.78 |
| BLR066 | Caraíbas | 800589 | 8194533 | Outcrop | Floor of road. Qtz-Spods/Felds | 9 | 3.1 | 12065 | 93 | 5 | 44 | 2.5 | 5 | 0.01 | 0.02 | 274.20 |
| BLR237 | Caraíbas | 803812 | 8194766 | Outcrop | Contact SCH-GPE. LB-43 - Presence of rubelite and lepidolite. Zoned lepidolite (external halo with Li). |
48 | 1455.6 | 28983 | 2457 | 64 | 1175 | 103 | 196 | 0.25 | 0.53 | 24.67 |
| BLR238 | Caraíbas | 803813 | 8194761 | Outcrop | Gpe (pegmaIte) whiIsh with >>schorlite + lepidolite. |
12 | 704.6 | 19693 | 1281 | 801 | 665 | 272 | 1245 | 0.13 | 0.28 | 29.61 |
| VLR1269 | Caraíbas | 803808 | 8194765 | Digging | PegmaIte rich in lepidolite (Li) and light green tourmaline(?) |
20 | 124.6 | 36937 | 97 | 5 | 574 | 2.5 | 5 | 0.01 | 0.02 | 64.35 |
| BLR233 | Caraíbas | 800277 | 8194702 | Outcrop | PegmaIte low angle. 40cm thickness. Green mica (LiIophilite)+quartz (petalite?). Presence of hyalinequartz vein. |
16 | 15 | 29528 | 5 | 23 | 309 | 188 | 5 | 0.00 | 0.00 | 95.56 |
| BLR064 | Caraíbas | 800237 | 8194676 | Outcrop | Stopped road crossed by drainage. Schist with large blocks of PEG (Musc+Qtz+Felds). Spod replaced bymusc(?). Sn 148/64 |
48 | 14.3 | 27711 | 5 | 19 | 282 | 184 | 5 | 0.00 | 0.00 | 98.27 |
| BLR232 | Caraíbas | 800283 | 8194700 | Float | Float (insitu?) Probable spodumene silicifed pseudomorph. |
9 | 3.8 | 10211 | 148 | 5 | 47 | 2.5 | 5 | 0.01 | 0.03 | 217.26 |
| BLR234 | Caraíbas | 802238 | 8195505 | Outcrop | Localidade Riachinho. Milk quartz vein with fractures flled by oxide Fe-Mn. Regional shear zone. Blank source. |
2.5 | 0.5 | 500 | 5 | 5 | 4 | 2.5 | 5 | 0.00 | 0.00 | 125.00 |
| VLR1298 | Caraíbas | 800192 | 8195040 | Subcrop | PegmaIte blocks chip. Presence tourmaline, feldspar, quartz and muscovite. |
46 | 29 | 30050 | 12 | 23 | 336 | 25 | 13 | 0.00 | 0.00 | 89.43 |
| VLR1297 | Caraíbas | 800121 | 8194970 | Subcrop | Floats of coarse feldspar, quartz, tourmaline andgarnet |
14 | 14.1 | 23857 | 27 | 21 | 297 | 51 | 5 | 0.00 | 0.01 | 80.33 |
| VLR1313 | Caraíbas | 801684 | 8193412 | Digging | Mining ornamental rocks. Large PegmaIte barren. Contact schist discordant. Quartz, tourmaline,albite and muscovite. |
10 | 16.6 | 24195 | 83 | 12 | 176 | 16 | 5 | 0.01 | 0.02 | 137.47 |
| VLR1304 | Caraíbas | 800037 | 8195488 | Outcrop | PegmaIte in river. Large outcrop. ComposiIon shorlite, quartz, muscovite and albite. Exposure at 12 meters. |
63 | 48.3 | 38204 | 101 | 19 | 575 | 49 | 5 | 0.01 | 0.02 | 66.44 |
| VLR1301 | Caraíbas | 800201 | 8195302 | Subcrop | PegmaIte blocks. No presence tourmaline. Crystal feldspar,quartz and muscovite |
93 | 42.7 | 26639 | 27 | 31 | 427 | 92 | 17 | 0.00 | 0.01 | 62.39 |
| VLR1296 | Caraíbas | 800104 | 8194927 | Float | Presence light green mica ( Li) in pegmaIte. Quartz and albite. |
137 | 29.7 | 30096 | 5 | 5 | 283 | 45 | 5 | 0.00 | 0.00 | 106.35 |
==> picture [842 x 52] intentionally omitted <==
| VLR1278 | Caraíbas | 801382 | 8194268 | Outcrop | Contact schist and pegmaIte with thickness 20 cm. Tourmaline, quartz, feldspar and muscovite. |
38 | 25.1 | 47210 | 5 | 5 | 333 | 5 | 5 | 0.00 | 0.00 | 141.77 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| VLR1302 | Caraíbas | 800077 | 8195454 | Outcrop | PegmaIte with presence tourmaline, quartz, albite and muscovite. In drainage. |
295 | 35.3 | 18736 | 16 | 16 | 256 | 37 | 5 | 0.00 | 0.00 | 73.19 |
| VLR1314 | Caraíbas | 801698 | 8193365 | Digging | Presence green mica, tourmaline, feldspar, quartz.. Borders are fnegrained. |
2.5 | 7.3 | 20015 | 10 | 5 | 148 | 2.5 | 5 | 0.00 | 0.00 | 135.24 |
| VLR1309 | Caraíbas | 800157 | 8195477 | Subcrop | PegmaIte rich muscovite. No occurrence tourmaline. ComposiIon:quartz and albite. |
68 | 83.2 | 39885 | 23 | 27 | 481 | 103 | 14 | 0.00 | 0.00 | 82.92 |
| VLR1319 | Caraíbas | 802135 | 8193553 | Outcrop | Presence light green mica (Li), tourmaline, quartz, albite. Low anglepegmaIte system. |
12 | 52.4 | 35478 | 27 | 14 | 289 | 9 | 5 | 0.00 | 0.01 | 122.76 |
| VLR1275 | Caraíbas | 801176 | 8194300 | Subcrop | Subcrop pegmaIte with tourmaline, feldspar and muscovite |
24 | 7.1 | 36061 | 46 | 5 | 185 | 6 | 5 | 0.00 | 0.01 | 194.92 |
| VLR1320 | Caraíbas | 802284 | 8193680 | Subcrop | Presence green mica, tourmaline, feldspar, quartz.. Borders are fnegrained. |
7 | 8.2 | 30804 | 33 | 21 | 188 | 26 | 5 | 0.00 | 0.01 | 163.85 |
| VLR1270 | Caraíbas | 800433 | 8194506 | Digging | PegmaIte | 25 | 12.6 | 26540 | 5 | 19 | 306 | 119 | 5 | 0.00 | 0.00 | 86.73 |
| VLR1316 | Caraíbas | 801580 | 8193362 | Digging | Mining ornamental rocks. Large PegmaIte barren. Contact schist discordant. Quartz, tourmaline, feldspar and muscovite. Graphic texture. Two sampling points. |
9 | 29.4 | 37173 | 102 | 5 | 255 | 9 | 5 | 0.01 | 0.02 | 145.78 |
| VLR1318 | Caraíbas | 801953 | 8193475 | Outcrop | Presence light green mica (Li), tourmaline, quartz, albite. Low anglepegmaIte system. |
10 | 12.6 | 34568 | 23 | 5 | 192 | 17 | 5 | 0.00 | 0.00 | 180.04 |
| VLR1312 | Caraíbas | 800252 | 8195177 | Outcrop | PegmaIte. Tourmaline, feldspar, quartz and muscovite. |
111 | 25.1 | 23224 | 24 | 13 | 276 | 32 | 5 | 0.00 | 0.01 | 84.14 |
| VLR1294 | Caraíbas | 802416 | 8194251 | Outcrop | Presence tourmaline feldspar, muscovite. Low angle systempegmaIte. |
2.5 | 10.3 | 65970 | 18 | 5 | 315 | 5 | 5 | 0.00 | 0.00 | 209.43 |
| VLR1289 | Caraíbas | 804010 | 8194282 | Outcrop | Composite lepidolite (?), quartz, feldspar and tourmaline. Low angle |
6 | 2.4 | 22759 | 5 | 5 | 78 | 2.5 | 5 | 0.00 | 0.00 | 291.78 |
| VLR1288 | Caraíbas | 803803 | 8194324 | Digging | PegmaIte barren. ComposiIon quartz, feldspar, tourmaline and lepidolite (possible?) Two sampling points. Mica with possible halo with Li |
68 | 69.8 | 26615 | 80 | 5 | 266 | 2.5 | 5 | 0.01 | 0.02 | 100.06 |
| VLR1279 | Caraíbas | 801561 | 8194338 | Outcrop | Great exposure on the pegmaIte river. ComposiIon tourmaline, feldspar, albite, quartz and muscovite. |
123 | 46.7 | 39492 | 11 | 22 | 375 | 7 | 5 | 0.00 | 0.00 | 105.31 |
| VLR1277 | Caraíbas | 801352 | 8194277 | Outcrop | PegmaIte rich tourmaline and muscovite, moderate weathered. |
7 | 12.6 | 16147 | 5 | 5 | 118 | 2.5 | 5 | 0.00 | 0.00 | 136.84 |
| VLR1323 | Caraíbas | 793813 | 8196363 | Float | Floats Quartz hyaline | 2.5 | 0.2 | 500 | 5 | 5 | 1.5 | 2.5 | 5 | 0.00 | 0.00 | 333.33 |
| VLR1281 | Caraíbas | 801972 | 8194244 | Outcrop | Presence of schorlite bearing pegmaIte. Small crystal |
28 | 20.9 | 33497 | 5 | 12 | 300 | 2.5 | 5 | 0.00 | 0.00 | 111.66 |
| VLR1272 | Caraíbas | 800886 | 8194378 | Outcrop | PegmaIte with quartz, muscovite and albite. Rich in muscovite |
12 | 13.3 | 32648 | 5 | 5 | 294 | 82 | 5 | 0.00 | 0.00 | 111.05 |
==> picture [842 x 52] intentionally omitted <==
| VLR1273 | Caraíbas | 800927 | 8194390 | Outcrop | PegmaIte in river. ComposiIon quartz+ muscovite+ albite+ tourmaline (light green and shorlite). 45 cm thickness. Low angle |
10 | 16.3 | 34268 | 5 | 16 | 293 | 100 | 5 | 0.00 | 0.00 | 116.96 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| VLR1287 | Caraíbas | 803758 | 8194345 | Digging | PegmaIte barren. ComposiIon quartz, feldspar, tourmaline and lepidolite (possible?) |
7 | 54.3 | 52038 | 125 | 5 | 477 | 2.5 | 5 | 0.01 | 0.03 | 109.09 |
| VLR1276 | Caraíbas | 801157 | 8194325 | Outcrop | PegmaIte composite quartz + feldspar + tourmaline and muscovite. Large outcrop in drainage. PegmaIte system low angle. |
35 | 25.6 | 29474 | 15 | 11 | 288 | 38 | 5 | 0.00 | 0.00 | 102.34 |
| VLR1274 | Caraíbas | 800983 | 8194323 | Outcrop | PegmaIte in river. ComposiIon quartz+ muscovite+ feldspar + tourmaline (shorlite). 62 cm thickness. |
20 | 14.2 | 31208 | 10 | 5 | 254 | 34 | 5 | 0.00 | 0.00 | 122.87 |
| VLR1321 | Caraíbas | 802323 | 8193707 | Outcrop | Presence green mica, tourmaline, feldspar, quartz. Borders are fnegrained. |
5 | 11.7 | 50146 | 5 | 5 | 271 | 16 | 5 | 0.00 | 0.00 | 185.04 |
| VLR1352 | Caraíbas | 801187 | 8193608 | Digging | PegmaIte rich in tourmaline. Quartz, feldspar and muscovite. Old mining. |
2.5 | 28.3 | 75569 | 124 | 5 | 458 | 2.5 | 5 | 0.01 | 0.03 | 165.00 |
| VLR1353 | Caraíbas | 801222 | 8193589 | Digging | PegmaIte rich in tourmaline. Quartz, feldspar and muscovite. Old mining. Two sampling points. |
5 | 36.3 | 51024 | 153 | 5 | 346 | 12 | 5 | 0.02 | 0.03 | 147.47 |
| VLR1362 | Caraíbas | 801443 | 8193851 | Digging | Mining ornamental rocks. PegmaIte barren. Presence quartz geode and pockets Muscovites. |
52 | 17.8 | 13342 | 51 | 5 | 135 | 15 | 5 | 0.01 | 0.01 | 98.83 |
| VLR1358 | Caraíbas | 801263 | 8193911 | Digging | Mining ornamental rocks. Large PegmaIte barren. Rich oriented tourmaline, Lm N100. Quartz, garnet,muscovite andquartz. |
11 | 4.9 | 12426 | 115 | 5 | 86 | 7 | 5 | 0.01 | 0.02 | 144.49 |
| VLR1357 | Caraíbas | 800800 | 8193046 | Outcrop | Presence green mica, tourmaline, feldspar, quartz andgarnet. 5m wide. |
8 | 9.7 | 31192 | 23 | 5 | 188 | 11 | 5 | 0.00 | 0.00 | 165.91 |
| VLR1359 | Caraíbas | 801261 | 8193929 | Digging | Mining ornamental rocks. Large PegmaIte barren. Rich oriented tourmaline, Lm N100. Quartz, garnet, muscovite and quartz. Two sampling points. |
14 | 9 | 13908 | 117 | 10 | 131 | 14 | 5 | 0.01 | 0.03 | 106.17 |
| VLR1363 | Caraíbas | 801435 | 8193851 | Digging | Presence green mineral, Pockets rich muscovite | 12 | 35.5 | 26793 | 60 | 19 | 296 | 46 | 5 | 0.01 | 0.01 | 90.52 |
| VLR1355 | Caraíbas | 800969 | 8193254 | Subcrop | PegmaIte barren. Feldspar, muscovite, tourmaline and muscovite. |
55 | 20.3 | 33075 | 12 | 10 | 274 | 13 | 5 | 0.00 | 0.00 | 120.71 |
| VLR1351 | Caraíbas | 802248 | 8194058 | Outcrop | PegmaIte barren. Tourmaline, felspar and liHle muscovite. Graphic texture |
2.5 | 28.9 | 62816 | 16 | 16 | 304 | 15 | 5 | 0.00 | 0.00 | 206.63 |
| VLR1332 | Caraíbas | 802231 | 8195730 | Float | Floats pegmaIte. Rich muscovite. Quartz and albite. |
38 | 17.5 | 29828 | 20 | 45 | 353 | 5 | 15 | 0.00 | 0.00 | 84.50 |
| VLR1328 | Caraíbas | 802357 | 8195977 | Float | Block big quartz milky in drainage | 2.5 | 0.05 | 500 | 5 | 5 | 1.5 | 2.5 | 5 | 0.00 | 0.00 | 333.33 |
| VLR1342 | Caraíbas | 802458 | 8195200 | Float | Block big quartz milky in drainage | 2.5 | 0.2 | 500 | 5 | 5 | 1.5 | 2.5 | 5 | 0.00 | 0.00 | 333.33 |
| VLR1325 | Caraíbas | 800630 | 8195146 | Outcrop | Outcrop pegmaIte in drainage. Green mica, quartz,albite. |
82 | 45.8 | 25223 | 13 | 14 | 296 | 88 | 5 | 0.00 | 0.00 | 85.21 |
| GB956 | Sidrônio | 801173 | 8189207 | Outcrop | Sampling at BLR150 point. Pegmatoidal granite with black tourmaline, albite, quartz. Down |
29 | 5.6 | 40159 | 29 | 5 | 310 | 2.5 | 5 | 0.00 | 0.01 | 129.55 |
==> picture [842 x 52] intentionally omitted <==
| under, it seems to be actually a pegmaIte into schist foliaIon. 020/35 |
||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| GB957 | Sidrônio | 801142 | 8189167 | Outcrop | PegmaIte. Difuse contacts with schist. Feldspar, qtz, muscovite. Turmaline content is lower. Peg345/40 |
131 | 9.4 | 21757 | 64 | 50 | 307 | 21 | 5 | 0.01 | 0.01 | 70.87 |
| GB959 | Sidrônio | 801121 | 8188941 | Outcrop | PegmaIte (1m to 1.5 wide ) with alb, qtz, KF musc, tourmaline. PegmaIte is boudinage. (Photos). Peg355/30 |
66 | 10.5 | 47250 | 5 | 15 | 305 | 11 | 5 | 0.00 | 0.00 | 154.92 |
| GB960 | Sidrônio | 801141 | 8188897 | Outcrop | PegmaIte, 1.5 to 2m wide. Within foliaIon. Ab,qtz, musc, tourmaline. Peg345/30 |
87 | 9.2 | 35645 | 16 | 5 | 246 | 8 | 5 | 0.00 | 0.00 | 144.90 |
| GB961 | Sidrônio | 801216 | 8188899 | Outcrop | PegmaIte conInuity from gb960. Difuse contacts. |
31 | 5.2 | 25844 | 28 | 5 | 175 | 2.5 | 5 | 0.00 | 0.01 | 147.68 |
| GB966 | Sidrônio | 802039 | 8189069 | Outcrop | Pegmatoidal granite or graniIc pegmaIte. Large outcrop, >20m. Intrusion? Or big pegmaIte? Tourmaline+ab+qtz+muscovite. |
8 | 7.2 | 51394 | 44 | 5 | 356 | 6 | 5 | 0.00 | 0.01 | 144.37 |
| GB967 | Sidrônio | 802513 | 8189071 | Outcrop | Sample from BLR153 point. | 18 | 3.9 | 32300 | 34 | 5 | 183 | 2.5 | 5 | 0.00 | 0.01 | 176.50 |
| GB974 | Sidrônio | 794757 | 8192353 | Float | Float blocks of pegmaIte with ab,qtz, muscovite and scholite. Borders are fne grained |
203 | 48.6 | 21764 | 66 | 103 | 650 | 23 | 57 | 0.01 | 0.01 | 33.48 |
| GB976 | Sidrônio | 794817 | 8192401 | Float | PegmaIte blocks chip. Blocks do not present visible schorlite, when it does it occur in small quanIty. Ab+qrz rich,+ muscovite,Kf. |
155 | 128.8 | 22980 | 24 | 87 | 854 | 50 | 115 | 0.00 | 0.01 | 26.91 |
| GB977 | Sidrônio | 794881 | 8192319 | Outcrop | 0.5m wide low dipping pegmaIte. Ab,qtz,musc pegmaIte. Peg100/02 |
1032 | 157 | 20696 | 17 | 69 | 619 | 29 | 90 | 0.00 | 0.00 | 33.43 |
| GB978 | Sidrônio | 794881 | 8192335 | Outcrop | PegmaIte hanging wall, outcropping as a 'foor'. Peg015/10 |
136 | 154.5 | 26921 | 5 | 72 | 882 | 36 | 158 | 0.00 | 0.00 | 30.52 |
| GB979 | Sidrônio | 794916 | 8192298 | Outcrop | "Floor"" Outcrop at pegmaIte HW. Schorlite, Ab, qtz,musc. |
203 | 199.5 | 23820 | 12 | 83 | 1058 | 61 | 148 | 0.00 | 0.00 | 22.51 |
| GB1003 | Sidrônio | 799291 | 8190896 | Subcrop | PegmaIte subcrop. Narrow, n30w strike. Feldspar + mica +qtz + tourmaline. |
68 | 10.2 | 32379 | 5 | 5 | 209 | 37 | 5 | 0.00 | 0.00 | 154.92 |
| GB1016 | Sidrônio | 795245 | 8192848 | Float | Float small blocks of pegmaIte. Green mica, feldspar, qtz. Sampled |
131 | 234 | 31468 | 5 | 68 | 1662 | 145 | 74 | 0.00 | 0.00 | 18.93 |
| GB1017 | Sidronio | 795159 | 8192841 | Float | PegmaIte foats with schorlite (<5%) present. Green mica, feldspar, qtz. Fine to coarse grained. |
236 | 168.1 | 24858 | 5 | 109 | 1055 | 62 | 98 | 0.00 | 0.00 | 23.56 |
| GB1020 | Sidronio | 795023 | 8192669 | Float | Presence of schorlite bearing pegmaIte foats. Medium sized blocks. |
203 | 124.8 | 26608 | 5 | 72 | 995 | 32 | 53 | 0.00 | 0.00 | 26.74 |
| GB1023 | Sidronio | 794947 | 8192565 | Float | PegmaIte foats. Barren composiIon. Schorlite is rare in this block. |
251 | 133 | 36827 | 12 | 59 | 1275 | 46 | 60 | 0.00 | 0.00 | 28.88 |
| GB1027 | Sidronio | 795282 | 8192454 | Float | PegmaIte foats. Big blocks. Schorlite bearing - peg,fne to coarsegrain. |
133 | 156 | 31451 | 21 | 90 | 977 | 815 | 62 | 0.00 | 0.00 | 32.19 |
| GB1030 | Sidronio | 796574 | 8192297 | Subcrop | Tonhao area, presence of pegmaIte blocks. Muscovite,feldspar,schorlite, qtz. |
116 | 177.6 | 17895 | 40 | 61 | 699 | 165 | 52 | 0.00 | 0.01 | 25.60 |
==> picture [842 x 52] intentionally omitted <==
Level 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
==> picture [842 x 52] intentionally omitted <==
APPENDIX 3 – SUMMARY OF CARAÍBAS AND SIDRÔNIO TENEMENTS
| Project Area | Licence / Tenement Number |
Size (Ha) |
Status | Current Phase | Registered Owner |
|---|---|---|---|---|---|
| Caraibas | 831.514/2018 | 176.41 | Active | Research Authorisation | Caraibas Granito Mineracao Exportacao e Importacao Ltda |
| 832.041/2011 | 716.85 | Active | MiningRequest | ||
| 831.424/2013 | 677.17 | Active | MiningRequest | ||
| 832.763/2014 | 134.56 | Active | Research Authorisation | ||
| 830.313/2014 | 28.34 | Active | Research Authorisation | ||
| Sidronio | 830.439/2015 | 705.76 | Active | Research Authorisation | Sidronio Teixeira Filho |
| 830.440/2015 | 932.63 | Active | Research Authorisation | ||
| TOTAL | 3,372 | ||||
| Caraibas | 1733.33 | ||||
| Sidronio | 1638.39 |