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FIRST LITHIUM LIMITED — Capital/Financing Update 2024
Sep 9, 2024
64921_rns_2024-09-09_a09157b0-1bae-42a0-9eb2-bb97d5796912.pdf
Capital/Financing Update
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10 September 2024
FINAL RESULTS RECEIVED FOR BLAKALA; VERY HIGH Li₂O ANALYTICAL RESULTS FROM SECOND SERIES DRILLING CONFIRMS SIGNIFICANT DEPTH AND STRIKE CONTINUITY OF THE EASTERN PEGMATITE
HIGHLIGHTS
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Second Series holes drilled on Eastern and Western Pegmatites, as well as Southern extension of the Main Pegmatite on the Blakala Prospect, with Reverse Circulation (RC) pre-collars and diamond tails to intersect targeted pegmatites under the First Series diamond holes at depths of approximately 50 – 100m below the surface
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High grade analytical results received for Second Series diamond tails BRCD16 to BRCD21 drilled in the Eastern Pegmatite, with high grades from all these holes covering circa 400m strike (Figures 1 & 2):
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✓ BRCD21 with 24.00m intersection @ 1.53% Li2O (from 129.0m)
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✓ BRCD19 with 28.59m intersection @ 1.51% Li2O (from 117.0m)
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✓ BRCD18 with 9.00m intersection @ 1.62% Li2O (from 117.0m)
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High grade analytical results received for First Series diamond hole BDFS46 confirming the additional northern extension to the Eastern Pegmatite (Figure 1):
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✓ BDFS46 with 12.27m intersection @ 1.65% Li2O (from 46.0m)
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High grade analytical results received for Second Series diamond tail BRCD25 drilled on the Southern extension of the Main Pegmatite, which shows the depth continuity of the Southern extension of the Main Pegmatite and is in addition to the excellent results reported for the Main Pegmatite Second Series drilling (Figures 1 & 3):
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✓ BRCD25 with 8.34m intersection @ 1.77% Li2O (from 137.0m)
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High grade analytical results received for Second Series diamond tails drilled on the Western Pegmatite, showing the mineralisation at depth and the significant width of this pegmatite body (Figures 1 & 4):
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✓ BRCD28 with 25.64m intersection @ 1.68% Li2O (from 137.0m); and
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✓ BRCD36 with 15.00m intersection @ 1.23% Li2O (from 96.0m)
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FIRST LITHIUM LIMITED ACN 009 081 770 (FL1.ASX) https://firstlithium.com.au
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ASX ANNOUNCEMENT
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First Lithium Ltd (“FL1” or “the Company”) is pleased to announce the receipt of assay results for the First Series diamond drillholes BDFS40 to BDFS46 (Table 1) and diamond tails from the Second Series holes BRCD16 to BRCD36 at the priority - lithium prospect at Blakala (Table 2), located in the Gouna permit, Mali. The high to very high-grade Li₂O results from the First Series diamond drill holes BDFS45 and BDFS46, at the most southern and northern drillholes on the Eastern Pegmatite, shows this pegmatite is still open on strike in both directions. The high to very high-grade Li₂O results from the Second Series diamond drill holes are from the Eastern Pegmatite (BRCD16 to BRCD24), the Southern extension of the Main Pegmatite (BRCD25 - BRCD27) and the Western Pegmatite (BRCD28 – BRCD36). The high Li₂O grades from holes BRCD16 to BRCD21 on the Eastern Pegmatite; hole BRCD25 on the Southern extension of the Main Pegmatite; and holes BRCD28, BRCD32, BRCD34 and BRCD36 on the Western Pegmatite follow on from the excellent analytical results returned for the First and Second Series diamond holes in the Main, Eastern and Western Pegmatite Bodies ¹[,2,3,4] and the very high grades from outcrop sampling at surface. The results from the Eastern Pegmatite holes (Table 2) are at vertical depth of between 60 to 120m, and clearly show the depth and strike extension (grade is continuous between 6 holes with a circa 400m strike) at the depth of the Second Series holes (Figures 1 and 2). The high Li₂O results from a significant intersection thickness (25.64m) from the Second Series hole (BRCD28) on the Western Pegmatite (Table 2) shows the significant depth potential of the Western Pegmatite as well (Figures 1 and 4). The intersection is at circa 90 to 100m vertical depth. These intersections all show the pegmatites are still open at depth.
FL1 Managing Director, Venkat Padala said:
“Completion of the analytical results is a milestone the Company is very proud to achieve, next step is the maiden JORC for the Project which is expected in the coming month. This, along with license renewals also expected shortly, will provide a significant understanding of the scope and scale of this project, something all involved are excited to understand".
1 ASX:FL1 Announcement 20/12/2023 – Significant discovery confirmed at Blakala including 111m @ 1.57% Li2O
2 ASX:FL1 Announcement 22/01/2024 – Exceptional results from Blakala holes 4 to 15.
3 ASX:TSL Announcement 05/02/2024 - Blakala discovery expands with first assay results from Western pegmatite including 33.72m @ 1.59% Li2O and 17.00m @ 1.81% Li2O
4 ASX:FL1 Announcement 22/08/2024 – License renewals in progress, series two drilling analytical results identify very high Li2O within the main pegmatite at Blakala.
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DETAILS
Eastern Pegmatite RC and diamond drillholes
The First Series diamond drill holes BDFS41, BDFS43, BDFS45 and BDFS46 were drilled on the Eastern pegmatite. While hole BDFS41 in the northern extension of the eastern Pegmatite did not intersect significant mineralisation, hole BDFS46 which is further north and the most northern hole drilled on this pegmatite body did intersect a wide zone with very high-grade Li₂O results, indicating that this pegmatite is still open on strike in the north. Similarly, the very high-grade Li₂O results from hole BDFS45 shows this pegmatite is still open on strike in the south (Table 1; Figure 1).
In the Second Series drilling utilizing RC precollars and diamond tails, the aim of the drilling was to intersect the Eastern Pegmatite at a vertical depth of between 50 to 100m, thus below the First Series diamond holes which intersected the pegmatite at approximately 20 to 50m below surface. The RC precollars were drilled until they intersected the Eastern Pegmatite, drilling then continued with diamond tail drilling. In two of the RC holes some of the Eastern Pegmatite was intersected before drilling switched to diamond tail drilling; in hole BRCD17 the last RC drilling returned 3.00m at 1.58% Li₂0, while in hole BRCD18 the final metre of the RC hole returned 1.00m at 1.48% Li₂0. The 9 Second Series holes drilled on the Eastern Pegmatite (BRCD16 to BRCD24), 7 intersected high Li₂0 results; the strike and depth extent with high Li₂0 grades of the Eastern Pegmatite has now been clearly shown with approximately 400m of strike with high grades at surface in the outcrop, high grades in the First Series holes and high grades in the Second Series holes (Table 2; Figures 1 and 2).
Western Pegmatite RC and diamond drillholes
The First Series diamond drill hole BDFS44 was drilled in the southern area of the Western pegmatite, with no significant mineralisation (Table 1; Figure 1).
For the analytical results from the Second Series drill holes BRCD28 to BRCD36 on the Western Pegmatite, holes BRCD28, BRCD32, BRCD34 and BRCD36 have high to very high-grade Li₂O intersections (Table 2). Particularly hole BRCD28, which was drilled to intersect under the First Series hole BDFS17 and is the most northern drilling line on the western pegmatite, and this returned very high-grade Li₂O over a wide intersection with 1.68% Li₂O at an intersection width of 25.64m (Figure 4). The Western Pegmatite is therefore open to the north (Figure 1).
Main Pegmatite Southern extension RC and diamond drillholes
The First Series diamond drill holes BDFS40 and BDFS42 were drilled in the southern extension area of the Main pegmatite, with significant mineralisation being encountered in hole BDFS40 (Table 1; Figure 1).
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ASX ANNOUNCEMENT
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Results for the Second Series holes BRCD25 - BRCD27 show good results for hole BRCD25 with an intersection thickness of 8.34m and 1.77% Li₂O (Table 2; Figures 1 and 3).
The diamond drill results received are for 534 samples, and additionally the results for 47 QA/QC samples (Duplicates, AMIS sourced chip reference Blanks and AMIS sourced reference Standards) were also received. Good accuracy and precision were found on all 47 QA/QC samples.
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Figure 1: Locality and analytical results of Blakala First Series BDFS40 to BDFS46 diamond drill holes (black with white background) and Second Series diamond tail drill holes BRCD16 to BRCD36 (red with yellow background).
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ASX ANNOUNCEMENT
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Table 1: Sampling, analytical results and weighted intersections from First Series diamond holes BDFS40 to BDFS46.
| BHID | SAMP ID | FROM (m) | TO (m) | Interval (m) | LITH | Li % | Li2O% | Weighted Li2O% | Interval (m) |
|---|---|---|---|---|---|---|---|---|---|
| BDFS40 | K9177 | 59.54 | 60.54 | 1.00 | MGW + thin peg(3cm) | 0.06 | 0.13 | ||
| BDFS40 | K9178 | 60.54 | 61.00 | 0.46 | Peg | 0.03 | 0.07 | ||
| BDFS40 | K9181 | 61.00 | 62.00 | 1.00 | Peg | 0.37 | 0.80 | ||
| BDFS40 | K9182 | 62.00 | 63.00 | 1.00 | Peg | 0.10 | 0.21 | ||
| BDFS40 | K9183 | 63.00 | 64.00 | 1.00 | Peg | 0.46 | 0.99 | 1.83 | 5.50 |
| BDFS40 | K9184 | 64.00 | 65.00 | 1.00 | Peg | 0.99 | 2.13 | ||
| BDFS40 | K9185 | 65.00 | 66.00 | 1.00 | Peg | 0.72 | 1.55 | ||
| BDFS40 | K9186 | 66.00 | 67.00 | 1.00 | Peg | 0.94 | 2.01 | ||
| BDFS40 | K9187 | 67.00 | 68.00 | 1.00 | Peg | 1.34 | 2.88 | ||
| BDFS40 | K9188 | 68.00 | 68.50 | 0.50 | Peg | 0.48 | 1.04 | ||
| BDFS40 | K9189 | 68.50 | 69.50 | 1.00 | MGW | 0.08 | 0.18 | ||
| BDFS40 | NS | 69.50 | 91.96 | 22.46 | |||||
| BDFS40 | K9190 | 91.96 | 92.50 | 0.54 | MGW + thin peg(3cm) | 0.01 | 0.01 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | Interval (m) | LITH | Li % | Li2O% | Weighted Li2O% | Interval (m) |
| BDFS41 | K9191 | 5.50 | 6.50 | 1.00 | Sap of Schist | 0.02 | 0.04 | ||
| BDFS41 | K9192 | 6.50 | 7.00 | 0.50 | Sap of Peg | 0.03 | 0.07 | ||
| BDFS41 | K9193 | 7.00 | 8.00 | 1.00 | Sap of Peg | 0.02 | 0.05 | ||
| BDFS41 | K9194 | 8.00 | 9.00 | 1.00 | Sap of Peg | 0.03 | 0.07 | ||
| BDFS41 | K9195 | 9.00 | 10.00 | 1.00 | Sap of Peg | 0.05 | 0.10 | ||
| BDFS41 | K9196 | 10.00 | 11.00 | 1.00 | Sap of Peg | 0.04 | 0.09 | ||
| BDFS41 | K9197 | 11.00 | 12.00 | 1.00 | Sap of Peg | 0.04 | 0.08 | ||
| BDFS41 | K9198 | 12.00 | 13.00 | 1.00 | Sap of Peg | 0.05 | 0.11 | ||
| BDFS41 | K9201 | 13.00 | 14.00 | 1.00 | Sap of Peg | 0.06 | 0.13 | ||
| BDFS41 | K9202 | 14.00 | 15.00 | 1.00 | Sap of Peg | 0.06 | 0.13 | ||
| BDFS41 | K9203 | 15.00 | 16.00 | 1.00 | Sap of Peg | 0.04 | 0.09 | ||
| BDFS41 | K9204 | 16.00 | 17.00 | 1.00 | Sap of Peg | 0.06 | 0.13 | ||
| BDFS41 | K9205 | 17.00 | 18.00 | 1.00 | Sap of Peg | 0.04 | 0.10 | ||
| BDFS41 | K9206 | 18.00 | 19.00 | 1.00 | Sap of Peg | 0.02 | 0.05 | ||
| BDFS41 | K9207 | 19.00 | 20.00 | 1.00 | Sap of Peg | 0.05 | 0.10 | ||
| BDFS41 | K9208 | 20.00 | 21.00 | 1.00 | Sap of Peg | 0.04 | 0.08 | ||
| BDFS41 | K9209 | 21.00 | 22.00 | 1.00 | Sap of Peg | 0.03 | 0.07 | ||
| BDFS41 | K9210 | 22.00 | 23.00 | 1.00 | Sap of Peg | 0.04 | 0.08 | ||
| BDFS41 | K9211 | 23.00 | 24.00 | 1.00 | Sap of Peg | 0.04 | 0.08 | ||
| BDFS41 | K9212 | 24.00 | 25.00 | 1.00 | Sap of Peg | 0.04 | 0.08 | ||
| BDFS41 | K9213 | 25.00 | 25.50 | 0.50 | Sap of Peg | 0.06 | 0.13 | ||
| BDFS41 | K9214 | 25.50 | 26.50 | 1.00 | Sap of Peg | 0.04 | 0.10 | ||
| BDFS41 | K9215 | 26.50 | 27.00 | 0.50 | Peg | 0.05 | 0.11 | ||
| BDFS41 | K9216 | 27.00 | 28.00 | 1.00 | Peg | 0.06 | 0.12 | ||
| BDFS41 | K9217 | 28.00 | 29.00 | 1.00 | Peg | 0.05 | 0.12 | ||
| BDFS41 | K9218 | 29.00 | 30.00 | 1.00 | Peg | 0.04 | 0.09 | ||
| BDFS41 | K9221 | 30.00 | 31.00 | 1.00 | Peg | 0.07 | 0.14 | ||
| BDFS41 | K9222 | 31.00 | 32.00 | 1.00 | Peg | 0.33 | 0.70 | ||
| BDFS41 | K9223 | 32.00 | 32.50 | 0.50 | Peg | 0.29 | 0.61 | ||
| BDFS41 | K9224 | 32.50 | 33.50 | 1.00 | MGW | 0.19 | 0.42 | ||
| BDFS41 | K9225 | 33.50 | 34.00 | 0.50 | MGW | 0.20 | 0.43 | ||
| BDFS41 | K9226 | 34.00 | 35.00 | 1.00 | MGW | 0.11 | 0.24 |
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ASX ANNOUNCEMENT
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| BDFS41 | K9227 | 35.00 | 36.00 | 1.00 | MGW | 0.06 | 0.14 |
|---|---|---|---|---|---|---|---|
| BDFS41 | K9228 | 36.00 | 37.00 | 1.00 | MGW | 0.07 | 0.15 |
| BDFS41 | K9229 | 37.00 | 38.00 | 1.00 | MGW | 0.07 | 0.15 |
| BDFS41 | K9231 | 38.00 | 39.00 | 1.00 | MGW + thin peg(9cm) | 0.08 | 0.16 |
| BDFS41 | K9232 | 39.00 | 40.00 | 1.00 | MGW | 0.08 | 0.17 |
| BDFS41 | K9233 | 40.00 | 41.00 | 1.00 | MGW | 0.07 | 0.16 |
| BDFS41 | K9234 | 41.00 | 42.00 | 1.00 | MGW | 0.09 | 0.19 |
| BDFS41 | K9235 | 42.00 | 43.00 | 1.00 | MGW | 0.06 | 0.13 |
| BDFS41 | K9236 | 43.00 | 44.00 | 1.00 | MGW | 0.06 | 0.13 |
| BDFS41 | K9237 | 44.00 | 45.00 | 1.00 | MGW | 0.07 | 0.15 |
| BDFS41 | K9238 | 45.00 | 46.00 | 1.00 | MGW | 0.06 | 0.13 |
| BDFS41 | K9241 | 46.00 | 46.83 | 0.83 | MGW | 0.09 | 0.19 |
| BDFS41 | K9242 | 46.83 | 47.96 | 1.13 | Peg | 0.04 | 0.08 |
| BDFS41 | K9243 | 47.96 | 49.00 | 1.04 | MGW | 0.12 | 0.25 |
| BDFS41 | K9244 | 49.00 | 50.00 | 1.00 | Peg | 0.02 | 0.04 |
| BDFS41 | K9245 | 50.00 | 50.45 | 0.45 | Peg | 0.02 | 0.04 |
| BDFS41 | K9246 | 50.45 | 51.45 | 1.00 | MGW | 0.08 | 0.18 |
| BDFS41 | NS | 51.45 | 86.87 | 35.42 | |||
| BDFS41 | K9247 | 86.87 | 87.87 | 1.00 | MGW | 0.10 | 0.20 |
| BDFS41 | K9248 | 87.87 | 89.00 | 1.13 | Peg | 0.04 | 0.09 |
| BDFS41 | K9249 | 89.00 | 90.00 | 1.00 | Peg | 0.05 | 0.11 |
| BDFS41 | K9250 | 90.00 | 91.00 | 1.00 | Peg | 0.09 | 0.20 |
| BDFS41 | K9251 | 91.00 | 92.00 | 1.00 | Peg | 0.05 | 0.10 |
| BDFS41 | K9252 | 92.00 | 93.10 | 1.10 | Peg | 0.05 | 0.11 |
| BDFS41 | K9253 | 93.10 | 94.00 | 0.90 | MGW + thin peg(13cm) | 0.13 | 0.28 |
| BDFS41 | K9254 | 94.00 | 95.00 | 1.00 | MGW | 0.09 | 0.19 |
| BDFS41 | K9255 | 95.00 | 96.00 | 1.00 | MGW | 0.10 | 0.22 |
| BDFS41 | K9256 | 96.00 | 97.00 | 1.00 | MGW + thin peg(10cm) | 0.09 | 0.20 |
| BDFS41 | K9257 | 97.00 | 97.50 | 0.50 | MGW + thin peg(5cm) | 0.14 | 0.30 |
| BDFS41 | K9258 | 97.50 | 98.00 | 0.50 | Peg | 0.03 | 0.07 |
| BDFS41 | K9261 | 98.00 | 99.00 | 1.00 | Peg | 0.05 | 0.10 |
| BDFS41 | K9262 | 99.00 | 100.16 | 1.16 | Peg | 0.06 | 0.13 |
| BDFS41 | K9263 | 100.16 | 100.78 | 0.62 | MGW + thin peg(20cm) | 0.10 | 0.21 |
| BDFS41 | K9264 | 100.78 | 102.00 | 1.22 | MGW + thin peg(4cm) | 0.15 | 0.32 |
| BDFS41 | K9265 | 102.00 | 103.00 | 1.00 | MGW + thin peg(5cm) | 0.23 | 0.49 |
| BDFS41 | K9266 | 103.00 | 104.00 | 1.00 | MGW | 0.22 | 0.47 |
| BDFS41 | K9267 | 104.00 | 105.00 | 1.00 | MGW | 0.16 | 0.35 |
| BDFS41 | K9268 | 105.00 | 106.00 | 1.00 | MGW | 0.12 | 0.26 |
| BDFS41 | K9269 | 106.00 | 107.07 | 1.07 | MGW | 0.21 | 0.46 |
| BDFS41 | K9271 | 107.07 | 108.00 | 0.93 | Peg | 0.28 | 0.59 |
| BDFS41 | K9272 | 108.00 | 109.00 | 1.00 | Peg | 0.65 | 1.40 |
| BDFS41 | K9273 | 109.00 | 109.75 | 0.75 | Peg | 0.02 | 0.04 |
| BDFS41 | K9274 | 109.75 | 110.75 | 1.00 | MGW+Thin peg vein | 0.08 | 0.17 |
| BDFS41 | NS | 110.75 | 127.84 | 17.09 | |||
| BDFS41 | K9275 | 127.84 | 128.84 | 1.00 | Sch | 0.05 | 0.12 |
| BDFS41 | K9276 | 128.84 | 129.82 | 0.98 | Peg | 0.01 | 0.01 |
| BDFS41 | K9277 | 129.82 | 130.82 | 1.00 | MGW+Thin peg (5cm) | 0.06 | 0.13 |
| BDFS41 | NS | 130.82 | 143.83 | 13.01 | |||
| BDFS41 | K9278 | 143.83 | 144.83 | 1.00 | MGW | 0.02 | 0.05 |
| BDFS41 | K9281 | 144.83 | 145.44 | 0.61 | Peg | 0.00 | 0.01 |
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| BDFS41 | K9282 | 145.44 | 146.44 | 1.00 | MGW | 0.02 | 0.03 | ||
|---|---|---|---|---|---|---|---|---|---|
| BHID | SAMP ID | FROM (m) | TO (m) | Interval (m) | LITH | Li % | Li2O% | Weighted Li2O% | Interval (m) |
| BDFS43 | K9283 | 51.82 | 52.82 | 1.00 | MGW | 0.08 | 0.17 | ||
| BDFS43 | K9284 | 52.82 | 54.00 | 1.18 | Peg | 0.02 | 0.04 | ||
| BDFS43 | K9285 | 54.00 | 55.00 | 1.00 | Peg | 0.03 | 0.06 | ||
| BDFS43 | K9286 | 55.00 | 55.40 | 0.40 | Peg | 0.02 | 0.05 | ||
| BDFS43 | K9287 | 55.40 | 56.40 | 1.00 | MGW | 0.09 | 0.19 | ||
| BDFS43 | NS | 56.40 | 72.75 | 16.35 | |||||
| BDFS43 | K9288 | 72.75 | 73.75 | 1.00 | MGW | 0.11 | 0.24 | ||
| BDFS43 | K9289 | 73.75 | 74.04 | 0.29 | Peg | 0.03 | 0.07 | ||
| BDFS43 | K9290 | 74.04 | 75.40 | 1.36 | MGW | 0.12 | 0.25 | ||
| BDFS43 | K9291 | 75.40 | 75.80 | 0.40 | Peg | 0.01 | 0.03 | ||
| BDFS43 | K9292 | 75.80 | 77.00 | 1.20 | MGW | 0.10 | 0.22 | ||
| BDFS43 | K9293 | 77.00 | 78.00 | 1.00 | MGW | 0.06 | 0.14 | ||
| BDFS43 | K9294 | 78.00 | 79.00 | 1.00 | MGW | 0.08 | 0.18 | ||
| BDFS43 | K9295 | 79.00 | 80.00 | 1.00 | MGW | 0.09 | 0.19 | ||
| BDFS43 | K9296 | 80.00 | 81.00 | 1.00 | MGW | 0.10 | 0.21 | ||
| BDFS43 | K9297 | 81.00 | 81.90 | 0.90 | Peg+Thin MGW(26cm) | 0.06 | 0.12 | ||
| BDFS43 | K9298 | 81.90 | 83.00 | 1.10 | Peg+Thin MGW(10cm) | 0.16 | 0.34 | ||
| BDFS43 | K9301 | 83.00 | 84.00 | 1.00 | MGW | 0.13 | 0.29 | ||
| BDFS43 | K9302 | 84.00 | 85.25 | 1.25 | MGW | 0.16 | 0.35 | ||
| BDFS43 | K9303 | 85.25 | 86.00 | 0.75 | Peg | 0.03 | 0.07 | ||
| BDFS43 | K9304 | 86.00 | 87.00 | 1.00 | Peg | 0.04 | 0.09 | ||
| BDFS43 | K9305 | 87.00 | 87.70 | 0.70 | Peg | 0.04 | 0.10 | ||
| BDFS43 | K9306 | 87.70 | 89.00 | 1.30 | Peg+Thin MGW(10cm) | 0.12 | 0.26 | ||
| BDFS43 | K9307 | 89.00 | 90.00 | 1.00 | Peg+Thin MGW(17cm) | 0.09 | 0.19 | ||
| BDFS43 | K9308 | 90.00 | 91.34 | 1.34 | Peg+Thin MGW(05cm) | 0.11 | 0.23 | ||
| BDFS43 | K9309 | 91.34 | 92.11 | 0.77 | Peg | 0.02 | 0.03 | ||
| BDFS43 | K9310 | 92.11 | 93.00 | 0.89 | MGW | 0.11 | 0.24 | ||
| BDFS43 | K9311 | 93.00 | 94.00 | 1.00 | MGW | 0.08 | 0.18 | ||
| BDFS43 | K9312 | 94.00 | 94.95 | 0.95 | Peg+Thin MGW(05cm) | 0.08 | 0.17 | ||
| BDFS43 | K9313 | 94.95 | 95.53 | 0.58 | Peg | 0.01 | 0.02 | ||
| BDFS43 | K9314 | 95.53 | 96.53 | 1.00 | MGW | 0.07 | 0.15 | ||
| BDFS43 | NS | 96.53 | 120.00 | 23.47 | |||||
| BDFS43 | K9315 | 120.00 | 121.00 | 1.00 | MGW | 0.03 | 0.06 | ||
| BDFS43 | K9316 | 121.00 | 121.34 | 0.34 | Peg | 0.00 | 0.01 | ||
| BDFS43 | K9317 | 121.34 | 122.34 | 1.00 | MGW | 0.03 | 0.06 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | Interval (m) | LITH | Li % | Li2O% | Weighted Li2O% | Interval (m) |
| BDFS44 | K9318 | 81.64 | 82.64 | 1.00 | MGW | 0.08 | 0.16 | ||
| BDFS44 | K9321 | 82.64 | 83.19 | 0.55 | Peg | 0.01 | 0.03 | ||
| BDFS44 | K9322 | 83.19 | 84.00 | 0.81 | Shale/MGW | 0.06 | 0.13 | ||
| BDFS44 | K9323 | 84.00 | 85.00 | 1.00 | Shale | 0.07 | 0.14 | ||
| BDFS44 | K9324 | 85.00 | 86.00 | 1.00 | MGW | 0.05 | 0.10 | ||
| BDFS44 | K9325 | 86.00 | 87.00 | 1.00 | MGW | 0.05 | 0.12 | ||
| BDFS44 | K9326 | 87.00 | 88.00 | 1.00 | MGW | 0.06 | 0.12 | ||
| BDFS44 | K9327 | 88.00 | 89.00 | 1.00 | MGW | 0.06 | 0.13 | ||
| BDFS44 | K9328 | 89.00 | 90.00 | 1.00 | MGW | 0.08 | 0.17 | ||
| BDFS44 | K9329 | 90.00 | 91.00 | 1.00 | Shale | 0.08 | 0.17 | ||
| BDFS44 | K9331 | 91.00 | 92.00 | 1.00 | Shale/MGW | 0.09 | 0.19 |
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| BDFS44 | K9332 | 92.00 | 93.00 | 1.00 | MGW | 0.11 | 0.24 | ||
|---|---|---|---|---|---|---|---|---|---|
| BDFS44 | K9333 | 93.00 | 94.30 | 1.30 | MGW | 0.16 | 0.35 | ||
| BDFS44 | K9334 | 94.30 | 95.00 | 0.70 | Peg | 0.08 | 0.18 | ||
| BDFS44 | K9335 | 95.00 | 96.08 | 1.08 | Peg | 0.03 | 0.07 | ||
| BDFS44 | K9336 | 96.08 | 97.00 | 0.92 | MGW+Peg(8cm) | 0.12 | 0.25 | ||
| BDFS44 | K9337 | 97.00 | 98.00 | 1.00 | MGW | 0.09 | 0.19 | ||
| BDFS44 | K9338 | 98.00 | 99.00 | 1.00 | MGW | 0.10 | 0.22 | ||
| BDFS44 | K9341 | 99.00 | 100.00 | 1.00 | MGW | 0.10 | 0.22 | ||
| BDFS44 | K9342 | 100.00 | 101.20 | 1.20 | MGW | 0.11 | 0.23 | ||
| BDFS44 | K9343 | 101.20 | 101.80 | 0.60 | Peg | 0.02 | 0.05 | ||
| BDFS44 | K9344 | 101.80 | 102.80 | 1.00 | MGW | 0.05 | 0.11 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | Interval (m) | LITH | Li % | Li2O% | Weighted Li2O% | Interval (m) |
| BDFS45 | K9345 | 81.20 | 82.20 | 1.00 | MGW+int(7cm) | 0.12 | 0.26 | ||
| BDFS45 | K9346 | 82.20 | 83.00 | 0.80 | Peg | 0.62 | 1.32 | 1.95 | 7.80 |
| BDFS45 | K9347 | 83.00 | 84.00 | 1.00 | Peg | 1.06 | 2.28 | ||
| BDFS45 | K9348 | 84.00 | 85.00 | 1.00 | Peg | 0.91 | 1.96 | ||
| BDFS45 | K9349 | 85.00 | 86.00 | 1.00 | Peg | 0.81 | 1.75 | ||
| BDFS45 | K9350 | 86.00 | 87.00 | 1.00 | Peg | 1.28 | 2.75 | ||
| BDFS45 | K9351 | 87.00 | 88.00 | 1.00 | Peg | 0.81 | 1.74 | ||
| BDFS45 | K9352 | 88.00 | 89.00 | 1.00 | Peg | 1.15 | 2.48 | ||
| BDFS45 | K9353 | 89.00 | 90.00 | 1.00 | Peg | 0.54 | 1.16 | ||
| BDFS45 | K9354 | 90.00 | 91.00 | 1.00 | MGW | 0.24 | 0.52 | ||
| BDFS45 | K9355 | 91.00 | 92.00 | 1.00 | MGW+thin Peg(16cm) | 0.09 | 0.20 | ||
| BDFS45 | K9356 | 92.00 | 93.18 | 1.18 | MGW | 0.09 | 0.20 | ||
| BDFS45 | K9357 | 93.18 | 94.00 | 0.82 | Peg | 0.07 | 0.15 | ||
| BDFS45 | K9358 | 94.00 | 95.00 | 1.00 | Peg | 0.12 | 0.26 | ||
| BDFS45 | K9361 | 95.00 | 96.00 | 1.00 | Peg | 0.09 | 0.19 | ||
| BDFS45 | K9362 | 96.00 | 97.00 | 1.00 | Peg | 0.10 | 0.22 | ||
| BDFS45 | K9363 | 97.00 | 98.00 | 1.00 | Peg | 0.10 | 0.22 | ||
| BDFS45 | K9364 | 98.00 | 99.00 | 1.00 | Peg | 0.09 | 0.20 | ||
| BDFS45 | K9365 | 99.00 | 100.00 | 1.00 | Peg | 0.04 | 0.09 | ||
| BDFS45 | K9366 | 100.00 | 100.90 | 0.90 | Peg | 0.06 | 0.12 | ||
| BDFS45 | K9367 | 100.90 | 101.90 | 1.00 | MGW+thin Peg(8cm) | 0.14 | 0.30 | ||
| BDFS45 | NS | 101.90 | 133.74 | 31.84 | |||||
| BDFS45 | K9368 | 133.74 | 134.05 | 0.31 | Peg | 0.01 | 0.02 | ||
| BDFS45 | NS | 134.05 | 149.00 | 14.95 | |||||
| BDFS45 | K9369 | 149.00 | 150.00 | 1.00 | MGW | 0.02 | 0.04 | ||
| BDFS45 | K9371 | 150.00 | 151.00 | 1.00 | MGW+Qv(texture peg) | 0.01 | 0.03 | ||
| BDFS45 | K9372 | 151.00 | 152.00 | 1.00 | MGW+Qv(texture peg) | 0.01 | 0.03 | ||
| BDFS45 | K9373 | 152.00 | 153.00 | 1.00 | MGW+Qv(texture peg) | 0.02 | 0.03 | ||
| BDFS45 | K9374 | 153.00 | 154.00 | 1.00 | MGW+Qv(texture peg) | 0.02 | 0.04 | ||
| BDFS45 | K9375 | 154.00 | 155.00 | 1.00 | MGW | 0.02 | 0.04 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | Interval (m) | LITH | Li % | Li2O% | Weighted Li2O% | Interval (m) |
| BDFS46 | K9376 | 39.00 | 40.00 | 1.00 | Sap of schist | 0.09 | 0.20 | ||
| BDFS46 | K9377 | 40.00 | 40.50 | 0.50 | Sap of Peg | 0.04 | 0.08 | ||
| BDFS46 | K9378 | 40.50 | 41.50 | 1.00 | Sap of schist | 0.04 | 0.08 | ||
| BDFS46 | K9381 | 41.50 | 42.50 | 1.00 | Sap of schist, sap of peg (10cm) | 0.03 | 0.06 | ||
| BDFS46 | K9382 | 42.50 | 43.00 | 0.50 | Sap of schist | 0.03 | 0.07 | ||
| BDFS46 | K9383 | 43.00 | 44.00 | 1.00 | Sap of Peg | 0.03 | 0.07 |
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| BDFS46 | K9384 | 44.00 | 45.00 | 1.00 | Peg | 0.08 | 0.17 | ||
|---|---|---|---|---|---|---|---|---|---|
| BDFS46 | K9385 | 45.00 | 46.00 | 1.00 | Peg | 0.12 | 0.27 | ||
| BDFS46 | K9386 | 46.00 | 47.00 | 1.00 | Peg | 0.91 | 1.95 | 1.65 | 12.27 |
| BDFS46 | K9387 | 47.00 | 48.00 | 1.00 | Peg | 0.81 | 1.75 | ||
| BDFS46 | K9388 | 48.00 | 49.00 | 1.00 | Peg | 0.87 | 1.87 | ||
| BDFS46 | K9389 | 49.00 | 50.00 | 1.00 | Peg | 0.94 | 2.02 | ||
| BDFS46 | K9390 | 50.00 | 51.00 | 1.00 | Peg | 0.54 | 1.16 | ||
| BDFS46 | K9391 | 51.00 | 52.00 | 1.00 | Peg | 0.85 | 1.84 | ||
| BDFS46 | K9392 | 52.00 | 53.00 | 1.00 | Peg | 0.80 | 1.73 | ||
| BDFS46 | K9393 | 53.00 | 54.00 | 1.00 | Peg | 1.12 | 2.42 | ||
| BDFS46 | K9394 | 54.00 | 54.65 | 0.65 | Peg | 0.38 | 0.81 | ||
| BDFS46 | K9395 | 54.65 | 55.00 | 0.35 | Mica schist | 0.29 | 0.63 | ||
| BDFS46 | K9396 | 55.00 | 56.00 | 1.00 | Peg | 0.57 | 1.24 | ||
| BDFS46 | K9397 | 56.00 | 57.00 | 1.00 | Peg | 0.84 | 1.81 | ||
| BDFS46 | K9398 | 57.00 | 57.85 | 0.85 | Peg | 0.79 | 1.70 | ||
| BDFS46 | K9401 | 57.85 | 58.27 | 0.42 | Mica schist | 0.28 | 0.59 | ||
| BDFS46 | K9402 | 58.27 | 59.44 | 1.17 | Peg | 0.03 | 0.06 | ||
| BDFS46 | K9403 | 59.44 | 60.44 | 1.00 | Mica schist | 0.17 | 0.36 | ||
| BDFS46 | NS | 60.44 | 100.29 | 39.85 | |||||
| BDFS46 | K9404 | 100.29 | 100.84 | 0.55 | Peg+thin MGW(13cm) | 0.02 | 0.03 | ||
| BDFS46 | NS | 100.84 | 128.50 | 27.66 | |||||
| BDFS46 | K9405 | 128.50 | 129.50 | 1.00 | MGW | 0.08 | 0.17 | ||
| BDFS46 | K9406 | 129.50 | 130.00 | 0.50 | Peg + vein of MGW | 0.04 | 0.08 | ||
| BDFS46 | K9407 | 130.00 | 131.00 | 1.00 | Peg | 0.05 | 0.10 | ||
| BDFS46 | K9408 | 131.00 | 132.00 | 1.00 | Peg | 0.02 | 0.04 | ||
| BDFS46 | K9409 | 132.00 | 133.00 | 1.00 | Peg | 0.03 | 0.07 | ||
| BDFS46 | K9410 | 133.00 | 134.00 | 1.00 | Peg | 0.06 | 0.12 | ||
| BDFS46 | K9411 | 134.00 | 134.69 | 0.69 | Peg | 0.03 | 0.07 | ||
| BDFS46 | K9412 | 134.69 | 136.00 | 1.31 | MGW+thin peg (8cm) | 0.09 | 0.19 | ||
| BDFS46 | K9413 | 136.00 | 137.00 | 1.00 | MGW | 0.08 | 0.18 | ||
| BDFS46 | K9414 | 137.00 | 138.13 | 1.13 | MGW | 0.09 | 0.20 | ||
| BDFS46 | K9415 | 138.13 | 139.36 | 1.23 | Peg | 0.01 | 0.02 | ||
| BDFS46 | K9416 | 139.36 | 139.64 | 0.28 | MGW | 0.11 | 0.24 | ||
| BDFS46 | K9417 | 139.64 | 140.00 | 0.36 | Peg | 0.02 | 0.04 | ||
| BDFS46 | K9418 | 140.00 | 141.00 | 1.00 | Peg | 0.03 | 0.07 | ||
| BDFS46 | K9421 | 141.00 | 142.00 | 1.00 | Peg | 0.02 | 0.05 | ||
| BDFS46 | K9422 | 142.00 | 143.00 | 1.00 | Peg | 0.03 | 0.06 | ||
| BDFS46 | K9423 | 143.00 | 144.00 | 1.00 | Peg | 0.03 | 0.07 | ||
| BDFS46 | K9424 | 144.00 | 145.00 | 1.00 | Peg | 0.02 | 0.04 | ||
| BDFS46 | K9425 | 145.00 | 146.00 | 1.00 | Peg | 0.02 | 0.05 | ||
| BDFS46 | K9426 | 146.00 | 147.00 | 1.00 | Peg | 0.02 | 0.05 | ||
| BDFS46 | K9427 | 147.00 | 148.00 | 1.00 | Peg | 0.04 | 0.09 | ||
| BDFS46 | K9428 | 148.00 | 149.00 | 1.00 | Peg | 0.03 | 0.07 | ||
| BDFS46 | K9429 | 149.00 | 150.00 | 1.00 | Peg | 0.03 | 0.06 | ||
| BDFS46 | K9431 | 150.00 | 150.53 | 0.53 | Peg | 0.03 | 0.06 | ||
| BDFS46 | K9432 | 150.53 | 151.53 | 1.00 | MGW | 0.10 | 0.23 |
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Table 2: Sampling, analytical results and weighted intersections from Second Series diamond tails BRCD16 to BRCD33, with results shown from the diamond drilled portions of the holes (RC portion of holes, collar information and pegmatite intersections previously reported - ASX:FL1 Announcement 22/08/2024 – License renewals in progress, series two drilling analytical results identify very high Li2O within the main pegmatite at Blakala).
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
|---|---|---|---|---|---|---|---|---|
| BRCD16 | K10374 | 137.25 | 138.25 | Sch | 0.19 | 0.41 | ||
| BRCD16 | K10375 | 138.25 | 139.25 | Sch | 0.28 | 0.60 | ||
| BRCD16 | K10376 | 139.25 | 140.25 | Peg | 0.06 | 0.13 | ||
| BRCD16 | K10377 | 140.25 | 141.25 | Peg | 0.09 | 0.20 | ||
| BRCD16 | K10378 | 141.25 | 142.10 | Peg | 0.18 | 0.38 | ||
| BRCD16 | K10381 | 142.10 | 142.60 | Sch | 0.36 | 0.78 | ||
| BRCD16 | K10382 | 142.60 | 143.10 | Peg | 0.08 | 0.17 | ||
| BRCD16 | K10383 | 143.10 | 143.52 | Sch | 0.36 | 0.78 | ||
| BRCD16 | K10384 | 143.52 | 144.00 | Peg | 0.05 | 0.12 | ||
| BRCD16 | K10385 | 144.00 | 145.00 | Sch | 0.74 | 1.58 | 1.29 | 4.00 |
| BRCD16 | K10386 | 145.00 | 146.00 | Peg | 0.95 | 2.05 | ||
| BRCD16 | K10387 | 146.00 | 147.00 | Peg | 0.38 | 0.83 | ||
| BRCD16 | K10388 | 147.00 | 148.00 | Peg | 0.32 | 0.69 | ||
| BRCD16 | K10389 | 148.00 | 149.00 | Peg | 0.12 | 0.27 | ||
| BRCD16 | K10390 | 149.00 | 149.43 | Peg | 0.02 | 0.04 | ||
| BRCD16 | K10391 | 149.43 | 150.43 | Sch | 0.14 | 0.31 | ||
| BRCD16 | K10392 | 150.43 | 151.43 | Sch | 0.17 | 0.36 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
| BRCD17 | K10393 | 99.00 | 100.00 | Peg | 0.64 | 1.38 | 1.44 | 11.00 |
| BRCD17 | K10394 | 100.00 | 101.00 | Peg | 0.75 | 1.62 | ||
| BRCD17 | K10395 | 101.00 | 102.00 | Peg | 0.40 | 0.86 | ||
| BRCD17 | K10396 | 102.00 | 103.00 | Peg | 0.43 | 0.92 | ||
| BRCD17 | K10397 | 103.00 | 104.00 | Peg | 0.36 | 0.77 | ||
| BRCD17 | K10398 | 104.00 | 105.00 | Peg | 0.78 | 1.67 | ||
| BRCD17 | K10401 | 105.00 | 106.00 | Peg | 0.91 | 1.96 | ||
| BRCD17 | K10402 | 106.00 | 107.00 | Peg | 0.78 | 1.67 | ||
| BRCD17 | K10403 | 107.00 | 108.00 | Peg | 0.92 | 1.97 | ||
| BRCD17 | K10404 | 108.00 | 109.00 | Peg | 0.73 | 1.57 | ||
| BRCD17 | K10405 | 109.00 | 110.00 | Peg | 0.69 | 1.48 | ||
| BRCD17 | K10406 | 110.00 | 110.48 | Peg | 0.02 | 0.05 | ||
| BRCD17 | K10407 | 110.48 | 111.48 | Sch | 0.14 | 0.30 | ||
| BRCD17 | K10408 | 111.48 | 112.48 | Sch | 0.14 | 0.31 | ||
| BRCD17 | NS | 112.48 | 117.45 | |||||
| BRCD17 | K10409 | 117.45 | 118.45 | Sch | 0.08 | 0.18 | ||
| BRCD17 | K10410 | 118.45 | 119.02 | Peg | 0.02 | 0.05 | ||
| BRCD17 | K10411 | 119.02 | 120.02 | Sch | 0.11 | 0.23 |
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| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
|---|---|---|---|---|---|---|---|---|
| BRCD18 | K10412 | 117.00 | 118.00 | Peg | 0.71 | 1.52 | 1.62 | 9.00 |
| BRCD18 | K10413 | 118.00 | 119.00 | Peg | 0.87 | 1.87 | ||
| BRCD18 | K10414 | 119.00 | 120.00 | Peg | 0.79 | 1.70 | ||
| BRCD18 | K10415 | 120.00 | 121.00 | Peg | 0.65 | 1.39 | ||
| BRCD18 | K10416 | 121.00 | 122.00 | Peg | 0.63 | 1.36 | ||
| BRCD18 | K10417 | 122.00 | 123.00 | Peg | 0.55 | 1.19 | ||
| BRCD18 | K10418 | 123.00 | 124.00 | Peg | 0.92 | 1.98 | ||
| BRCD18 | K10421 | 124.00 | 125.00 | Peg | 1.06 | 2.29 | ||
| BRCD18 | K10422 | 125.00 | 126.00 | Peg | 0.58 | 1.25 | ||
| BRCD18 | K10423 | 126.00 | 126.60 | Peg | 0.03 | 0.07 | ||
| BRCD18 | K10424 | 126.60 | 127.60 | Sch | 0.12 | 0.25 | ||
| BRCD18 | K10425 | 127.60 | 128.60 | Sch | 0.06 | 0.13 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
| BRCD19 | K10426 | 117.00 | 117.30 | Peg+Sch(10cm) | 0.24 | 0.52 | 0.52 | 0.30 |
| BRCD19 | K10427 | 117.30 | 118.41 | Sch | 0.18 | 0.39 | ||
| BRCD19 | K10428 | 118.41 | 119.00 | Peg | 0.60 | 1.29 | 1.51 | 28.59 |
| BRCD19 | K10429 | 119.00 | 120.00 | Peg | 0.96 | 2.06 | ||
| BRCD19 | K10431 | 120.00 | 120.40 | Peg | 0.49 | 1.05 | ||
| BRCD19 | K10432 | 120.40 | 121.04 | Sch | 0.33 | 0.71 | ||
| BRCD19 | K10433 | 121.04 | 122.00 | Peg | 0.53 | 1.14 | ||
| BRCD19 | K10434 | 122.00 | 123.00 | Peg | 1.02 | 2.20 | ||
| BRCD19 | K10435 | 123.00 | 124.00 | Peg | 0.98 | 2.11 | ||
| BRCD19 | K10436 | 124.00 | 125.00 | Peg | 0.93 | 2.00 | ||
| BRCD19 | K10437 | 125.00 | 126.00 | Peg | 0.68 | 1.46 | ||
| BRCD19 | K10438 | 126.00 | 127.00 | Peg | 0.71 | 1.53 | ||
| BRCD19 | K10441 | 127.00 | 128.00 | Peg | 0.83 | 1.78 | ||
| BRCD19 | K10442 | 128.00 | 129.00 | Peg | 0.75 | 1.61 | ||
| BRCD19 | K10443 | 129.00 | 130.00 | Peg | 0.92 | 1.99 | ||
| BRCD19 | K10444 | 130.00 | 131.00 | Peg | 0.70 | 1.51 | ||
| BRCD19 | K10445 | 131.00 | 132.00 | Peg | 0.74 | 1.59 | ||
| BRCD19 | K10446 | 132.00 | 133.00 | Peg | 0.55 | 1.18 | ||
| BRCD19 | K10447 | 133.00 | 134.00 | Peg | 0.60 | 1.30 | ||
| BRCD19 | K10448 | 134.00 | 135.00 | Peg | 0.24 | 0.51 | ||
| BRCD19 | K10449 | 135.00 | 136.00 | Peg | 0.21 | 0.46 | ||
| BRCD19 | K10450 | 136.00 | 137.00 | Peg | 0.25 | 0.54 | ||
| BRCD19 | K10451 | 137.00 | 138.00 | Peg | 0.47 | 1.00 | ||
| BRCD19 | K10452 | 138.00 | 139.00 | Peg | 0.70 | 1.50 | ||
| BRCD19 | K10453 | 139.00 | 140.00 | Peg | 0.61 | 1.31 | ||
| BRCD19 | K10454 | 140.00 | 141.00 | Peg | 0.80 | 1.71 | ||
| BRCD19 | K10455 | 141.00 | 142.00 | Peg | 0.82 | 1.76 | ||
| BRCD19 | K10456 | 142.00 | 143.00 | Peg | 0.69 | 1.48 |
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| BRCD19 | K10457 | 143.00 | 144.00 | Peg | 0.83 | 1.79 | ||
|---|---|---|---|---|---|---|---|---|
| BRCD19 | K10458 | 144.00 | 145.00 | Peg | 0.98 | 2.10 | ||
| BRCD19 | K10461 | 145.00 | 146.00 | Peg | 1.03 | 2.22 | ||
| BRCD19 | K10462 | 146.00 | 147.00 | Peg | 0.85 | 1.84 | ||
| BRCD19 | K10463 | 147.00 | 148.00 | Peg | 0.21 | 0.45 | ||
| BRCD19 | K10464 | 148.00 | 149.00 | Thinpeg+Sch | 0.09 | 0.20 | ||
| BRCD19 | K10465 | 149.00 | 150.00 | Sch | 0.06 | 0.13 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
| BRCD20 | K10466 | 131.00 | 132.00 | Sch | 0.07 | 0.16 | ||
| BRCD20 | K10467 | 132.00 | 133.00 | Sch | 0.08 | 0.17 | ||
| BRCD20 | K10468 | 133.00 | 134.00 | Peg | 0.66 | 1.43 | 1.31 | 9.00 |
| BRCD20 | K10469 | 134.00 | 135.00 | Peg | 0.98 | 2.11 | ||
| BRCD20 | K10471 | 135.00 | 136.00 | Peg | 0.73 | 1.58 | ||
| BRCD20 | K10472 | 136.00 | 137.00 | Peg | 0.58 | 1.24 | ||
| BRCD20 | K10473 | 137.00 | 138.00 | Peg | 0.58 | 1.25 | ||
| BRCD20 | K10474 | 138.00 | 139.00 | Peg | 0.34 | 0.73 | ||
| BRCD20 | K10475 | 139.00 | 140.00 | Peg | 0.59 | 1.27 | ||
| BRCD20 | K10476 | 140.00 | 140.52 | Sch | 0.31 | 0.66 | ||
| BRCD20 | K10477 | 140.52 | 141.00 | Peg | 0.39 | 0.83 | ||
| BRCD20 | K10478 | 141.00 | 142.00 | Peg | 0.68 | 1.45 | ||
| BRCD20 | K10481 | 142.00 | 143.00 | Peg | 0.04 | 0.08 | ||
| BRCD20 | K10482 | 143.00 | 144.00 | Sch | 0.11 | 0.24 | ||
| BRCD20 | K10483 | 144.00 | 145.00 | Sch | 0.07 | 0.16 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
| BRCD21 | K10484 | 129.00 | 130.00 | Peg | 0.88 | 1.89 | 1.53 | 24.00 |
| BRCD21 | K10485 | 130.00 | 131.00 | Peg | 0.45 | 0.97 | ||
| BRCD21 | K10486 | 131.00 | 132.00 | Thin sch +peg | 0.39 | 0.85 | ||
| BRCD21 | K10487 | 132.00 | 133.00 | Peg | 0.30 | 0.64 | ||
| BRCD21 | K10488 | 133.00 | 133.82 | Peg | 0.85 | 1.83 | ||
| BRCD21 | K10489 | 133.82 | 134.28 | Sch | 0.41 | 0.89 | ||
| BRCD21 | K10490 | 134.28 | 135.00 | Peg | 0.43 | 0.92 | ||
| BRCD21 | K10491 | 135.00 | 136.00 | Peg | 0.85 | 1.83 | ||
| BRCD21 | K10492 | 136.00 | 137.00 | Peg | 0.87 | 1.87 | ||
| BRCD21 | K10493 | 137.00 | 138.00 | Peg | 0.91 | 1.96 | ||
| BRCD21 | K10494 | 138.00 | 139.00 | Peg | 0.90 | 1.93 | ||
| BRCD21 | K10495 | 139.00 | 140.00 | Peg | 0.93 | 2.01 | ||
| BRCD21 | K10496 | 140.00 | 141.00 | Peg | 0.63 | 1.35 | ||
| BRCD21 | K10497 | 141.00 | 142.00 | Peg | 0.83 | 1.78 | ||
| BRCD21 | K10498 | 142.00 | 143.00 | Peg | 0.80 | 1.72 | ||
| BRCD21 | K12001 | 143.00 | 144.00 | Peg | 0.43 | 0.92 | ||
| BRCD21 | K12002 | 144.00 | 145.00 | Peg | 0.99 | 2.13 | ||
| BRCD21 | K12003 | 145.00 | 146.00 | Peg | 0.92 | 1.98 |
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| BRCD21 | K12004 | 146.00 | 147.00 | Peg | 0.81 | 1.75 | ||
|---|---|---|---|---|---|---|---|---|
| BRCD21 | K12005 | 147.00 | 148.00 | Peg | 0.48 | 1.03 | ||
| BRCD21 | K12006 | 148.00 | 149.00 | Peg | 0.78 | 1.69 | ||
| BRCD21 | K12007 | 149.00 | 150.00 | Peg | 0.70 | 1.51 | ||
| BRCD21 | K12008 | 150.00 | 151.00 | Peg | 0.77 | 1.66 | ||
| BRCD21 | K12009 | 151.00 | 152.00 | Peg | 0.89 | 1.91 | ||
| BRCD21 | K12010 | 152.00 | 153.00 | Peg | 0.36 | 0.77 | ||
| BRCD21 | K12011 | 153.00 | 154.00 | Peg | 0.12 | 0.27 | ||
| BRCD21 | K12012 | 154.00 | 154.33 | Peg | 0.09 | 0.20 | ||
| BRCD21 | K12013 | 154.33 | 155.33 | Sch | 0.09 | 0.20 | ||
| BRCD21 | K12014 | 155.33 | 156.33 | Sch | 0.06 | 0.13 | ||
| BRCD21 | K12015 | 156.33 | 157.33 | Sch | 0.05 | 0.12 | ||
| BRCD21 | K12016 | 157.33 | 158.44 | Peg+Sch | 0.03 | 0.06 | ||
| BRCD21 | K12017 | 158.44 | 159.00 | Sch | 0.04 | 0.09 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
| BRCD22 | K12018 | 63.00 | 64.00 | Peg | 0.06 | 0.12 | ||
| BRCD22 | K12021 | 64.00 | 64.30 | Peg | 0.02 | 0.04 | ||
| BRCD22 | K12022 | 64.30 | 65.00 | Sch | 0.13 | 0.29 | ||
| BRCD22 | K12023 | 65.00 | 66.00 | Sch | 0.12 | 0.27 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
| BRCD25 | K12024 | 137.00 | 138.00 | Sch | 0.12 | 0.25 | ||
| BRCD25 | K12025 | 138.00 | 139.11 | Sch | 0.20 | 0.43 | ||
| BRCD25 | K12026 | 139.11 | 140.00 | Peg | 0.41 | 0.88 | 1.77 | 8.34 |
| BRCD25 | K12027 | 140.00 | 141.00 | Peg | 0.97 | 2.09 | ||
| BRCD25 | K12028 | 141.00 | 142.00 | Peg | 0.40 | 0.86 | ||
| BRCD25 | K12029 | 142.00 | 143.00 | Peg | 0.92 | 1.98 | ||
| BRCD25 | K12031 | 143.00 | 144.00 | Peg | 0.88 | 1.90 | ||
| BRCD25 | K12032 | 144.00 | 145.00 | Peg | 0.83 | 1.80 | ||
| BRCD25 | K12033 | 145.00 | 146.00 | Peg | 1.05 | 2.27 | ||
| BRCD25 | K12034 | 146.00 | 147.00 | Peg | 0.91 | 1.96 | ||
| BRCD25 | K12035 | 147.00 | 147.45 | Peg | 1.15 | 2.48 | ||
| BRCD25 | K12036 | 147.45 | 148.00 | Peg(silicified) | 0.03 | 0.07 | ||
| BRCD25 | K12037 | 148.00 | 149.00 | Sch | 0.15 | 0.32 | ||
| BRCD25 | K12038 | 149.00 | 150.00 | Sch | 0.19 | 0.41 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
| BRCD28 | K12041 | 111.00 | 112.25 | Peg | 0.11 | 0.24 | ||
| BRCD28 | K12042 | 112.25 | 113.00 | Peg | 0.40 | 0.86 | 1.52 | 3.75 |
| BRCD28 | K12043 | 113.00 | 114.00 | Peg | 0.69 | 1.48 | ||
| BRCD28 | K12044 | 114.00 | 115.00 | Peg | 1.02 | 2.20 | ||
| BRCD28 | K12045 | 115.00 | 116.00 | Peg | 0.64 | 1.38 | ||
| BRCD28 | K12046 | 116.00 | 117.00 | Sch | 0.11 | 0.23 | ||
| BRCD28 | K12047 | 117.00 | 118.00 | Sch | 0.08 | 0.17 |
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| BRCD28 | K12048 | 126.00 | 127.00 | Sch | 0.09 | 0.20 | ||
|---|---|---|---|---|---|---|---|---|
| BRCD28 | K12049 | 127.00 | 128.00 | Sch | 0.13 | 0.28 | ||
| BRCD28 | K12050 | 128.00 | 129.26 | Sch | 0.26 | 0.56 | ||
| BRCD28 | K12051 | 129.26 | 130.00 | Peg | 0.02 | 0.05 | ||
| BRCD28 | K12052 | 130.00 | 131.00 | Peg | 0.67 | 1.45 | 1.68 | 25.64 |
| BRCD28 | K12053 | 131.00 | 132.00 | Peg | 0.97 | 2.09 | ||
| BRCD28 | K12054 | 132.00 | 133.00 | Peg | 0.73 | 1.57 | ||
| BRCD28 | K12055 | 133.00 | 134.00 | Peg | 0.63 | 1.36 | ||
| BRCD28 | K12056 | 134.00 | 135.00 | Peg | 0.71 | 1.53 | ||
| BRCD28 | K12057 | 135.00 | 136.00 | Peg | 0.64 | 1.38 | ||
| BRCD28 | K12058 | 136.00 | 137.00 | Peg | 0.64 | 1.37 | ||
| BRCD28 | K12061 | 137.00 | 138.00 | Peg | 0.47 | 1.02 | ||
| BRCD28 | K12062 | 138.00 | 139.00 | Peg | 1.03 | 2.21 | ||
| BRCD28 | K12063 | 139.00 | 140.00 | Peg | 0.76 | 1.64 | ||
| BRCD28 | K12064 | 140.00 | 141.00 | Peg | 0.82 | 1.76 | ||
| BRCD28 | K12065 | 141.00 | 142.00 | Peg | 0.66 | 1.42 | ||
| BRCD28 | K12066 | 142.00 | 143.00 | Peg | 0.79 | 1.71 | ||
| BRCD28 | K12067 | 143.00 | 144.00 | Peg | 0.88 | 1.89 | ||
| BRCD28 | K12068 | 144.00 | 145.00 | Peg | 0.78 | 1.68 | ||
| BRCD28 | K12069 | 145.00 | 146.00 | Peg | 0.50 | 1.08 | ||
| BRCD28 | K12071 | 146.00 | 147.00 | Peg | 1.09 | 2.35 | ||
| BRCD28 | K12072 | 147.00 | 148.00 | Peg | 1.04 | 2.24 | ||
| BRCD28 | K12073 | 148.00 | 149.00 | Peg | 0.99 | 2.14 | ||
| BRCD28 | K12074 | 149.00 | 150.00 | Peg | 0.73 | 1.56 | ||
| BRCD28 | K12075 | 150.00 | 151.00 | Peg | 0.85 | 1.83 | ||
| BRCD28 | K12076 | 151.00 | 152.00 | Peg | 0.94 | 2.03 | ||
| BRCD28 | K12077 | 152.00 | 153.00 | Peg | 0.68 | 1.47 | ||
| BRCD28 | K12078 | 153.00 | 154.00 | Peg | 0.68 | 1.47 | ||
| BRCD28 | K12081 | 154.00 | 155.00 | Peg | 0.77 | 1.65 | ||
| BRCD28 | K12082 | 155.00 | 155.64 | Peg | 0.82 | 1.77 | ||
| BRCD28 | K12083 | 155.64 | 156.40 | Peg | 0.16 | 0.35 | ||
| BRCD28 | K12084 | 156.40 | 157.00 | Sch | 0.13 | 0.28 | ||
| BRCD28 | K12085 | 157.00 | 158.00 | Sch | 0.13 | 0.28 | ||
| BRCD28 | K12086 | 158.00 | 159.00 | Sch | 0.11 | 0.23 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
| BRCD30 | K12087 | 75.00 | 76.00 | Peg | 0.24 | 0.53 | ||
| BRCD30 | K12088 | 76.00 | 77.00 | Peg | 0.78 | 1.68 | 1.51 | 3.00 |
| BRCD30 | K12089 | 77.00 | 78.00 | Peg | 0.81 | 1.74 | ||
| BRCD30 | K12090 | 78.00 | 79.00 | Peg | 0.51 | 1.10 | ||
| BRCD30 | K12091 | 79.00 | 80.00 | Peg | 0.09 | 0.20 | ||
| BRCD30 | K12092 | 80.00 | 81.00 | Peg | 0.10 | 0.21 | ||
| BRCD30 | K12093 | 81.00 | 82.00 | Peg | 0.54 | 1.17 | 1.17 | 1.00 |
| BRCD30 | K12094 | 82.00 | 83.00 | Peg | 0.06 | 0.13 |
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| BRCD30 | K12095 | 83.00 | 84.00 | Peg | 0.13 | 0.28 | ||
|---|---|---|---|---|---|---|---|---|
| BRCD30 | K12096 | 84.00 | 85.00 | Peg | 0.05 | 0.11 | ||
| BRCD30 | K12097 | 85.00 | 86.00 | Peg | 0.27 | 0.57 | ||
| BRCD30 | K12098 | 86.00 | 87.00 | Peg | 0.22 | 0.47 | ||
| BRCD30 | K12101 | 87.00 | 88.00 | Peg | 0.32 | 0.69 | ||
| BRCD30 | K12102 | 88.00 | 89.00 | Peg | 0.09 | 0.20 | ||
| BRCD30 | K12103 | 89.00 | 90.00 | Peg | 0.14 | 0.29 | ||
| BRCD30 | K12104 | 90.00 | 91.00 | Peg | 0.07 | 0.15 | ||
| BRCD30 | K12105 | 91.00 | 92.00 | Peg | 0.10 | 0.22 | ||
| BRCD30 | K12106 | 92.00 | 93.00 | Peg | 0.09 | 0.20 | ||
| BRCD30 | K12107 | 93.00 | 94.00 | Peg | 0.14 | 0.30 | ||
| BRCD30 | K12108 | 94.00 | 95.00 | Peg | 0.38 | 0.82 | ||
| BRCD30 | K12109 | 95.00 | 96.00 | Peg | 0.62 | 1.34 | 1.40 | 2.00 |
| BRCD30 | K12110 | 96.00 | 97.00 | Peg | 0.68 | 1.47 | ||
| BRCD30 | K12111 | 97.00 | 98.13 | Peg | 0.16 | 0.34 | ||
| BRCD30 | K12112 | 98.13 | 99.00 | Sch | 0.12 | 0.25 | ||
| BRCD30 | K12113 | 99.00 | 100.00 | Sch | 0.11 | 0.24 | ||
| BRCD30 | NS | 100.00 | 181.62 | |||||
| BRCD30 | K12114 | 181.62 | 182.62 | Sch | 0.12 | 0.26 | ||
| BRCD30 | K12115 | 182.62 | 183.05 | Peg | 0.32 | 0.69 | ||
| BRCD30 | K12116 | 183.05 | 184.05 | Peg | 0.55 | 1.19 | 1.19 | 1.00 |
| BRCD30 | K12117 | 184.05 | 185.05 | Peg | 0.22 | 0.47 | ||
| BRCD30 | K12118 | 185.05 | 186.05 | Peg | 0.13 | 0.29 | ||
| BRCD30 | NS | 186.05 | 199.50 | |||||
| BRCD30 | K12121 | 199.50 | 200.50 | Sch | 0.11 | 0.25 | ||
| BRCD30 | K12122 | 200.50 | 201.21 | Peg | 0.03 | 0.06 | ||
| BRCD30 | K12123 | 201.21 | 202.21 | Sch | 0.12 | 0.27 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
| BRCD32 | K12124 | 69.00 | 70.00 | Peg | 0.68 | 1.46 | 1.72 | 7.00 |
| BRCD32 | K12125 | 70.00 | 71.00 | Peg | 0.74 | 1.59 | ||
| BRCD32 | K12126 | 71.00 | 72.00 | Peg | 0.91 | 1.96 | ||
| BRCD32 | K12127 | 72.00 | 73.00 | Peg | 0.99 | 2.14 | ||
| BRCD32 | K12128 | 73.00 | 74.00 | Peg | 0.74 | 1.59 | ||
| BRCD32 | K12129 | 74.00 | 75.00 | Peg | 0.69 | 1.48 | ||
| BRCD32 | K12131 | 75.00 | 76.00 | Peg | 0.83 | 1.79 | ||
| BRCD32 | K12132 | 76.00 | 76.90 | Peg | 0.20 | 0.43 | ||
| BRCD32 | K12133 | 76.90 | 77.26 | Peg | 0.03 | 0.05 | ||
| BRCD32 | K12134 | 77.26 | 78.26 | Sch | 0.17 | 0.36 | ||
| BRCD32 | NS | 78.26 | 110.00 | |||||
| BRCD32 | K12135 | 110.00 | 111.00 | Sch | 0.32 | 0.69 | ||
| BRCD32 | K12136 | 111.00 | 111.73 | Sch+Peg | 0.08 | 0.17 | ||
| BRCD32 | K12137 | 111.73 | 112.20 | Peg | 0.01 | 0.03 | ||
| BRCD32 | K12138 | 112.20 | 113.00 | Peg | 0.02 | 0.05 |
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| BRCD32 | K12141 | 113.00 | 114.00 | Peg | 0.02 | 0.03 | ||
|---|---|---|---|---|---|---|---|---|
| BRCD32 | K12142 | 114.00 | 115.00 | Peg | 0.04 | 0.10 | ||
| BRCD32 | K12143 | 115.00 | 116.00 | Peg | 0.03 | 0.06 | ||
| BRCD32 | K12144 | 116.00 | 117.00 | Peg | 0.08 | 0.17 | ||
| BRCD32 | K12145 | 117.00 | 118.00 | Peg | 0.03 | 0.06 | ||
| BRCD32 | K12146 | 118.00 | 118.30 | Peg | 0.02 | 0.04 | ||
| BRCD32 | K12147 | 118.30 | 119.34 | Qtz vein | 0.02 | 0.05 | ||
| BRCD32 | K12148 | 119.34 | 119.64 | Peg | 0.69 | 1.49 | 1.49 | 0.30 |
| BRCD32 | K12149 | 119.64 | 120.30 | Qtz vein | 0.01 | 0.02 | ||
| BRCD32 | K12150 | 120.30 | 121.14 | Peg | 0.04 | 0.09 | ||
| BRCD32 | K12151 | 121.14 | 121.62 | Qtz vein | 0.01 | 0.03 | ||
| BRCD32 | K12152 | 121.62 | 122.62 | Peg | 0.02 | 0.04 | ||
| BRCD32 | K12153 | 122.62 | 123.00 | Qtz vein +Peg | 0.07 | 0.15 | ||
| BRCD32 | K12154 | 123.00 | 123.33 | Peg | 0.14 | 0.30 | ||
| BRCD32 | K12155 | 123.33 | 124.00 | Sch+Peg | 0.05 | 0.10 | ||
| BRCD32 | K12156 | 124.00 | 124.86 | Sch | 0.24 | 0.51 | ||
| BRCD32 | K12157 | 124.86 | 125.35 | Peg | 0.06 | 0.12 | ||
| BRCD32 | K12158 | 125.35 | 126.00 | Peg | 0.20 | 0.43 | ||
| BRCD32 | K12161 | 126.00 | 127.00 | Peg | 0.04 | 0.09 | ||
| BRCD32 | K12162 | 127.00 | 127.45 | Peg | 0.03 | 0.07 | ||
| BRCD32 | K12163 | 127.45 | 127.83 | Sch+Qtz | 0.06 | 0.13 | ||
| BRCD32 | K12164 | 127.83 | 128.75 | Peg | 0.04 | 0.09 | ||
| BRCD32 | K12165 | 128.75 | 130.00 | Sch | 0.13 | 0.29 | ||
| BRCD32 | K12166 | 130.00 | 131.00 | Sch | 0.12 | 0.27 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
| BRCD34 | K12167 | 152.41 | 153.41 | Sch | 0.14 | 0.31 | ||
| BRCD34 | K12168 | 153.41 | 154.00 | Peg | 0.05 | 0.10 | ||
| BRCD34 | K12169 | 154.00 | 155.00 | Peg | 0.03 | 0.07 | ||
| BRCD34 | K12171 | 155.00 | 156.00 | Peg | 0.06 | 0.13 | ||
| BRCD34 | K12172 | 156.00 | 157.00 | Peg | 0.06 | 0.13 | ||
| BRCD34 | K12173 | 157.00 | 158.00 | Peg | 0.10 | 0.21 | ||
| BRCD34 | K12174 | 158.00 | 159.00 | Peg | 0.26 | 0.56 | ||
| BRCD34 | K12175 | 159.00 | 160.00 | Peg | 0.07 | 0.15 | ||
| BRCD34 | K12176 | 160.00 | 161.00 | Peg | 0.09 | 0.20 | ||
| BRCD34 | K12177 | 161.00 | 162.00 | Peg | 0.36 | 0.77 | ||
| BRCD34 | K12178 | 162.00 | 163.00 | Peg | 1.13 | 2.43 | 1.67 | 6.00 |
| BRCD34 | K12181 | 163.00 | 163.42 | Peg | 1.60 | 3.44 | ||
| BRCD34 | K12182 | 163.42 | 164.26 | Sch | 0.32 | 0.69 | ||
| BRCD34 | K12183 | 164.26 | 165.00 | Peg | 0.39 | 0.83 | ||
| BRCD34 | K12184 | 165.00 | 166.00 | Peg | 0.73 | 1.56 | ||
| BRCD34 | K12185 | 166.00 | 167.00 | Peg | 0.87 | 1.87 | ||
| BRCD34 | K12186 | 167.00 | 168.00 | Peg | 0.71 | 1.53 | ||
| BRCD34 | K12187 | 168.00 | 168.30 | Peg | 0.06 | 0.13 |
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| BRCD34 | K12188 | 168.30 | 169.00 | Sch | 0.12 | 0.26 | ||
|---|---|---|---|---|---|---|---|---|
| BRCD34 | K12189 | 169.00 | 170.00 | Sch | 0.09 | 0.20 | ||
| BHID | SAMP ID | FROM (m) | TO (m) | LITH | Li % | Li2O% | Weighted Li2O% |
Interval (m) |
| BRCD36 | K12190 | 96.00 | 97.00 | Peg | 0.68 | 1.46 | 1.23 | 15.00 |
| BRCD36 | K12191 | 97.00 | 98.00 | Peg | 0.50 | 1.08 | ||
| BRCD36 | K12192 | 98.00 | 99.00 | Peg | 0.54 | 1.15 | ||
| BRCD36 | K12193 | 99.00 | 100.00 | Peg | 0.35 | 0.74 | ||
| BRCD36 | K12194 | 100.00 | 101.00 | Peg | 0.51 | 1.10 | ||
| BRCD36 | K12195 | 101.00 | 102.00 | Peg | 0.20 | 0.42 | ||
| BRCD36 | K12196 | 102.00 | 103.00 | Peg | 0.66 | 1.41 | ||
| BRCD36 | K12197 | 103.00 | 104.00 | Peg | 0.28 | 0.60 | ||
| BRCD36 | K12198 | 104.00 | 105.00 | Peg | 0.10 | 0.21 | ||
| BRCD36 | K12201 | 105.00 | 106.00 | Peg | 0.62 | 1.34 | ||
| BRCD36 | K12202 | 106.00 | 107.00 | Peg | 0.63 | 1.35 | ||
| BRCD36 | K12203 | 107.00 | 108.00 | Peg | 0.87 | 1.87 | ||
| BRCD36 | K12204 | 108.00 | 109.00 | Peg | 1.06 | 2.29 | ||
| BRCD36 | K12205 | 109.00 | 110.00 | Peg | 0.99 | 2.13 | ||
| BRCD36 | K12206 | 110.00 | 111.00 | Peg | 0.75 | 1.61 | ||
| BRCD36 | K12207 | 111.00 | 111.90 | Peg | 0.09 | 0.19 | ||
| BRCD36 | K12208 | 111.90 | 113.00 | Sch | 0.16 | 0.33 | ||
| BRCD36 | K12209 | 113.00 | 114.00 | Sch | 0.11 | 0.23 | ||
| BRCD36 | NS | 114.00 | 239.76 | |||||
| BRCD36 | K12210 | 239.76 | 240.76 | Sch | 0.14 | 0.31 | ||
| BRCD36 | K12211 | 240.76 | 241.14 | Peg | 0.03 | 0.05 | ||
| BRCD36 | K12212 | 241.14 | 242.06 | Peg | 0.04 | 0.09 | ||
| BRCD36 | K12213 | 242.06 | 243.00 | Sch | 0.28 | 0.60 | ||
| BRCD36 | NS | 243.00 | 270.31 | |||||
| BRCD36 | K12214 | 270.31 | 271.31 | Sch | 0.14 | 0.31 | ||
| BRCD36 | K12215 | 271.31 | 272.00 | Peg | 0.28 | 0.61 | ||
| BRCD36 | K12216 | 272.00 | 273.00 | Peg | 0.24 | 0.51 | ||
| BRCD36 | K12217 | 273.00 | 274.00 | Peg | 0.38 | 0.83 | 1.24 | 3.00 |
| BRCD36 | K12218 | 274.00 | 275.00 | Peg | 0.53 | 1.14 | ||
| BRCD36 | K12221 | 275.00 | 276.00 | Peg | 0.81 | 1.75 | ||
| BRCD36 | K12222 | 276.00 | 276.85 | Peg | 0.30 | 0.65 | ||
| BRCD36 | K12223 | 276.85 | 278.00 | Peg | 0.20 | 0.42 | ||
| BRCD36 | K12224 | 278.00 | 279.00 | Sch | 0.15 | 0.33 |
- Li% to Li₂O% conversion of 2.153 used
** Missing holes were not sampled
*** NS no sample taken in unmineralized material
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Figure 2: Section showing the previously reported results (black on white) for First Series BDFS25 on the Eastern Pegmatite; and Second Series BRCD18 intersecting the Eastern Pegmatite at depth, with the new results (red on yellow) from the diamond drilling portion of BRCD18.
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Figure 3: Section showing the previously reported results (black on white) for First Series BDFS38 on the southern extension of the Main Pegmatite; and Second Series BRCD25 intersecting the Main Pegmatite at depth, with the new results (red on yellow) from the diamond drilling portion of BRCD25.
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Figure 4: Section showing the previously reported results (black on white) for First Series BDFS17 on the Western Pegmatite; and Second Series BRCD28 intersecting the Western Pegmatite at depth, with the new results (red on yellow) from the diamond drilling portion of BRCD28.
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ABOUT FIRST LITHIUM
First Lithium (ASX code: FL1) is at the forefront of lithium exploration and sustainable development, focusing on pioneering projects like Blakala and Faraba in Mali. Our management team has significant in-country experience and specialist advisors with extensive lithium exploration and government relations expertise.
Our commitment goes beyond the pursuit of lithium riches; it’s about powering tomorrow responsibly. We recognise the global demand for lithium and are dedicated to positively impacting local communities while ensuring environmentally sensitive practices.
Ends-
The Board of Directors of First Lithium Ltd authorised this announcement to be given to the ASX.
Further information contact:
Venkatesh Padala Managing Director
T: +61 8 9481 0389 E: [email protected]
Competent Persons Statement
Except where indicated, exploration results above have been reviewed and compiled by Mr Kobus Badenhorst, a Competent Person who is a Member of SACNASP and the South African Geological Society (GSSA), with over 26 years of experience in metallic and energy mineral exploration and development, and as such has sufficient experience which is relevant to the style of mineralisation and type of deposits under consideration as a Competent Person as defined in the 2012 Edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”. Mr Badenhorst is the Managing Director of GeoActiv Dynamic Geological Services and consents to the inclusion of this technical information in the format and context in which it appears.
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Forward-Looking Statements
This announcement contains forward-looking statements which are identified by words such as ‘may’, ‘could’, ‘believes’, ‘estimates’, ‘targets’, ‘expects’, or ‘intends’ and other similar words that involve risks and uncertainties.
These statements are based on an assessment of present economic and operating conditions, and on a number of assumptions regarding future events and actions that, as at the date of this announcement, are expected to take place.
Such forward-looking statements are not guarantees of future performance and involve known and unknown risks, uncertainties, assumptions and other important factors, many of which are beyond the control of the Company, the Directors and the Company’s management.
The Company cannot and does not give any assurance that the results, performance or achievements expressed or implied by the forward-looking statements contained in this announcement will actually occur, and investors are cautioned not to place undue reliance on these forward-looking statements.
The Company has no intention to update or revise forward-looking statements, or to publish prospective financial information in the future, regardless of whether new information, future events or any other factors affect the information contained in this announcement, except where required by law.
These forward-looking statements are subject to various risk factors that could cause the Company’s actual results to differ materially from the results expressed or anticipated in these statements.
FIRST LITHIUM LIMITED ACN 009 081 770
Level 8, London House CONTACT: 216 St. Georges Terrace Venkatesh Padala Perth Western Australia 6000 Managing Director Tel: +61 (08) 9481 0389 Tel: +61 8 9481 0389 Facsimile: +61 (08) 9463 6103 [email protected] http://firstlithium.com.au
DIRECTORS
Lee Christensen Venkatesh Padala Jason Ferris Andrew Law CODE: ASX: FL1
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Appendix 1
JORC Code, 2012 Edition – Table 1
Section 1 Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections.)
| Criteria JORC Code explanation Commentary |
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. • • • • • • • • • • • |
Diamond drilling at Blakala Diamond drilling of HQ and NQ2 core size holes was used to obtain core for sampling and analysis. Previously reported 39 First Series diamond holes, now reporting the last 7 holes, BDFS40 to BDFS46. Previously reporting the first 15 of 42 diamond drill tails to the RC precollars of the Second Series BRCD, now reporting from holes 16 to 28 drilled on mainly the Eastern Pegmatite body, 3 holes on the Main Pegmatite body and 1 hole on the Western Pegmatite body to intersect the pegmatite at approximately 50 to 100m under the surface. All logging and sampling took place according to detailed diamond Standard Procedure documents. The core was first accurately fitted to the orientation line (bottom of hole) of the orientated core accurately drawn with a permanent paint marker; logging took place using the orientation line, and sampling was then marked on the retention portion of the core. Sampling done as ½ core sampling. Diamond drilling for the current program is completed, with a total of 8368.10m of diamond drilling completed. Reverse Circulation (RC) drilling at Blakala RC precollars, with diamond drilling tails, drilled to intersect the Western, Main and Eastern Pegmatite bodies at depth below the First Series diamond holes. RC sampling done at the drill rig of all intersected pegmatites. All logging and sampling took place according to detailed RC Standard Procedure documents. RC precollar drilling for the current program is completed, with a total of 3,838m of RC drilling completed. |
1
| Criteria JORC Code explanation Commentary |
Criteria JORC Code explanation Commentary |
|---|---|
| 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). • • • • • • • |
Diamond drilling at Blakala Diamond wireline drillholes of HQ and NQ2 core size completed of a planned 6,000m drilling program at Blakala Prospect. The drill core was downhole orientated using the electronic REFLEX ACT III tool; a core orientation line was marked for all geological and sampling depth information. Diamond drilling is considered a standard industry drilling technique for vein or pegmatite deposits. The drilling rig used was a YS1500 with a Cummins QSB 6.7 engine. Diamond drill rods used were 3m long. The holes are inclined at -50°. The drilling onsite is governed by a Daimond Drilling Guideline to ensure consistency in application of the method between geologists and drillers. Reverse Circulation (RC) drilling at Blakala RC drilling rig has the following specifications: oHydco-3 RC truck mounted, 8 x 4; oCummins 610hp hydraulic / compressor engine; o350psi / 900cfm compressor (rig mounted); oTop head drive, variable speed control, Low Gear – 8,600Nm/75rpm,HighGear, 300Nm/150rpm; |
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| Criteria JORC Code explanation Commentary |
Criteria JORC Code explanation Commentary |
|---|---|
o10.3m fully welded RHS lattice mast; o22mm nonrotating wire ropes with hydraulic tensioners; oPull-out 23,000kg – Pulldown 15,000kg; oDrill hole diameter 121 mm. |
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| 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. • • • • • • |
Diamond drilling at Blakala Diamond drill sample recovery is monitored by measuring and recording the total core recovery on a drill run basis for the entire hole. Core recovery data is entered into the project drillhole database. RQD data is collected and core recoveries and associated RQD % for runs studied, where 100% recovery not obtained. Very good recovery and generally solid core was found in the drillholes. Reverse Circulation (RC) drilling at Blakala The pegmatite mineralisation is found in mostly dark coloured altered sediment country rock (not granite) and therefore easily identifiable in the RC for logging and sampling. The recovery is determined by weighing the full weight of every meter of sample drilled. |
| 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. • Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. • The total length and percentage of the relevant intersections logged. • • • • • • • |
Diamond drilling at Blakala Core logging took place only after careful fitting of all core, followed by the orientation of the core from the Reflex orientation data, followed by core recovery and RQD data collection. This work took place at the drill rig. Initial geological logging took place at the drill rig, followed by detailed and appropriate lithological, structural and weathering logging at the core shed that took place on the full core using the orientation line for interval measurements. All logging data is entered into the project drillhole database. All core was photographed before and after sampling. Reverse Circulation (RC) drilling at Blakala Logging took place at the drill rig. Small heaps of samples from each 1m intersection are placed on the ground to assist with logging of colour etc. Detailed logging is done on washed chips, with the chips then placed in reference chip boxes. |
| Sub-sampling techniques • 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. • • |
Diamond drilling at Blakala Sampling takes place according to a sampling protocol document. HQ andNQ size corewas ½ core sampled by a core cutter. |
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| Criteria JORC Code explanation Commentary |
Criteria JORC Code explanation Commentary |
|---|---|
| and sample preparation • 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. • • • • • • • |
All pegmatite intersections were sampled, as well as all thin schist bands within the pegmatites. Sampling is done lithologically, to a minimum sample length of 30cm and an average size of 1.00m. The sampling interval is seen as representative. Bulk Density via wet-dry Archimedes technique has been completed for all core. Reverse Circulation (RC) drilling at Blakala Sampling takes place according to a sampling protocol document. Samples are collected at the cyclone at 1m intervals and sampling is then done on all pegmatite intersections on 1m interval basis. Hangingwall and footwall schist sampling also takes place. |
| 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. • • • • • • • |
Samples sent to the analytical laboratory (SGS in Johannesburg, South Africa), with assay results for diamond drillholes BDFS40 to BDFS46 and diamond tails to the RC precollars BDRC16 to BDRC36 received, all the precollar RC results already reported. Analyses was via Na2O2 Fusion, HNO3, ICPAES. This is seen as an appropriate analytical technique with the suite of 27 elements covered. SGS is an accredited analytical laboratory. 31 AMIS reference standards (AMIS0603, AMIS0524 and AMIS0682 were used), 31 AMIS chip blanks and 11 pulp Duplicates were inserted by FL1 and analysed as part of this batch of results. SGS added internal standards (OREAS906 and AMIS0355), as well as repeat analyses. Good correlation was found from the QC samples in the results reported here. Inter-laboratory QC testing of c 5% of the total amount of samples was performed by ALS Ireland. A very good correlation with QC samples was found with the ALS results (internal ALS and blind introduced QC samples) and a good correlation with the SGS results was found. |
| 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. • • • |
On site logging took place with experienced geologists, and a senior company geologist checking all the logging being undertaken by detailed logging. The geological field data is manually transcribed into a master Microsoft Excel spreadsheet which is appropriate for this stage in the exploration program. Theraw field datais checkedintheMicrosoftExcel formatfirst to |
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| Criteria | JORC Code explanation | Commentary | |
|---|---|---|---|
| identify any obvious errors or outlier data. The data is then imported | |||
| into a Microsoft Access database where it is subjected to various | |||
| validation queries. | |||
| Location | of | •Accuracy and quality of surveys used to locate drill holes (collar and |
•Drillhole locations were recorded using a hand-held GPS, collars were |
| data points | down-hole surveys), trenches, mine workings and other locations used | then surveyed via DGPS. |
|
| in Mineral Resource estimation. | •Down-hole verticality surveys are done on all holes by multishot survey. | ||
| •Specification of the grid system used. | •A Digital Terrain Model (DTM) via a drone survey has been conducted | ||
| •Quality and adequacy of topographic control. | on the project. | ||
| Data spacing | • Data spacing for reporting of Exploration Results. |
•Drilling took place in phases, with First Series diamond holes drilled | |
| and | close to the outcrop of the main Western, Main and Eastern Pegmatite | ||
| distribution | •Whether the data spacing and distribution is sufficient to establish the | bodies to intersect the pegmatites at approximately between 30m and |
|
| degree of geological and grade continuity appropriate for the Mineral | 70m below surface. |
||
| Resource and Ore Reserve estimation procedure(s) and classifications | •Second Series holes of RC precollars, with diamond drilling tails, drilled |
||
| applied. •Whether sample compositing has been applied_._ |
to intersect the Western, Main and Eastern Pegmatite bodies at depth below the First Series holes. |
||
| Orientation | of | •Whether the orientation of sampling achieves unbiased sampling of |
•Intersection thicknesses are reported incorporating deeper |
| data | in | possible structures and the extent to which this is known, considering |
intersections of the pegmatites confirming dip and thickness. |
| relation | to | the deposit type. |
|
| geological | •If the relationship between the drilling orientation and the orientation of | ||
| structure | key mineralised structures is considered to have introduced a sampling | ||
| bias, this should be assessed and reported if material. |
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Section 2 Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this section.)
| Criteria | Criteria | JORC Code explanation | Commentary |
|---|---|---|---|
| Mineral | • Type, reference name/number, location and ownership including | •Permits for the Mali Lithium project are in their first renewal period |
|
| tenement and | agreements or material issues with third parties such as joint ventures, |
granted by the original Mali decree “Order No. 2022-0276/MMEE-SG” |
|
| land | tenure | partnerships, overriding royalties, native title interests, historical sites, |
(Blakala Prospect permit) and “Order No. 2022-0275/MMEE-SG” |
| status | wilderness or national park and environmental settings. | (Gouna permit). Both permits are valid for the exploration of Group 3 | |
| • The security of the tenure held at the time of reporting along with any | elements (Li, Co, Cr, Nb, Ni, PGE, REE, Sn, Ta, Ti, V, W and Zr) and |
||
| known impediments to obtaining a licence to operate in the area. | are considered early stage Li exploration projects. | ||
| •On Mali's online repository, the Faraba permit is valid from March 16, | |||
| 2021 to March 16, 2024, and the Gouna permit is valid from May 15, | |||
| 2021 to May 15, 2024. | |||
| Exploration | • Acknowledgment and appraisal of exploration by other parties. | •Historic exploration work was completed by Russian geologists during | |
| done by other | 1963-64. Geological prospecting was carried out in the central part of | ||
| parties | the Bougouni pegmatite field. | ||
| •The Company has obtained the digital data in relation to this historic | |||
| information. | |||
| •The historic results have not been reported. | |||
| Geology | • Deposit type, geological setting and style of mineralisation. | ||
| •Blakala prospect in the Gouna licence is Palaeo-Proterozoic in age. | |||
| The regional lithological assemblages comprise of felsic intrusives | |||
| such as granite, granodiorites, and schists of variable composition and | |||
| laterite. The schists have a metasedimentary origin with coarse grains | |||
| of quartz and mica, which have been subjected to multiple | |||
| deformations to form schists. | |||
| •The pegmatites are a pale greyish-white colour, fresh hand specimen | |||
| shows a whitish-earthy matrix of feldspar with phenocrysts of | |||
| spodumene, quartz and muscovite. The pegmatites have a varied | |||
| width from a few centimeters to up to 45 meters where the two separate | |||
| pegmatite bands merge together. | |||
| Drill | hole | • A summary of all information material to the understanding of the |
•Summary drill hole information has previously been reported. |
| Information | exploration results including a tabulation of the following information for | ||
| all Material drill holes: | |||
o easting and northing of the drill hole collar |
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o elevation or RL (Reduced Level – elevation above sea level in |
|||
| metres) of the drill hole collar |
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| Criteria | JORC Code explanation | Commentary | |
|---|---|---|---|
o dip and azimuth of the hole |
|||
o down hole length and interception depth |
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o hole length. |
|||
| • If the exclusion of this information is justified on the basis that the | |||
| information is not Material and this exclusion does not detract from the | |||
| understanding of the report, the Competent Person should clearly | |||
| _explain why this is the case. _ | |||
| Data | • In reporting Exploration Results, weighting averaging techniques, | • No upper or lower grade cut-offs have been used. |
|
| aggregation methods |
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. |
• The pegmatites in the drillhole intersections are mineralised throughout in the results received, no low grade or very low grade areas were aggregated in the intercepts. • Intercepts are weighted and shown in Table 1 of the main body, all outcrop sampling results are shown in the table. |
|
| • The assumptions used for any reporting of metal equivalent values | • The Li to Li₂O conversion of 2.153 has been used. |
||
| should be clearly stated. | |||
| Relationship | • These relationships are particularly important in the reporting of | •The pegmatites generally dip at -80° to the west at Blakala. The |
|
| between | Exploration Results. | diamond holes are drilled perpendicular to the general strike of the | |
| mineralisation | • If the geometry of the mineralisation with respect to the drill hole angle |
pegmatite bodies, at a dip of -50°. |
|
| widths | and | is known, its nature should be reported. |
•The pegmatites generally dip at -70° to the south-west. The diamond |
| intercept lengths |
• 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 |
holes are drilled perpendicular to the general strike of the pegmatite bodies, at a dip of -50°. |
|
| width not known’). | •Downhole widths are reported. | ||
| Diagrams | • Appropriate maps and sections (with scales) and tabulations of | •Figures are displayed in the main text. |
|
| 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. _ | |||
| Balanced | • Where comprehensive reporting of all Exploration Results is not | •All results are reported, with all Li results shown in the body of the |
|
| reporting | practicable, representative reporting of both low and high grades | Announcement in Table 1. |
|
| and/or widths should be practiced to avoid misleading reporting of | •Full analytical results shown in Appendix 1. |
||
| Exploration Results. |
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| Criteria JORC Code explanation Commentary |
Criteria JORC Code explanation Commentary |
|---|---|
| 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. • |
No other material exploration information has been gathered by the Company. |
| 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 highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive. • • • • |
Blakala Prospect All planned First and Second Series holes have been completed on the Western, Eastern and Main Pegmatite Bodies. Now waiting for receipt of all analytical results. Metallurgical testwork currently taking place. 3D modelling, JORC compliant mineral resource modelling estimate and reporting in progress. |
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