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CHARIOT RESOURCES LTD Capital/Financing Update 2024

Feb 1, 2024

64615_rns_2024-02-01_c924f83e-2d08-4101-8c4d-c0c867257d5f.pdf

Capital/Financing Update

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ASX ANNOUNCEMENT

2 February 2024

intersections in Wyoming; and Base Metals (Cu, Zn and Pb) potential identified

HIGHLIGHTS:

  • Black Mountain maiden drill program delivers strong initial hard rock lithium results with multiple mineralised lithium intersections from first three (3) holes

  • the potential of the Black Mountain LCT pegmatite swarms

  • BMDDH23_01 15.48m @ 1.12% Li2O and 79ppm Ta2O5 from 2.74m, including 4.27m @ 2.46% Li2O and 128 ppm Ta2O5 from 9.94m

  • BMDDH23_02 14.33m @ 0.84% Li2O and 61ppm Ta2O5 from 1.83m, including 2.29m @ 3.09% Li2O and 138ppm Ta2O5 from 10.67m

  • BMDDH23_03 18.81m @ 0.85% Li2O and 98ppm Ta2O5 from 45.26m, including 5.79m @ 1.08% Li2O and 105ppm Ta2O5 from 47.55m

  • High-grade potential with individual grades downhole of up to 3.79% Li2O and 230ppm Ta2O5

  • Drilling continues with eight (8) holes having been completed to date, assay results for the subsequent five (5) holes are pending and expected to be announced by April 2024

  • BDDDH23_01 intersected a zone of stockwork vein and disseminated pyrite-pyrrhotite mineralisation over an interval of approximately 100m within the biotite schist

  • The Company is optimistic it may have intersected the peripheral portion of a potentially larger base metal mineral system, with selected intervals grading up to 0.6% (6,012ppm) Cu, 1.0% (9,931ppm) Zn and 15.4% (154,412ppm) Pb

  • The Company plans to extend the soil sampling program and run preliminary IP lines over the base metals anomaly in Q3 2024

Chariot Corporation Limited (“ Chariot ” or the “ Company ”) is pleased to advise that it has intersected significant zones of strong lithium-tantalum mineralisation in the first three (3) holes (“ First Three Holes ”) of the maiden drill program at the Black Mountain Project (“ Black Mountain ”), in Wyoming, U.S.A.

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li thium c aesium t antalum (“ LCT ”) pegmatite swarms with the assays returning individual lithium and tantalum values of up to 3.79% Li2O (BMDDH23_01-0021) and 230ppm Ta2O5 (BMDDH23_01-0033).

Wyoming Lithium Pty Ltd (“ WLPL ”) and Panther Lithium Corporation (“ PLC” ) co-founder[1] , Dr Edward Max Baker[2] commented:

“We’ve got stunning initial results in the midst of the North American winter. The targeted hard rock lithium system has been intersected in multiple holes, but we need to come back in the North American summer for a 5,000 – 10,000m drill program to get a better handle of the resource potential. The base-metals sulfide mineralisation is also very promising and indicates the potential for base metals and/or gold mineralisation, separate from the lithium mineralisation.”

First Three Holes: Drill Results

The First Three Holes (being drill holes BMDDH23_01 to BMDDH23_03) have been completed and assayed with the results summarised in Table 1 (see also Figure 1). A total of eight (8) holes have been drilled to date. The assay results for the subsequent five (5) drill holes are pending and expected to be announced by the end of April 2024.

Mountain LCT pegmatites (see Table 1), as indicated by the surface rock chip sampling results which were disclosed in the Company’s initial public offering prospectus and the Company’s announcement dated 9 November 2023.

Dill Hl F T Itl LiO% **TO **
r oe rom (m) o (m) nerva (m) **2 ** a25 ppm
BMDDH23_01 2.74 18.23 15.48 (14*) 1.12 78.8
including 4.15 5.49 1.34 1.91 68.0
and 9.94 14.2 4.27 2.46 128.4
BMDDH23_02 1.83 16.15 14.33 (13*) 0.84 61.3
including 10.67 12.95 2.29 3.09 137.7
BMDDH23_03
Includes 2.29m of core loss between
45.26m and 47.55m
45.26 62.73 18.81 (8*) 0.85 98.4
including 47.55 53.34 5.79 1.08 104.9

widths which are greater than true widths. * Denotes estimated true width.

1 Chariot holds a 93.9% interest in WLPL. PLC is a wholly owned subsidiary of WLPL.

2 Dr Baker holds 7,926,860 ordinary shares in Chariot (equal to a 5.3% interest in the undiluted shares on issue of Chariot). Dr Baker is also engaged as a consultant by Chariot.

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chariotcorporation.com ABN 13 637 559 847

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The visual inspection of the drill cores indicates that the high-grade lithium values are from intervals containing spodumene mineralisation, with no other lithium bearing mineral phases being visually identified to date.

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Northwest Area
Southeast Area
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Figure 1: Plan View of the Black Mountain Project, showing the pegmatite outcrops (dark red) and interpreted folded geometry (in light red) along with the Northwest and Southeast Cross-Section Lines and Drill Collars. The rock chip and soil geochemistry results are also shown. Refer to the Prospectus for the complete set of rock chip assay results[1] .

BMDDH23_01 and BMDDH23_02 were drilled from Pad 1 in the central Northwest swarm area (“ Northwest Area ”). BMDDH-23-01 hole was drilled to a depth of 177m at an azimuth of 260 degrees and a dip of -50 degrees (see Figure 2, Figure 3 and Figure 4 for selected photos of Drill Core). BMDDH23_02 hole was drilled to a total depth of 42m with the same azimuth BMDDH-23-01, but with a dip of -65 degrees (see Figure 1).

BMDDH23_01 and BMDDH23_02 both intersected the same pegmatite (see Figure 5).

1 The Prospectus can be downloaded from the Company website: www.chariotcorporation.com

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Figure 2: Pegmatite intersection in BMDDH23_01 from 10.5m (34.5ft.) to 13.7m (45ft.) showing some of the spodumene mineralisation.

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Figure 3: Drill Core sample from BMDDH23_01 – from 10.6m

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Figure 4: Pegmatite intersection in BMDDH23_02 from 9.6m (31.5ft.) to 14.5m (47.5ft.).

The BMDDH23_01 and BMDDH23_02 Drill Cores indicate that the Northwest Area comprise steeply dipping limbs of a tightly folded package of dikes, where the fold is now interpreted to be more open than initial anticipated before drilling, whereby the dikes to the west of drill pad 1 are expected to dip westward at a dip approximately parallel to BMDDH23_01 (See Figure 5).

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Figure 5: A – AA cross section (see Figure 1) through the Northwest Area showing BMDDH23_01 and BMDDH23__02 drill traces with the intersected pegmatite shown in red.

BMDDH23_03 was drilled in the central southeast swarm area (the “ Southeast Area ”) with an azimuth of 160° and dip of 50° to a depth of 78m. The pegmatite dike swarms in the Southeast Area comprise a complex fold-hinge, which based on the location of the intercept of pegmatite in BMDDH23_03 (see Figure 6) appears to dip moderately steeply to the southeast (see Figure 7).

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46.0m 47.5m 49.1m
50.9m
55.3m
56.3m
52.4m
50.0m
53.9m
61.4m
55.3m
63.4m
53.9m
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Figure 6: Pegmatite intersection in BMDDH23_03 from 45.3m (161ft.) to 63.4m (208ft.).

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Figure 7: B-BB cross section through the SouthEast Area showing BMDDH23_03 drill trace with the intersected pegmatite shown in red.

Independent Technical Guidance and Review of Exploration Results

ERM Australia Consultants Pty Ltd (previously CSA Global), ERM Sustainable Mining Services (“ CSA Global ”), have provided technical guidance for the development of the Black Mountain exploration plan and completed an independent review of the data, geological interpretations and exploration results pertaining to this announcement. CSA Global are satisfied these scientific and technical disclosures were appropriate to support the reporting of these Exploration Results.

Phase 1 Drill Program

The Phase 1 maiden drilling program (“ Phase 1 Drill Program ”) consisting of 10-15 holes was designed to test under outcropping pegmatite dikes swarms with anomalous Li rock chip values to determine the geometry of the dikes and to confirm the hard rock lithium potential ahead of a comprehensive resource drill-out in Q3 2024.

Major Drilling Group International Inc. (“ Major Drilling ”) has been contracted to drill oriented triple tube HQ sized diamond drill core (“ Drill Core ”) using a Boart Longyear LF90 Surface Diamond Core Drill Rig (the “ Drill Rig ”) (see Figure 8). Drill Core from Black Mountain is transported to Chariot’s core handling and storage facility in Jeffrey City, Wyoming, where each Drill Core is photographed, logged, and measured for density and recovery (see Figure 9). Drill Core samples are being assayed by American Assay Labs in Reno, Nevada.

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Figure 8: Drill Rig at Black Mountain.

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Figure 9: Chariot Senior Project Geologist, Willis Blakeslee, inspecting Drill Core.

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Exploration permitting in Wyoming on federal land is a two-step process. Approval from United States Bureau of Land Management in Wyoming (“ BLM ”) is required. At ‘Notice’ of Intent (“ NOI ”) levels of exploration (a basic level), a maximum disturbance of only five (5) acres is allowed and, if disturbance is likely to exceed this level, a more thorough Exploration Plan of Operations (“ EPO ”) must be submitted. An EPO, which typically requires biological and cultural/archaeological studies, can take 6- 12 months to complete, although there is then no restriction on the size of the disturbance.

The Phase 1 Program was limited to the currently permitted seven (7) drill pads due to the 5-acre limit on disturbance under the NOI, which applies to both access roads and the drill pads.

Chariot plans to apply for an EPO to increase the area of disturbance from 5-acres under the NOI to up to 2,500 acres for the Phase 2 Resource Drill Program commencing in Q3 2024.

The Phase 1 Drill Program was limited to testing the two central pegmatite swarms (of the four pegmatite swarms identified at Black Mountain), being the Northwest Area and the Southeast Area.

The upper section of BMDDH23_01 intersected pyrite-pyrrhotite mineralisation, occurring as veinlets and dissemination within the biotite schist over an interval of approximately 100m. At this early stage, only several select intervals of this mineralisation were sampled and assayed (see Table 2).

Based on the location of this drill hole relative to an 800m long by 150m wide zone of anomalous zincin-soils, the Company is optimistic that it has intersected the peripheral portion of a potentially larger base metal mineral system (see Figure 10). The zinc and lead anomalies are situated on the contact between metabasalt to the south and metasediments to the north coincident with a two-meter-wide zone of black massive chert outcrops along the southern margin of the soil anomaly. Based on the anomalous drill intercepts, the geological setting and the extent of the zinc and lead soil anomaly, the Company plans to further investigate this base metal mineralisation by extending the soil sampling program and conducting a preliminary induced polarisation survey (“ IP ”) lines across the anomaly in Q3 2024.

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Hole ID From
(m)
To
(m)
Interval
(m)
Cu
(ppm)
Pb
(ppm)
S
(ppm)
Zn
(ppm)
BMDDH23_01 23.4 23.8 0.3 6,012 0 150,328 1,294
BMDDH23_01 23.8 25 1.2 660 0 120,231 1,991
BMDDH23_01 32.5 32.9 0.3 1,258 0 129,887 3,958
BMDDH23_01 36.8 37.6 0.9 610 79 80,607 3,540
BMDDH23_01 39.2 39.7 0.5 479 46 71,688 3,829
BMDDH23_01 41.1 41.8 0.7 360 18 36,406 1,292
BMDDH23_01 42.7 43.1 0.4 777 34 110,999 3,778
BMDDH23_01 43.1 43.4 0.3 769 33 88,317 3,326
BMDDH23_01 44.9 45.5 0.6 671 30 86,750 3,640
BMDDH23_01 45.5 45.9 0.4 1,214 48 114,744 5,103
BMDDH23_01 47.2 47.5 0.3 1,222 76 119,702 3,017
BMDDH23_01 64 64.9 0.9 1,228 345 95,799 177
BMDDH23_01(a) 121 121.7 0.7 3,891 154,412a 28,970 9,931
Typical Assay Values in areas without
Pyrite Veins
Pegmatites
<30
<30
<200
<50
Schist
<500
<30
<1000
<200

Table 2: Intervals of vein and disseminated pyrite, pyrrhotite mineralisation from BMDDH23_01 showing Zn and Pb values several times higher than what appears to be background in this area. Note (a): Sample sent for re-assay due to exceptionally high Pb values. Refer to Appendix 3.

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Figure 10: Zone of anomalous Zinc in soils to the north of the pyrite-pyrrhotite mineralisation intersected in BMDDH23_01 (see Table 2) shown in relation to the outcropping pegmatites with soil sample locations showing Zn in ppm. Refer to Appendix 4 for the complete set of soil geochemistry results.

2024 Black Mountain Exploration Plans

The Phase 1 Program at Black Mountain is scheduled to continue through until 1 March 2024, with the objective of determining the three-dimensional shape and near-surface grades, down to 100m, within the three major pegmatite dike zones as shown in Figure 1 and Figure 10. In addition to the eight (8) holes already drilled, another seven holes are planned for the remainder of the Phase 1 Program, which will conclude on 1 March 2024.

drill program expected to commence in Q3 2024 (the “Phase 2 (Resource Drilling) Program ”).

Phase 2 (Resource Drilling) Program to Commence in Q3 2024

In anticipation of the Phase 2 Resource Drill Program, the initial focus will consist of detailed re-logging of the Phase 1 Program drill core along with a detailed petrographic study of the mineralisation and selection and submittal of samples for initial metallurgical testing. At the same time, the existing rock

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and base metal anomalies.

In addition, the Company plans to run a preliminary IP/Resistivity survey over the area of anomalous Zn-Pb soil geochemistry to assist in siting several holes to test the nature of this base metal mineralisation in Q3-Q4 2024 (see Figure 11).

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Figure 11: IP/Resistivity survey over anomalous Zn-Pb soil geochemistry.

The Company is currently in the process of lodging an application for an EPO (to drill) in order to expand the area of disturbance and increase the number of drill pads in preparation for a maiden resource drill-out. The Phase 2 (Resource Drill) Program is expected to commence in the North American summer in Q3 2024 or when the EPO is approved by the BLM. Refer to Figure 12 for an indicative exploration timeline for Black Mountain.

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Black Mountain Jan Feb Mar Apr May Jun Jul Aug Sep
Phase 1 Winter Drilling Program
Relog Phase 1 Core / Petrographic Study
Phase 1 Metallurgical Testing/ Study
Additional Rock Chip and Soil Geochemistry Survey
Phase 2 (Resource Drilling) Program
IP/Resistivity Program
Permitting - EPO

Figure 12: Indicative Black Mountain exploration timeline[1]

Authorised on behalf of the Board of Directors.

Shanthar Pathmanathan Managing Director Chariot Corporation Ltd

1 The above timeline is indicative only and subject to change based on factor within and outside of the Company’s control.

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Competent Person Statement - Exploration Results

Information in this announcement that relates to exploration results is based on information compiled by Dr E Max Baker who is a Geological Consultant to Chariot. Dr Baker is a Fellow of The Australian Institute of Mining and Metallurgy and has sufficient experience relevant to the style of mineralisation and type of deposit under consideration and to the activity that he is undertaking, to qualify as Competent Person as defined in the 2012 Edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves". Dr Baker consents to the inclusion in this announcement of the information pertaining to exploration results in the form and context in which it appears.

Dr Baker holds 7,926,860 ordinary shares in Chariot (equal to a 5.3% interest in the undiluted shares on issue of Chariot). Dr Baker is also engaged as a consultant by Chariot.

Important Notice

Statements in this announcement are made only as of the date of this announcement unless otherwise stated and the information in this announcement remains subject to change without notice.

corporate, their respective officers, directors, employees, advisors and agents or any other person accepts any liability as to or in relation to the accuracy or completeness of the information, statements, opinions or matters (express or implied) arising out of, contained in or derived from this announcement or any omission from this announcement or of any other written or oral information or opinions provided now or in the future to any person.

This announcement may contain some references to forecasts, estimates, assumptions and other forward-looking statements. Although the Company believes that its expectations, estimates and projected outcomes are based on reasonable assumptions, it can give no assurance that they will be achieved.

Cautionary Statement - Visual Estimates

This announcement contains references to visual results and visual estimates of mineralisation. The Company draws attention to uncertainty in reporting visual results. Visual estimates of mineral abundance should never be considered a proxy or substitute for laboratory analyses where concentrations or grades are the factor of principal economic interest. Visual estimates also potentially provide no information regarding impurities or deleterious physical properties relevant to valuations.

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About Chariot

Chariot Corporation Limited is a mineral exploration company focused on discovering and developing high-grade and near surface lithium opportunities in the United States. Chariot has twelve (12) lithium projects, including two core projects (the “ Core Projects ”) and a number of exploration pipeline projects which Chariot majority owns and operates. In addition, Chariot holds interests in a number of projects which have either been sold or conditionally divested through option agreements to publicly-listed companies (the “ Divested Projects ”).

lithium) in Wyoming, USA and the Resurgent Project (which is prospective for claystone lithium) in Nevada and Oregon, USA. Initial survey results from the Core Projects indicate high-grade lithium mineralisation at surface.

Chariot holds an interest in six exploration pipeline projects located in Wyoming, USA, including, the Copper Mountain Project, the South Pass Project and four other hard rock lithium projects.

Chariot holds an interest in the Lida and Amargosa projects in Nevada, USA which are prospective for claystone hosted lithium.

Chariot holds an interest in a hard rock lithium project in Zimbabwe which is prospective for spodumene bearing pegmatites and an early-stage hard rock lithium exploration project in Western Australia.

Each of the Divested Projects is operated or explored by Chariot’s publicly-listed counterparty under the relevant sale or option agreement and, depending upon the particular transaction, may generate additional revenues for Chariot dependent on the counterparty’s exploration success and financial wherewithal, the achievement of prescribed milestones, the mere effluxion of time or the production of saleable minerals payable under a net smelter royalty.

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ABN 13 637 559 847

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Appendix 1 – Drill Collar Table[1]

EAST
(m)
NORTH
(m)
RL
(mASL)
DDH No Azimuth Dip Depth
(m)
Assay Status
299884.9 4738509.2 2415.5 BMDDH23_01 260 -50 177.2 Assayed
299884.9 4738509.2 2415.5 BMDDH23_02 260 -65 42.4 Assayed
300193.2 4738176.0 2414.5 BMDDH23_03 160 -50 77.7 Assayed
300193.2 4738176.0 2414.5 BMDDH23_05 225 -45 158.2 Assays Pending
300193.2 4738176.0 2414.5 BMDDH23_06 225 -70 126.6 Assays Pending
300193.2 4738176.0 2414.5 BMDDH23_04 255 -50 69.5 Assays Pending
299785.7 4738489.5 2405.7 BMDDH23_09 290 -65 130 Assays Pending
299653.4 4738555.6 2365.0 BMDDH23_11 135 -40 200 Assays Pending

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1 All coordinates are in NAD83 Z13N

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Appendix 2 – Drill Assay Data

Hole_ID From
(m)
To (m) Interval
(m)
Cu
(ppm)
Fe
(ppm)
Li (ppm) Pb
(ppm)
S (ppm) Ta
(ppm)
Zn
(ppm)
BMDDH23_01 0.0 1.2 1.2 34 26902 589 <LoD 257 35.3 95
BMDDH23_01 1.2 2.4 1.2 27 16217 134 <LoD 476 66.7 100
BMDDH23_01 2.4 2.7 0.3 <LoD 4456 189 <LoD 258 19.4 24
BMDDH23_01 2.7 3.2 0.5 <LoD 20995 1323 <LoD 249 37.1 40
BMDDH23_01 3.2 4.0 0.7 <LoD 6790 3551 <LoD <LoD 41 51
BMDDH23_01 4.0 4.1 0.2 9 5225 148 <LoD <LoD 42.1 43
BMDDH23_01 4.1 4.7 0.5 <LoD 6303 7256 <LoD <LoD 41.3 23
BMDDH23_01 4.7 5.5 0.8 <LoD 7193 9969 <LoD <LoD 65.6 34
BMDDH23_01 5.5 5.9 0.4 <LoD 6229 3146 <LoD <LoD 50 40
BMDDH23_01 5.9 6.7 0.8 531 57694 355 <LoD 1712 9.1 119
BMDDH23_01 6.7 7.8 1.1 162 47846 200 <LoD 206 10.8 91
BMDDH23_01 7.8 9.5 1.7 204 86144 885 <LoD 268 2.1 211
BMDDH23_01 9.5 9.9 0.4 34 88335 1565 <LoD <LoD 1.2 142
BMDDH23_01 9.9 10.5 0.6 <LoD 6080 7497 <LoD <LoD 76.5 18
BMDDH23_01 10.5 11.0 0.5 <LoD 8447 14186 <LoD 238 88.3 33
BMDDH23_01 11.0 12.0 1.0 <LoD 7225 7555 <LoD 254 92.2 58
BMDDH23_01 12.0 12.7 0.7 <LoD 6806 9582 <LoD <LoD 168.2 39
BMDDH23_01 12.7 13.1 0.4 <LoD 9184 17383 <LoD <LoD 88.8 45
BMDDH23_01 13.1 13.7 0.6 <LoD 9397 17601 <LoD <LoD 128.2 29
BMDDH23_01 13.7 14.2 0.5 <LoD 7039 11153 <LoD <LoD 81.3 44
BMDDH23_01 14.2 14.7 0.5 <LoD 4525 4973 <LoD <LoD 134.7 13
BMDDH23_01 14.7 15.3 0.6 <LoD 3937 2226 <LoD <LoD 91.1 8
BMDDH23_01 15.3 16.0 0.7 <LoD 8459 9162 <LoD <LoD 74.7 51
BMDDH23_01 16.0 16.4 0.4 8 28882 1183 <LoD <LoD 53 106
BMDDH23_01 16.4 16.8 0.4 <LoD 8053 1405 <LoD <LoD 104.5 72
BMDDH23_01 16.8 17.7 0.9 <LoD 5989 112 <LoD <LoD 100.2 45
BMDDH23_01 17.7 18.2 0.5 <LoD 12826 2490 <LoD <LoD 87.6 147
BMDDH23_01 18.2 18.7 0.5 <LoD 5989 76 <LoD <LoD 49.1 64
BMDDH23_01 18.7 19.4 0.6 <LoD 7148 95 <LoD <LoD 72.6 76
BMDDH23_01 19.4 20.1 0.7 22 21179 282 <LoD <LoD 188.1 265
BMDDH23_01 20.1 20.7 0.6 249 128295 302 <LoD 1447 32.6 427
BMDDH23_01 20.7 21.5 0.8 32 21431 61 <LoD <LoD 52.4 117
BMDDH23_01 21.5 21.9 0.5 51 19094 95 <LoD <LoD 74.8 191
BMDDH23_01 21.9 22.6 0.6 63 24992 68 <LoD <LoD 48.2 240
BMDDH23_01 22.6 23.4 0.9 115 109279 84 <LoD 11623 38.2 190

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Hole_ID From
(m)
To (m) Interval
(m)
Cu
(ppm)
Fe
(ppm)
Li (ppm) Pb
(ppm)
S (ppm) Ta
(ppm)
Zn
(ppm)
BMDDH23_01 23.4 23.8 0.3 6012 201027 100 <LoD 150328 66.5 1294
BMDDH23_01 23.8 25.0 1.2 660 159070 201 <LoD 120231 0.8 1991
BMDDH23_01 32.5 32.9 0.3 1258 159818 305 <LoD 129887 1.7 3958
BMDDH23_01 36.8 37.6 0.9 609.8 163569 161 79 80607 0.55 3540
BMDDH23_01 39.2 39.7 0.5 479.3 159839 452 46 71688 1.81 3829
BMDDH23_01 41.1 41.8 0.7 359.8 130186 27 18 36406 0.18 1292
BMDDH23_01 42.7 43.1 0.4 776.9 250000 313 34 110999 0.51 3778
BMDDH23_01 43.1 43.4 0.3 769.2 229656 371 33 88317 0.7 3326
BMDDH23_01 44.9 45.5 0.6 670.6 224385 149 30 86750 1.02 3640
BMDDH23_01 45.5 45.9 0.4 1213.5 250000 224 48 114744 0.51 5103
BMDDH23_01 47.2 47.5 0.3 1222.4 206162 254 76 119702 0.46 3017
BMDDH23_01 64.0 64.9 0.9 1227.8 157227 229 345 95799 1.54 177
BMDDH23_01 121.0 121.7 0.7 3891.2 149484 311 154412 28970 10.8 9931
BMDDH23_01 138.5 139.0 0.5 5 10234 54 <LoD 1037 82.4 291
BMDDH23_01 139.0 139.7 0.7 17 5116 16 <LoD 899 40.2 361
BMDDH23_01 139.7 140.1 0.4 <LoD 3646 30 <LoD 273 23.8 315
BMDDH23_01 140.1 140.7 0.6 <LoD 3601 17 <LoD 303 30.5 321
BMDDH23_01 140.7 141.1 0.4 <LoD 3382 8 <LoD <LoD 16.1 295
BMDDH23_01 141.1 141.6 0.5 <LoD 2682 18 <LoD 204 6.4 345
BMDDH23_01 141.6 142.2 0.6 <LoD 4254 36 <LoD 533 30.6 442
BMDDH23_01 142.2 142.7 0.5 <LoD 5538 46 <LoD 290 34.9 261
BMDDH23_01 142.7 143.5 0.8 <LoD 7194 38 <LoD <LoD 25.3 122
BMDDH23_01 143.5 145.4 1.9 32 98293 371 <LoD 505 3.5 2804
BMDDH23_01 145.4 146.3 0.9 10 107414 151 <LoD 215 4.3 2067
BMDDH23_01 146.3 147.0 0.6 <LoD 4625 29 <LoD <LoD 29.2 226
BMDDH23_01 147.0 147.6 0.6 <LoD 4276 18 <LoD <LoD 44.4 182
BMDDH23_01 147.6 148.1 0.5 <LoD 6114 62 <LoD <LoD 71.4 141
BMDDH23_01 148.1 148.7 0.5 5 5160 32 <LoD <LoD 19.8 177
BMDDH23_01 148.7 149.5 0.9 43 92231 157 <LoD 1827 4 1151
BMDDH23_01 172.5 173.2 0.7 128 144747 408 <LoD 19149 1.7 4242
BMDDH23_01 173.2 173.7 0.4 <LoD 20404 79 <LoD 371 62.5 820
BMDDH23_01 173.7 174.7 1.0 32 112291 237 <LoD 1322 2.5 1440
BMDDH23_02 0.0 0.8 0.8 25 75598 237 <LoD <LoD 1.4 224
BMDDH23_02 0.8 1.2 0.5 7 76974 495 <LoD <LoD 5 304
BMDDH23_02 1.2 1.8 0.6 27 72312 339 <LoD <LoD 1.2 169
BMDDH23_02 1.8 2.7 0.9 <LoD 23584 769 <LoD <LoD 53.2 90
BMDDH23_02 2.7 3.4 0.6 <LoD 10000 4949 <LoD <LoD 42.5 104

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chariotcorporation.com

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Hole_ID From
(m)
To (m) Interval
(m)
Cu
(ppm)
Fe
(ppm)
Li (ppm) Pb
(ppm)
S (ppm) Ta
(ppm)
Zn
(ppm)
BMDDH23_02 3.4 4.3 0.9 <LoD 57981 1250 <LoD <LoD 14.9 168
BMDDH23_02 4.3 4.7 0.5 14 60538 1202 <LoD <LoD 21.8 220
BMDDH23_02 4.7 5.3 0.6 <LoD 7708 8149 <LoD <LoD 58.7 37
BMDDH23_02 5.3 5.9 0.6 <LoD 5999 3516 <LoD <LoD 33 35
BMDDH23_02 5.9 6.6 0.6 43 63851 1895 <LoD <LoD 3 75
BMDDH23_02 6.6 7.0 0.5 13 74942 1872 <LoD <LoD 0.9 110
BMDDH23_02 7.0 9.6 2.6 16 70704 1823 <LoD <LoD 2.5 121
BMDDH23_02 9.6 10.1 0.5 44 81958 1280 <LoD <LoD 0.5 86
BMDDH23_02 10.1 10.7 0.6 22 92141 1573 <LoD <LoD 2.1 111
BMDDH23_02 10.7 11.1 0.5 <LoD 8881 11404 <LoD <LoD 117.6 35
BMDDH23_02 11.1 11.9 0.8 <LoD 11053 15472 <LoD <LoD 136.4 73
BMDDH23_02 11.9 12.2 0.3 <LoD 11991 15766 <LoD <LoD 71.4 84
BMDDH23_02 12.2 13.0 0.7 <LoD 10167 14384 <LoD <LoD 104.2 57
BMDDH23_02 13.0 14.5 1.5 59 77195 729 <LoD 9777 97.7 417
BMDDH23_02 14.5 15.3 0.8 38 95135 518 <LoD 26132 81.5 164
BMDDH23_02 15.3 16.2 0.9 31 35979 1412 <LoD 3478 95.1 192
BMDDH23_02 16.2 17.0 0.9 27 36377 320 <LoD 2209 55.2 214
BMDDH23_02 17.0 17.7 0.6 158 134084 330 <LoD 16424 82.3 572
BMDDH23_02 17.7 18.4 0.7 242 163215 94 <LoD 32945 10.3 217
BMDDH23_02 18.4 19.2 0.8 190 176611 131 <LoD 28463 13.9 637
BMDDH23_02 19.2 20.2 1.0 103 131557 54 <LoD 16888 2.4 819
BMDDH23_02 20.2 21.2 1.0 44 128142 65 <LoD 26559 8.8 1189
BMDDH23_02 21.2 22.3 1.1 96 41534 80 <LoD 2863 130.4 465
BMDDH23_02 22.3 23.0 0.8 40 38851 113 <LoD 3976 70.2 278
BMDDH23_02 23.0 23.4 0.4 415 65441 138 <LoD 15252 93 317
BMDDH23_02 23.4 24.1 0.7 121 61499 82 <LoD 2263 34.7 671
BMDDH23_02 24.1 24.7 0.6 124 52638 77 <LoD 1530 68.4 549
BMDDH23_02 24.7 25.3 0.6 19 21962 61 <LoD 643 70.4 181
BMDDH23_02 25.3 26.2 0.9 202 86047 224 <LoD 305 29 942
BMDDH23_02 26.2 38.4 12.2 112 109919 188 <LoD 819 3.4 428
BMDDH23_02 38.4 39.6 1.2 59 107651 245 <LoD <LoD 1.1 140
BMDDH23_02 39.6 39.9 0.3 <LoD 9747 80 <LoD <LoD 46.3 59
BMDDH23_02 39.9 41.1 1.2 38 107547 302 <LoD <LoD 1.5 125
BMDDH23_03 39.3 39.9 0.6 43 91907 255 <LoD 647 1.6 101
BMDDH23_03 39.9 40.8 0.9 32 90802 237 <LoD <LoD 1.5 96
BMDDH23_03 40.8 40.9 0.2 61 84235 234 <LoD 1818 1.3 103
BMDDH23_03 40.9 42.1 1.1 23 83816 246 <LoD 650 7.1 94

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ABN 13 637 559 847

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Hole_ID From
(m)
To (m) Interval
(m)
Cu
(ppm)
Fe
(ppm)
Li (ppm) Pb
(ppm)
S (ppm) Ta
(ppm)
Zn
(ppm)
BMDDH23_03 42.1 42.9 0.9 27 80594 209 <LoD 647 1 95
BMDDH23_03 42.9 43.5 0.5 <LoD 83751 230 <LoD 235 0.9 94
BMDDH23_03 43.5 43.9 0.5 170 105247 401 <LoD 4686 1.2 119
BMDDH23_03 45.3 45.3 0.0 <LoD 12179 4846 <LoD -200 115.2 32
BMDDH23_03 46.0 46.0 0.0 <LoD 6429 6504 <LoD <LoD 88.1 12
BMDDH23_03 46.7 46.7 0.0 <LoD 7360 1970 <LoD <LoD 91.6 41
BMDDH23_03 47.5 48.5 0.9 <LoD 7437 4919 <LoD <LoD 123.9 28
BMDDH23_03 48.5 49.1 0.6 <LoD 7420 7879 <LoD <LoD 147.6 18
BMDDH23_03 49.1 50.0 0.9 <LoD 6331 4989 <LoD <LoD 99.2 16
BMDDH23_03 50.0 50.9 0.9 <LoD 5443 3074 <LoD <LoD 68.7 23
BMDDH23_03 50.9 51.8 0.9 <LoD 6120 4222 <LoD <LoD 88.2 25
BMDDH23_03 51.8 52.4 0.6 <LoD 4215 1545 <LoD <LoD 36.5 15
BMDDH23_03 52.4 53.3 0.9 <LoD 5871 8398 <LoD <LoD 41.2 13
BMDDH23_03 53.3 54.4 1.1 <LoD 4509 3477 <LoD <LoD 37.2 12
BMDDH23_03 54.4 55.3 0.9 <LoD 4230 1346 <LoD <LoD 39.5 17
BMDDH23_03 55.3 56.3 1.0 <LoD 4880 2260 <LoD <LoD 45.3 21
BMDDH23_03 56.3 57.3 1.0 <LoD 5243 3472 <LoD <LoD 66.5 15
BMDDH23_03 57.3 58.2 0.9 <LoD 5136 1533 <LoD <LoD 67.6 21
BMDDH23_03 58.2 59.2 1.0 <LoD 5079 2675 <LoD <LoD 103.8 15
BMDDH23_03 59.2 60.4 1.2 <LoD 6300 3032 <LoD <LoD 151 26
BMDDH23_03 60.4 61.1 0.8 <LoD 6551 4539 <LoD <LoD 117.2 24
BMDDH23_03 61.1 61.8 0.6 <LoD 5077 4414 <LoD <LoD 49.6 28
BMDDH23_03 61.8 62.7 0.9 7 7629 6573 <LoD <LoD 79 37
BMDDH23_03 62.7 64.3 1.6 37 30895 163 <LoD 395 2.1 51
BMDDH23_03 74.1 74.9 0.8 23 73165 263 <LoD 1015 2.7 107

Note: Less than limit of detection (“<LoD”)

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Appendix 3 – Select core samples re-analyzed for Base Metals

Cu Pb S Zn Pb*
SAMPLES ppm ppm ppm ppm ppm
BMDDH 0043 609.8 79 80607 3540
BMDDH 0044 479.3 46 71688 3829
BMDDH 0045 359.8 18 36406 1292
BMDDH 0046 776.9 34 110999 3778
BMDDH 0046-X 806.2 33 111687 3687
BMDDH 0047 769.2 33 88317 3326
BMDDH 0048 670.6 30 86750 3640
BMDDH 0049 1213.5 48 114744 5103
BMDDH 0050 26.6 60 2652 90
BMDDH 0051 1222.4 76 119702 3017
BMDDH 0052 1227.8 345 95799 177
BMDDH 0053 3891.2 >10000 28970 9931 154412
BMDDH 0053-X 3922.6 >10000 30576 9831
BMDDH 0053 (RUN FROM COARSE REJECT) 4172.6 >10000 31188 9608 146022

*Samples returning assay values > 10,000 ppm Pb were reanalyzed

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Appendix 4 – Soil Geochemistry Results[1]

EAST
(m)
NORTH
(m)
Soil Type Composited Comp Distance Li (ppm) Pb (ppm) Zn (ppm)
299963.7 4737906 Colluvium Yes 22.2 13 78
300402.3 4737801 Colluvium Yes 22.5 18 82
299913.3 4737904 Colluvium Yes 22.7 13 70
300253.4 4737800 Colluvium Yes 22.7 17 73
300199.1 4737805 Colluvium Yes 22.7 19 75
300304.6 4737800 Colluvium Yes 23 20 78
300352.1 4737801 Colluvium Yes 23.4 21 94
299670.6 4738905 Colluvium Yes 24 19 82
299615.9 4738902 Colluvium Yes 24.2 18 83
300002.4 4737805 Colluvium Yes 24.2 16 70
299566.9 4738901 Colluvium Yes 24.4 19 99
299865.4 4737906 Colluvium Yes 24.4 18 83
299467.3 4738702 Colluvium Yes 24.5 25 260
299452.1 4738602 Colluvium Yes 24.9 18 119
300216.9 4737905 Colluvium Yes 25 19 76
300312.2 4737898 Colluvium Yes 25 18 80
300113.9 4737905 Colluvium Yes 25.5 16 90
300364.4 4737900 Colluvium Yes 25.7 18 80
299554.9 4738608 Colluvium F 25.8 17 255
299466 4738903 Colluvium Yes 25.8 17 84
299499.6 4739002 Alluvium F 25.9 18 79
299718.3 4738902 Colluvium Yes 26 19 154
299870.7 4738908 Colluvium Yes 26 18 87
299798.4 4738001 Colluvium Yes 26 18 76
299550.7 4738203 Colluvium F 15 Meters 26.1 16 122
299668.6 4739305 Colluvium Yes 26.1 18 70
299897.7 4738205 Colluvium F 26.2 15 90
299716.4 4739303 Colluvium Yes 26.2 16 74
299817.4 4739304 Colluvium Yes 26.2 17 68
299601.4 4738800 Colluvium F 26.3 20 94
299512.4 4738699 Colluvium Yes 26.3 24 131
299414.4 4738502 Colluvium Yes 26.3 14 93
299515.3 4739102 Colluvium F 26.4 18 76

1 All coordinates are in NAD83 Z13N

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EAST
(m)
NORTH
(m)
Soil Type Composited Comp Distance Li (ppm) Pb (ppm) Zn (ppm)
299502.4 4738611 Colluvium F 26.5 17 116
299765.8 4738703 Colluvium Yes 26.5 23 90
299820.1 4738706 Colluvium Yes 26.7 23 82
299547.9 4739001 Colluvium F 26.8 20 94
299598.8 4738201 Colluvium F 15 Meters 26.8 17 85
299766.3 4739306 Colluvium Yes 26.8 18 70
299363.9 4738505 Colluvium Yes 26.9 15 78
300352.2 4738004 Colluvium Yes 26.9 17 78
300247.7 4738004 Colluvium Yes 26.9 18 76
299952 4738800 Colluvium F 15 Meters 27 19 83
300011.6 4737907 Colluvium Yes 27 16 79
300068.5 4737910 Colluvium Yes 27.1 14 83
300265.8 4737903 Colluvium Yes 27.1 17 85
299751.5 4738200 Colluvium F 15 Meters 27.3 16 103
299650.8 4738203 Colluvium Yes 15 Meters 27.6 18 82
299514.7 4739306 Colluvium Yes 27.6 19 78
299848.9 4738004 Colluvium F 27.6 17 71
300052.3 4738800 Colluvium F 27.7 24 89
299948.7 4738205 Colluvium F 15 Meters 27.8 20 90
299752.4 4738800 Colluvium F 27.9 20 85
300102.4 4737805 Colluvium Yes 27.9 20 74
299566.9 4738701 Colluvium Yes 28.1 20 100
300153.6 4737804 Colluvium Yes 28.1 19 85
299700.7 4738201 Colluvium F 15 Meters 28.2 21 112
299769.8 4738108 Colluvium Yes 28.2 18 89
299801.5 4738802 Colluvium F 28.3 18 84
299667.9 4738702 Colluvium Yes 28.3 17 101
299719.6 4738700 Colluvium Yes 28.3 18 89
299651.1 4738801 Colluvium F 28.4 19 87
299817.5 4739104 Colluvium Yes 28.6 18 76
299551.2 4738800 Colluvium F 28.7 19 93
299615.5 4739306 Colluvium Yes 28.7 18 77
299852.7 4738799 Colluvium F 28.9 17 81
299559.4 4738506 Colluvium Yes 28.9 18 99
299701.9 4738801 Colluvium F 29 19 91
299999 4738204 Colluvium F 15 Meters 29 22 103
299871.5 4738704 Colluvium Yes 29 19 89
299668.2 4738100 Colluvium Yes 29 18 102
299872.3 4738100 Colluvium Yes 29 18 79
300002.2 4738801 Colluvium F 29.1 21 88
299565.4 4739100 Colluvium Yes 29.1 18 79

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EAST
(m)
NORTH
(m)
Soil Type Composited Comp Distance Li (ppm) Pb (ppm) Zn (ppm)
299898.3 4738006 Colluvium Yes 29.2 19 77
299902 4738801 Colluvium F 29.3 20 90
299617.9 4738701 Colluvium Yes 29.3 19 95
299456.7 4738508 Colluvium Yes 29.3 17 119
299501.3 4738799 Colluvium F 29.5 21 136
299516.2 4738900 Colluvium Yes 29.5 13 80
299922.9 4738102 Colluvium Yes 29.5 19 78
300316.1 4738105 Colluvium Yes 29.5 18 89
299399.5 4738402 Colluvium F 15 Meters 29.6 15 76
300098.9 4737795 Colluvium Yes 29.6 17 75
299963.1 4739098 Colluvium Yes 29.6 18 75
300014.4 4738905 Colluvium Yes 29.6 18 85
299820.5 4738104 Colluvium Yes 29.6 16 86
299413.9 4738302 Colluvium F 15 Meters 29.7 23 78
299948.2 4738003 Colluvium Yes 29.8 19 131
300051.5 4738200 Colluvium F 15 Meters 29.9 19 96
299901.7 4739000 F 30 19 89
299869.5 4739303 Colluvium Yes 30.1 18 76
299715.5 4739102 Colluvium Yes 30.1 18 84
299715.4 4738105 Colluvium Yes 30.1 15 87
299948.4 4739000 Colluvium F 30.3 17 84
299515.6 4738302 Colluvium F 15 Meters 30.3 18 82
300301.5 4738005 Colluvium Yes 30.3 19 82
300050.5 4737804 Colluvium Yes 30.3 13 75
299713.9 4738502 Colluvium Yes 30.4 21 101
299465.5 4738304 Colluvium F 15 Meters 30.6 19 83
299599.4 4739002 Colluvium F 30.7 19 89
299704.2 4738603 Colluvium F 30.7 30 388
299766.8 4739103 Colluvium Yes 30.7 17 79
300001.2 4738004 Colluvium Yes 30.7 16 99
300200.5 4738008 Colluvium Yes 30.8 17 77
299497.5 4739199 Colluvium Yes 31 19 79
299914.2 4739099 Colluvium Yes 31 18 85
299849.9 4739003 Colluvium F 15 Meters 31.1 19 83
299753.6 4738607 Colluvium F 31.2 20 193
299566.1 4739305 Colluvium Yes 31.3 19 82
299511.2 4738508 Colluvium Yes 31.4 17 91
299548.2 4739199 Colluvium Yes 31.6 19 79
299667.8 4739101 Colluvium Yes 31.6 19 91
299919.3 4738702 Colluvium Yes 31.6 19 94
299966.2 4738104 Colluvium Yes 31.7 17 82
299652.7 4738604 Colluvium F 31.9 22 519

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EAST
(m)
NORTH
(m)
Soil Type Composited Comp Distance Li (ppm) Pb (ppm) Zn (ppm)
299865.7 4739101 Colluvium Yes 31.9 18 91
300067.1 4738700 Colluvium Yes 32.3 24 157
299666.4 4738302 Colluvium F 15 Meters 32.6 19 110
299770.9 4738910 Colluvium Yes 32.6 19 105
299917.4 4738906 Colluvium Yes 32.6 19 102
299659.2 4738503 Colluvium Yes 32.6 17 95
299966.8 4738904 Colluvium Yes 32.7 17 118
299615.3 4739105 Colluvium Yes 32.8 17 80
299817.6 4738910 Colluvium Yes 32.8 17 89
299896.6 4739196 F 33.2 18 89
299798.3 4739001 Colluvium F 33.3 19 102
299608.8 4738513 Colluvium Yes 33.3 17 99
299564.3 4738304 Colluvium F 33.5 12 108
300166.9 4737905 Alluvium Yes 33.8 19 78
299748.9 4739003 F 34.2 19 155
300202.3 4738404 F 15 Meters 34.2 19 77
299701.7 4738402 Colluvium Yes 15 Meters 34.2 16 86
299714.7 4738305 Colluvium F 15 Meters 34.2 17 91
300299.4 4738200 Colluvium F 15 Meters 34.3 21 107
299702.8 4739003 Colluvium F 34.6 23 115
299797.5 4739201 Colluvium Yes 34.9 17 79
299968.5 4738307 Colluvium F 15 Meters 34.9 17 90
300017.1 4738702 Colluvium Yes 34.9 25 274
300103.3 4738596 Colluvium Yes 34.9 34 265
299748 4739196 F 35.1 19 90
299647.6 4739202 Colluvium Yes 35.1 22 88
299862 4739199 F 35.2 16 93
299749.1 4738402 Colluvium F 35.3 16 88
299914.5 4738306 Colluvium F 15 Meters 35.3 16 89
300017.5 4738306 Colluvium F 15 Meters 35.8 17 99
300049.8 4738005 Colluvium Yes 35.8 15 95
300274.9 4738102 Colluvium Yes 37.3 19 94
299966.3 4738699 Colluvium Yes 37.4 24 114
299998.8 4739002 Colluvium F 37.5 21 100
299604.2 4738598 Colluvium F 37.6 14 212
300163 4738506 Colluvium Yes 38.1 21 83
300112.3 4738504 Colluvium Yes 38.2 21 84
299801.6 4738603 Colluvium F 38.6 29 258
300016.9 4738105 Colluvium Yes 38.9 17 75
299802.4 4738205 Colluvium F 39.1 17 93
299950.3 4738401 Colluvium F 39.3 21 103
299550 4738404 Colluvium Yes 39.3 18 88

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EAST
(m)
NORTH
(m)
Soil Type Composited Comp Distance Li (ppm) Pb (ppm) Zn (ppm)
299847.1 4738204 Colluvium F 39.3 10 78
300117.2 4738307 Colluvium F 15 Meters 39.8 18 104
299651.7 4738403 Colluvium F 15 Meters 39.9 16 87
299648.1 4739004 F 40.3 20 92
299601.8 4738403 Colluvium Yes 15 Meters 40.6 14 101
300217 4738304 F 15 Meters 41 19 81
299699.1 4739197 Colluvium Yes 41 16 84
299597.3 4739200 Colluvium Yes 41 18 82
300066.9 4738305 Colluvium F 41.4 18 108
299764.7 4738302 Colluvium F 15 Meters 42.4 18 83
300049.2 4738401 Colluvium Yes 15 Meters 42.6 18 84
300250.4 4738198 Colluvium F 15 Meters 43.9 18 95
300000 4738401 Colluvium F 15 Meters 45.3 19 87
300054.1 4738605 Colluvium Yes 46.4 31 261
300067.7 4738103 Colluvium Yes 46.4 18 84
299614.8 4738303 Colluvium F 15 Meters 46.6 14 87
300148.3 4738402 Colluvium F 46.9 14 80
300163.6 4738301 Colluvium F 15 Meters 48.4 24 104
299450.3 4738402 Colluvium F 49.8 13 89
300011.4 4738507 Colluvium Yes 50.2 24 121
299853.7 4738607 Colluvium F 50.3 19 131
300101.3 4738400 Colluvium F 51.7 21 97
299898 4738401 Colluvium Yes 15 Meters 53.3 19 94
299800.2 4738404 Colluvium F 15 Meters 53.3 19 96
300099.4 4738202 Colluvium F 15 Meters 55.4 16 82
299500.5 4738401 Colluvium Yes 15 Meters 56.8 20 112
299851.1 4738404 Colluvium Yes 15 Meters 60.1 24 114
300060.9 4738505 Colluvium Yes 60.4 20 81
299863.2 4738303 Colluvium F 61.8 14 86
300002.2 4738608 Colluvium Yes 62.1 35 423
300199.2 4738205 Colluvium F 15 Meters 63.3 17 92
300117.7 4738105 Colluvium Yes 67 18 76
299810.4 4738506 Colluvium Yes 69.8 25 104
300150.7 4738206 F 15 Meters 77.1 18 88
299904.4 4738606 Colluvium F 77.9 16 105
299811 4738306 Alluvium F 81.5 18 95
299952.4 4738605 Colluvium F 85.4 13 259
300224.3 4738104 Colluvium Yes 93 18 87
299764.6 4738505 Colluvium Yes 93.3 19 110
299864.7 4738506 Colluvium Yes 114.8 26 130
299915.7 4738505 Colluvium Yes 117.3 24 124
299963.4 4738503 Colluvium Yes 118.2 50 176

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EAST
(m)
NORTH
(m)
Soil Type Composited Comp Distance Li (ppm) Pb (ppm) Zn (ppm)
299763.7 4738510 Colluvium Yes 152.1 16 103
300172 4738106 Colluvium Yes 169.7 20 82

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Appendix 5 – JORC Table 1

JORC Code, 2012 Edition – Table 1

Section 1 Sampling Techniques and Data

Criteria JORC Code explanation Commentary Commentary
Sampling Nature and quality of sampling (eg cut channels, Diamond drilling which produces drill core has been utilised to sample the
techniques random chips, or specific specialised industry pegmatite below ground surface. This method is recognised as providing high
standard measurement tools appropriate to the quality information and samples of the unexposed geology.
minerals under investigation, such as down hole Core is split in half longitudinally using a core saw, and the half core was
gamma sondes, or handheld XRF instruments, sampled on variable intervals typically between 0.25 and 1.5m intervals.
etc). These examples should not be taken as Sampling was based primarily on rock type taking care not to include pegmatite
limiting the broad meaning of sampling. and schist in the one sample, in larger dikes samples were further divided
Include reference to measures taken to ensure based on mineralogy. Sample mass ranged between 0.5 and 1.5kg primarily
sample representivity and the appropriate reflecting sample interval width, the typical mass averaged approximately 1kg.
calibration of any measurement tools or systems Samples were from ‘B horizon’ and were taken as composites consisting of
used. three sub-samples spaced approximately 5m apart. Samples were dried and
Aspects of the determination of mineralisation screened at the Laboratory and the -10 to +80 mesh fraction retained for
that are Material to the Public Report. analysis. Soil samples were assigned unique alphanumeric sample codes.
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.
Drilling Drill type (eg core, reverse circulation, open-hole Diamond core drilling was done using HQ (triple tube) rods from surface with a
techniques hammer, rotary air blast, auger, Bangka, sonic, Longyear LF90 rig at the Black Mountain Project from November to December
etc) and details (eg core diameter, triple or 2023.
standard tube, depth of diamond tails, face- Most holes are inclined at between 40° and 70° to intersect the moderately to
sampling bit or other type, whether core is steeply dipping pegmatites.
oriented and if so, by what method, etc). Core was oriented with typicalgyroscopic setupon the topof the core barrel,

30

Criteria JORC Code explanation Commentary Commentary
downhole surveys taken every 30m.
Drill sample Method of recording and assessing core and chip
Recoveries were based on measured recovered intervals between the core-
recovery sample recoveries and results assessed. blocks.
Measures taken to maximise sample recovery Recoveries were generally very high except in the rare highly fractured fault
and ensure representative nature of the samples. zones which were typically 0.5 to 1m in width comprising less than several
Whether a relationship exists between sample percent overall. Intervals of broken core were sampled separately and where
recovery and grade and whether sample bias down-hole contamination, if present, was rare and was noted with the interval
may have occurred due to preferential loss/gain not included in assay reporting.
of fine/coarse material. Overall recovery was +97%. There was no apparent relationship between
recovery and grade due to the overall high recoveries.
Weathering is not intense. It is restricted to the upper 2 to 5m and did not have
any effect on recoveries.
Logging Whether core and chip samples have been Quantitative and qualitative core logging was conducted on an ongoing basis
geologically and geotechnically logged to a level during the drill program. Detailing lithologies, alteration and mineral species
of detail to support appropriate Mineral Resource present along with oxidation etc, were the basis for selecting sampling intervals.
estimation, mining studies and metallurgical Core was photographed with recoveries and RQD measured prior to splitting.
studies. All core was geologically logged before splitting and sampling for assaying.
Whether logging is qualitative or quantitative in All logging and photographic data are stored in the database.
nature. Core (or costean, channel, etc) Core was oriented and a reference line drawn along the top of the core, cut line
photography. was drawn adjacent to the orientation line, the half without the orientation line
The total length and percentage of the relevant was sampled. The half retained after sampling was that with the reference line.
intersections logged.
Sub-sampling
If core, whether cut or sawn and whether quarter, Core is sawn in half, and the half core was sampled on variable intervals
techniques
and sample
preparation
half or all core taken.
If non-core, whether riffled, tube sampled, rotary
split, etc and whether sampled wet or dry.

typically between 0.25 and 1.5m intervals.
Standards, duplicates, and blanks are inserted sequentially every 10thsample.
The half core samples were dried in the Lab, crushed to >70% - 2mm; split,
For all sample types, the nature, quality and then pulverized 500g to >85% -75 micron.
appropriateness of the sample preparation Duplicate samples were taken in the Laboratory, the crushed core was split into
technique. two sub samples, which were pulverized and analysed. The Company provided
Quality control procedures adopted for all sub- a numbered sample bag for any remaining coarse reject from the duplicate.
sampling stages to maximise representivity of The drilling produced HQ drill core and is considered toprovide a representative

31

Criteria JORC Code explanation Commentary Commentary
samples. sample of the pegmatite which is coarse-grained and half core samples
Measures taken to ensure that the sampling is collected ranging from 0.25-1.5m from the hanging wall to footwall contacts.
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 beingsampled.
Quality of The nature, quality and appropriateness of the The samples were assayed for a suite of 50 elements including: Co, Cs, Fe, Li,
assay data
and
laboratory
tests
assaying and laboratory procedures used and
whether the technique is considered partial or
total.
Ni, Pb, Rb, Sn, Ta and Zn.
Sample pulps were analysed at American Assay Labs (1506 Glendale Ave,
Sparks, NV 89431, USA) using a sodium peroxide fusion of an XXg aliquot with
For geophysical tools, spectrometers, handheld ICP-OES finish (method code IMNF53). Over limit values (> 10,000 ppm Li)
XRF instruments, etc, the parameters used in were re-assayed using ICP analysis. Intervals of sulfide mineralisation were
determining the analysis including instrument assayed using method IM-4AB52.
make and model, reading times, calibrations Peroxide fusion results in the complete digestion of the sample into a molten
factors applied and their derivation, etc. flux. As fusion digestions are more aggressive than acid digestion methods,
Nature of quality control procedures adopted (eg they are suitable for many refractory, difficult-to-dissolve minerals such as
standards, blanks, duplicates, external laboratory chromite, ilmenite, spinel, cassiterite and minerals of the tantalum-tungsten
checks) and whether acceptable levels of solid solution series. They also provide a more-complete digestion of some
accuracy (ie lack of bias) and precision have silicate mineral species and are considered to provide the most reliable
been established. determinations of lithium mineralisation.
Sodium peroxide fusion is a total digest and considered the preferred method of
assaying pegmatite samples.
A standard industry accepted Quality Assurance and Quality Control (“QA/QC”)
program was employed to monitor the precision, accuracy and general reliability
of the assay results from the drilling programme. The protocol included the
insertion of duplicates, blanks and certified reference materials (CRMs) into the
sample stream. In addition, American Assay Labs also incorporated its own
internal QA/QC procedures to monitor its assay results prior to release to
Chariot.
OREAS standards were checked for laboratory accuracy, blanks checked for
evidence of laboratory contamination and duplicate assays on crushed core
reviewed for potential nugget effects. Variations, where present, were within
acceptable limits.

32

Criteria JORC Code explanation Commentary Commentary
Refer to the JORC Table 1 in the Prospectus for further details on the rock chip
sampling program.
Geophysical instruments were not used in assessing the mineralisation. One
core sample returned values >10,000 ppm Pb which was re analyzed using IM-
4AB52 with Ore Grade finish.
Soil samples were screened and -10+80 mesh fraction split and assayed by
total digest and 48 elements determined by ICP-OES & MS analyses.
The Competent Person is satisfied that the results of the QA/QC are acceptable
and that the assay data from American Assay Labs is suitable for the reporting
of the exploration results.
Verification of
The verification of significant intersections by The one high-grade Pb sample was re-assayed using coarse reject material.
sampling and
assaying
either independent or alternative company
personnel.
Internal verification of the drilling and pegmatite intersections was routinely
conducted by the exploration manager.
The use of twinned holes. No independent reviews or check sampling or assays have been conducted.
Documentation of primary data, data entry The sampling served to verify historical mapping and sampling results.
procedures, data verification, data storage Logging was entered on field logs. Data was entered and stored electronically in
(physical and electronic) protocols. an Access database.
Discuss any adjustment to assay data. All core photos are stored on the Company database.
No material data recording issues have been identified.
No verification was conducted on soil samples.
Assay data has not been adjusted.
Location of Accuracy and quality of surveys used to locate Drill hole collar location and elevations are determined from the handheld GPS
data points drill holes (collar and down-hole surveys), and are suitable for the reporting of exploration results (approximately 2.5m
trenches, mine workings and other locations used vertical and 5m vertical). Elevations were checked against the available USGS
in Mineral Resource estimation. DTM with 3m resolution. Locations were recorded using a handheld Garmin
Specification of the grid system used. GPS.
Quality and adequacy of topographic control. Angled holes were surveyed using standard a standard drilling gyroscopic tool.
Soil sample locations recorded via a handheld GPS.

All coordinates are reported in UTM NAD83 Zone 13N.

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Criteria JORC Code explanation Commentary Commentary
Data spacing Data spacing for reporting of Exploration Results. This first phase of exploration drilling at Black Mountain, designed to confirm the
and
distribution
Whether the data spacing and distribution is
sufficient to establish the degree of geological
thickness, orientation and grade of mineralisation beneath the identified
outcropping pegmatites in preparation for a more detailed closer spaced and
and grade continuity appropriate for the Mineral systematic second phase of resource definition drilling.
Resource and Ore Reserve estimation Samples are typically between 0.5 and 1.5m in length, no compositing of
procedure(s) and classifications applied. samples will be done at this early stage.
Whether sample compositing has been applied.
Orientation of Whether the orientation of sampling achieves The pegmatite dikes dip at between 70° and 90° degrees. The inclination of the
data in
relation to
geological
structure
unbiased sampling of possible structures and the
extent to which this is known, considering the
deposit type.
drill holes varied between 60° and 65 degrees° and orientated normal to the
strike of the pegmatite.
Reported intervals are apparent widths which are greater than the true widths.
If the relationship between the drilling orientation Based on the drill hole orientations relative to the pegmatite orientation the
and the orientation of key mineralised structures estimated true widths are range between 40% and 90% of the apparent width
is considered to have introduced a sampling bias, but have not been accurately established at this point.
this should be assessed and reported if material. The relationship between drilling orientation and mineralisation is considered
appropriate and should not introduce any sampling bias.
Sample The measures taken to ensure sample security. Sample security is not considered to be issue for the Black Mountain Project.
security Core was promptly removed from the drill site to the core logging facility where
it remained until being shipped to the laboratory by Chariot personnel.
Audits or The results of any audits or reviews of sampling ERM Australia Consultants Pty Ltd (previously CSA Global) (“CSA Global”),
reviews techniques and data. ERM Sustainable Mining Services, have provided technical guidance for the
development of the Black Mountain exploration plan and completed an
independent review of the data, geological interpretations and exploration
results pertaining to this announcement. CSA Global are satisfied these
scientific and technical disclosures were appropriate to support the reporting of
these Exploration Results.

Section 2 Reporting of Exploration Results

Criteria JORC Code explanation Commentary Commentary
Mineral Type, reference name/number, location and The Black Mountain project area comprises 134 unpatented lode mining claims
tenement and ownershipincludingagreements or material coveringan area of 878 ha in Natrona Country, Wyoming.

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Criteria JORC Code explanation Commentary Commentary
land tenure issues with third parties such as joint ventures, Chariot currently holds a 93.9% interest in Wyoming Lithium Pty Ltd which holds
status partnerships, overriding royalties, native title a 100% interest in Panther Lithium Corporation (“PLC”). PLC holds 100%
interests, historical sites, wilderness or national interest in the Black Mountain Project.
park and environmental settings. There are no known impediments to the company tenure nor related issues
The security of the tenure held at the time of which affect our ability to conduct exploration.
reporting along with any known impediments to
obtaininga licence to operate in the area.
Exploration Acknowledgment and appraisal of exploration by The Black Mountain pegmatite deposit is first described by Love (1942). A
done by other
parties
other parties. single spodumene dyke striking ENE with a dip of 30oto 60oto SSE. The dyke
is described as 250 feet (75 m) in strike length and up to 10 feet (3 m) in
thickness. The dyke in obscured by alluvium on its south-western end and is
folded and irregular. The pegmatite contains spodumene with coarse K-
feldspar, white quartz, mica and tourmaline. At this time development consisted
of two small prospecting pits.
A number of other exploration pits thought to date back to this period have also
been identified from satellite imagery but is possibly related to some
undocumented exploration.
A comprehensive description of pegmatite occurrences in Wyoming and
Colorado was compiled by the USGS and is provided by Hanley et al. (1950).
This study describes 114 pegmatite occurrences in these states with an
emphasis on beryl bearing pegmatites as the main commodity of economic
interest at that time. Other commodities considered in this study were beryllium,
lithia (Li2O), muscovite, columbium-tantalum, potash feldspar and rare earth
pegmatites.
Two types of lithium-bearing pegmatite are known in Colorado and Wyoming. In
one variety, the lithia is predominantly in the mineral lepidolite, a lithium mica,
and in the other it is in the minerals spodumene and amblygonite.
In 2022, Chariot conducted a first pass geochemistry survey at the Black
Mountain Project comprising of ten (10) rock chip samples collected from
pegmatite outcrops.
In 2023, Chariot conducted a follow up geochemistry survey at the Black
Mountain Project comprising of twelve (12) rock chip samples collected from
pegmatite outcrops.

35

Criteria JORC Code explanation Commentary Commentary
Geology Deposit type, geological setting and style of The Black Mountain is a typical LCT-type Pegmatite dike swarm with coarse
mineralisation. grained spodumene outcropping at surface. The Pegmatite dikes are hosted
within Archean Greenstones and are assumed to be associated with Late-
Archean to Lower Proterozoic dated between 2.6 and 2.5 Ga.
The LCT-type pegmatite dike swarm is located within the Granite Mountains of
Central Wyoming, USA, comprising part of the Archean-Neoproterozoic
supracrustal belt of North America.
Drill hole A summary of all information material to the Drillhole collars, survey and assay data are summarised in Appendix 1 of this
Information understanding of the exploration results including announcement.
a tabulation of the following information for all
Material drill holes:
o
easting and northing of the drill hole
collar
o
elevation or RL (Reduced Level –
elevation above sea level in meters) of
the drill hole collar
o
dip and azimuth of the hole
o
down hole length and interception depth
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 Intervals are reported as weighted averages based on interval lengths.
aggregation
methods
averaging techniques, maximum and/or minimum
grade truncations (e.g., cutting of high grades)


No cut-off grades are applied to these exploration results.
Lithium assays in ppm are converted to % Li2O grades by multiplying by a
and cut-off grades are usually Material and factor of 2.153 and then dividing by 10,000 to get to % Li2O.
should be stated. Tantalum assays in ppm are converted to Ta2O5 in ppm by multiplying by a
Where aggregate intercepts incorporate short factor of 1.2211.
lengths of high-grade results and longer lengths No equivalent values are used or reported.
of low-grade results, theprocedure used for such

36

Criteria JORC Code explanation Commentary Commentary
aggregation should be stated and some typical
examples of such aggregations should be shown
in detail.
The assumptions used for any reporting of metal
equivalent values should be clearlystated.
Relationship These relationships are particularly important in Majority of samples were taken at 0.25-1.5m lengths.
between
mineralisation
widths and
intercept
lengths

the reporting of Exploration Results.
If the geometry of the mineralisation with respect
to the drill hole angle is known, its nature should
be reported.
The pegmatite dikes dip at between 70 and 90 degrees, the azimuth of the drill
holes was normal to the pegmatite strike and the inclination of the drill holes
varied between 50 and 65 degrees, typically intersecting the dikes at an angle
between 45 and 70 degrees. Since most drilling intersections do not represent
If it is not known and only the down hole lengths the true thickness and the estimated true widths range between 40% and 90%
are reported, there should be a clear statement to of the of the mineralised drill intervals reported in this announcement.
this effect (e.g. ‘down hole length, true width not The relationship between drilling orientation and mineralisation is considered
known’). appropriate and should not introduce any sampling bias.
Diagrams Appropriate maps and sections (with scales) and Refer to the body of the announcement for the appropriate section and plan
tabulations of intercepts should be included for view maps.
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
All exploration results applicable to the Black Mountain Project have been
reporting Results is not practicable, representative reported.
reporting of both low and high grades and/or
widths should be practiced to avoid misleading
reportingof Exploration Results.
Other Other exploration data, if meaningful and Chariot completed a high-resolution ground magnetics survey at Black
substantive
exploration
data
material, should be reported including (but not
limited to): geological observations; geophysical
survey results; geochemical survey results; bulk
Mountain comprising 108 east-west orientated lines, spaced 25 m apart, and
each 3.55 km long for a total of 383.4 line-km. Refer to the Prospectus for
further details.
samples – size and method of treatment;
metallurgical test results; bulk density,
groundwater, geotechnical and rock
characteristics;potential deleterious or

37

Criteria JORC Code explanation Commentary Commentary
contaminatingsubstances.
Further work The nature and scale of planned further work Chariot plans to conduct a detailed re-logging of the Phase 1 Program drill core
(e.g., tests for lateral extensions or depth along with a detailed petrographic study of the mineralisation and selection and
extensions or large-scale step-out drilling). submittal of samples for initial metallurgical testing.
Diagrams clearly highlighting the areas of Phase 2 Resource Drilling Program, will be contingent on the results of the
possible extensions, including the main Phase 1 drilling and will include a more extensive 5,000 to 10,000m initial
geological interpretations and future drilling resource definition drill program expected to commence in Q3 or Q4 of 2024.
areas, provided this information is not In addition, the Company plans to run a preliminary IP/Resistivity survey over
commercially sensitive. the area of anomalous Zn-Pb soil geochemistry to assist in siting several holes
to test the nature of this base metal mineralisation.

Section 3 (Estimation and Reporting of Mineral Resources) has been excluded as no Mineral Resources have been estimated for the Black Mountain Project to date.

38