Metallica Minerals Limited

METALLICA MINERALS LIMITED

A.C.N. 076 696 092

EPM 25779 - “Warrior”

ESMERALDA PROJECT

ANNUAL REPORT FOR THE FIRST YEAR PERIOD

25/06/2015 to 24/06/2016

TENEMENT HOLDER: TOUCHSTONE RESOURCES PTY LTD

MANAGER: Metallica Minerals Ltd

AUTHORS: N. FORBES

MAP SHEETS: 1: 250 000 Croydon SE54-11

1: 100 000 Prospect 7360

COMMODITIES: GRAPHITE, Au, Cu, Pt, Ti

GEOGRAPHIC COORDS: -18° 50'S / 142°12'E

TECTONIC: Georgetown Inlier

DATE: 24 June 2016

1 Table of Contents

Page No.

1. SUMMARY ...... 7

2. INTRODUCTION ...... 8

3. LOCATION, ACCESS & SETTING ...... 9

ENVIRONMENTAL CONSIDERATIONS ...... 9 Endangered Regional Ecosystems ...... 9 Other Environmentally Sensitive Areas ...... 11 Cultural Heritage / Aboriginal Cultural Heritage / Heritage Sites ...... 11 4. INDUSTRY BACKGROUND AND MARKET ...... 13

5. TENURE ...... 14

TENEMENT RESTRICTIONS ...... 14 RELINQUISHED SUB BLOCKS ...... 14 NATIVE TITLE ...... 14 6. GEOLOGICAL SUMMARY ...... 16

REGIONAL ...... 16 LOCAL GEOLOGY ...... 17 MINERALISATION ...... 19 7. PREVIOUS EXPLORATION ...... 20

SUMMARY ...... 20 8. TECHNICAL SUMMARY OF WORK COMPLETED IN THE FIRST YEAR ... 25

COMPLIANCE STATEMENT FOR PROGRAM OF ACTIVITIES ...... 25 Approved Work Program for Year 1 ...... 25 DATA REVIEW ...... 25 HISTORIC PERCUSSION DRILL CHIPS ...... 25 DRILLING ...... 26 Drilling Contractor ...... 26 Field Logistics ...... 26 Access Tracks & Drill Pad Preparation ...... 27 Accommodation ...... 27 Drill Hole Details ...... 27 Hole WD002 ...... 28 Hole WD003 ...... 29 Hole Completion ...... 30 Core Handling ...... 31 Core Transport ...... 31 Core Cutting ...... 32 CORE LOGGING ...... 32 Geological ...... 32 Magnetic Susceptibility...... 33 Specific Gravity ...... 33 PETROLOGY ...... 33 Generalised Hydrothermal Alteration Assemblage ...... 34 Graphite Mineralisation origin ...... 34 Petrologist’s Comments; ...... 35 GEOCHEMISTRY ...... 36 PRELIMINARY METALLURGY ...... 37 2 GEOLOGICAL MODEL ...... 38 RESOURCES & RESERVES ...... 38 ECONOMIC POTENTIAL OF EPM 25779 WARRIOR ...... 38 9. PROPOSED EXPLORATION PROGRAMME FOR YEAR 2 ...... 39

10. REFERENCES ...... 40

11. ATTACHMENTS ...... 43

ATTACHMENT 1 ...... 43 Drill Hole Plan 1:50,000 ...... 43 12. APPENDICES ...... 44

APPENDIX 1 ...... 45 Warrior Historic Drilling ...... 45 APPENDIX 2 ...... 48 Detailed Geological Logs ...... 48 APPENDIX 3 ...... 66 Drill Hole Assays ...... 66 APPENDIX 3A ...... 71 WD002 Assay Certificates ...... 71 APPENDIX 3B ...... 72 WD003 Assay Certificates ...... 72 APPENDIX 3C ...... 73 Assay Data ...... 73 APPENDIX 4 ...... 74 Specific Gravity & Magnetic Susceptibility ...... 74 APPENDIX 5 ...... 79 Preliminary Metallurgical Report ...... 79 APPENDIX 6 ...... 80 RC002A Drill Chip (Historic) Mineral Liberation Report ...... 80 APPENDIX 7 ...... 81 Petrology Report Geochempet Services...... 81 APPENDIX 8A ...... 82 WD002 Core Tray Photography ...... 82 APPENDIX 8B ...... 83 WD003 Core Tray Photography ...... 83

Note:

This report complies with the MRA reporting regulations as prescribed in sections 13B, 13C or 13D of the Mineral Resources Regulation 1989. The exploration work completed on these tenements complies with the Work Program in the tenure document. Expenditures on the tenements have been met or exceeded.

LIST OF TABLES

Table 1: Graphite Types ...... 13 Table 2: Sub blocks in EPM...... 14 Table 3: Geological Sequence in the North Western Georgetown Inlier ...... 17 Table 4: Warrior Previous Exploration ...... 21

Table 5: Year 1 Approved Program ...... 25 Table 6: Drill Hole Details ...... 28

Table 7: Summary Drill Log ...... 32 Table 8: Petrology ...... 34 Table 9: Analysis Details ...... 37 Table 10: Graphitic Carbon Intervals ...... 37 Table 11: Year 2 Approved Program ...... 39 Table 12: EPMs 25779 Warrior Historic Exploration ...... 41 Table 13: Warrior Historic Drilling Details ...... 45

LIST OF FIGURES

Figure 1: Location Map ...... 10 Figure 2: EPA Environmentally Sensitive Areas ...... 12 Figure 3: Sub Block Location Map ...... 15 Figure 4: EPM 25779 Geology ...... 18 Figure 5: Graphite in Core ...... 19 Figure 6: Warrior Magnetics, EM & Historic Drilling ...... 21 Figure 7: Drill Rig ...... 26 Figure 8: Drill Hole Plan ...... 27 Figure 9: Rowe Bore Camp ...... 30 Figure 10: Core Handling...... 31 Figure 11: Core Transport ...... 31

5 Copyright Statement

ACKNOWLEDGEMENT AND WARRANTY

1. Subject to 2, the tenure holder acknowledges that this Report, including the material, information and data incorporated in it, has been made under the direction or control of the State of Queensland (the State) within the meaning of section 176 of the Copyright Act 1968 (Cwth).

2. To the extent that copyright in any material included in this Report is not owned by the State, the tenure holder warrants that it has the full legal right and authority to grant, and does hereby grant, to the State, subject to any confidentiality obligation undertaken by the State, the right to do (including to authorise any other person to do) any act in the copyright, including to: use; reproduce; publish; and Communicate in electronic form to the public, such material, including any data and information included in the material.

3. Without limiting the scope of 1 and 2 above, the tenure holder warrants that all relevant authorisations and consents have been obtained for all acts referred to in 1 and 2 above, to ensure that the doing of any of the acts is not unauthorised within the meaning of section

29(6) of the Copyright Act (Cwth) .

6 1. SUMMARY

The Esmeralda Project was established in late 2014 by Touchstone Resources Pty Ltd a wholly owned subsidiary of ASX Listed 7Company Metallica Minerals Ltd (ASX Code MLM). The project was initiated to investigate the graphitic granites of the Esmeralda Super-suite in the Croydon Province, North Queensland. EPM 25779 “Warrior” is part of the Esmeralda Project which also comprises EPMs 25806 “Esmeralda West” and 25807 “Esmeralda East”

Hydrothermal mineralisation models have been developed by Touchstone for the graphitic Esmeralda Granite. Touchstone is confident that the Warrior style mineralisation is extensive regionally within the Esmeralda Granite and is similar in mineralisation style to the Croydon graphites identified 70km to the north.

The Esmeralda Graphite Project is located in the Proterozoic Croydon Province in North Queensland. Both the Esmeralda Super-suite Granites and Croydon Volcanics are inherently graphitic (2%) which make them unusual and extremely rare. They have been the subject of historic investigation particularly looking for links between the gold mineralisation at Croydon and it’s relationship to the graphite.

Work completed in the first year included a detailed literature review of historic exploration in the region and associated papers relating to graphite mineralisation within the Esmeralda Granites.

MLM completed two (2) core holes for 309m drilled to twin historic exploration holes with graphite mineralisation. Both holes intersected broad intersections of graphitic granite which was split for petrography and geochemical analysis, as well as preliminary metallurgical analysis. Core drilling was primarily to confirm the known graphite occurrence and provide sample to determine if quality of the graphite mineralisation within the region.

The graphite mineralisation is pervasive and consistent through the graphitic granite and with promising recovery (92%) and purity (97.8%) achieved in preliminary metallurgy, is an attractive target for additional exploration.

7 2. INTRODUCTION

The Esmeralda Project is 100% owned and operated by Metallica Minerals Ltd (MLM) subsidiary company Touchstone Resource Pty Ltd. The project is covered by Cainozoic and Mesozoic sediments beneath which is known Proterozoic basement rocks believed to be part the Esmeralda Supersuite. MLM is primarily targeting hydrothermal graphite mineralisation within the interpreted Esmeralda Granite.

EPM 25779 was granted on 24 June 2015 for an initial period of five (5) years. The tenement initially comprised 54 sub-blocks within the Normanton Block, and largely located within the Esmeralda Station. The tenement is located south of the town of Croydon and is accessed from Croydon Richmond Road. Warrior is located on the Croydon (7361) 1:100,000 map sheets on the Croydon SE55 11 1:250,000 map sheet.

Warrior was considered attractive as it covered known intersections of graphitic granites of the Esmeralda Supersuite. Graphite mineralisation has been identified in the region previously, with only cursory investigations of its quality and potential uses.

MLM completed two core holes in 2015 and conducted preliminary metallurgical analysis to determine the potential quality of the graphite and whether it is an attractive exploration target.

8 3. LOCATION, ACCESS & SETTING

The Warrior Project area is located in North West Queensland 70km south of the township of Croydon. The tenement is accessed via the Croydon-Richmond Road which is a sealed and formed dirt road which accesses the Gulf Development Road approximately 28km east of Croydon. (Figure 1)

The Warrior Project is located predominantly on Esmeralda Station, approximately 70 kilometres south of the town of Croydon in North West Queensland. The project is contained within the Croydon (SE54-11) 1:250,000 and the Prospect (7360) 1:100,000 map sheets and is centred on 142.2°E -18.8°S.

The Warrior EPM is set on flat open country and Pastoral activities of cattle breeding and grazing are the main land use.

Environmental Considerations

The Warrior tenure holds Environmental Authority (EA) for Level 2 Code Compliant activities, formerly termed a Standard EA. The environmental authority for EPM 22779 is EPSX02556214. At this stage there are no significant additional conditions attached to the EA of EPM 25779, apart from a reminder to comply with the Code of Environmental Compliance for Exploration and Mineral Development Projects.

Endangered Regional Ecosystems

Endangered Regional Ecosystems (EREs) are described in Sattler and Williams (1999) "The Conservation Status of Queensland Bioregional Ecosystems" as well as additional information and surveys conducted by the Queensland Herbarium. Such definitions were required following the proclamation of the Vegetation Management Act 1999 . Endangered regional ecosystems are "Category B Environmentally Sensitive Areas" in the Codes of Environmental Compliance for Exploration, Mineral Development and Mining Projects for Level 2 Code Compliant Activities. For exploration projects, activities involving machinery cannot be undertaken in, or within 500 metres of an ERE.

EPM 25779 has no environmentally sensitive areas identified and there is no major impediment to exploration.

9 Figure 1: Location Map

10 Other Environmentally Sensitive Areas

There are no other environmentally sensitive areas identified.

Cultural Heritage / Aboriginal Cultural Heritage / Heritage Sites

Initial searches have shown that there are no Aboriginal Cultural Heritage sites within this EPM, as recorded by the Department of Natural Resources and Water.

MLM understands that all significant Aboriginal cultural heritage in Queensland is protected under the Aboriginal Cultural Heritage Act 2003 . MLM takes all reasonable and practical measures to ensure that their activities do not harm Aboriginal Cultural Heritage, as required under the legislation.

11 Figure 2: EPA Environmentally Sensitive Areas

12 4. INDUSTRY BACKGROUND AND MARKET

Global graphite demand is increasing, particularly the high value high purity graphite being used in the Li-ion batteries used in the emerging electric vehicle production.

Currently there is negligible graphite production in Queensland with only small historic mining to reference. As graphite is basically the element of carbon in a crystalline flake form, the most common occurrence of economic graphite worldwide is within Proterozoic metamorphic terrains.

As graphite purity is the main driver for value, the inorganic contaminants (ash) within the graphite is significant and can affect value. Graphite value is variable with Amorphous graphite generally worth $500 / tonne, with Flake graphite double that and high purity Vein and Synthetic graphite worth several thousand dollars a tonne.

Metamorphic graphites are currently the most exploited natural graphites and have developed their own rule of thumb for quality and value which isn’t translatable to the other form. The main value driver is using flake (crystal) size as a proxy for purity, that is the larger the flake, the purer the graphite and hence its value.

Tabulated in Table 1 is a summary of the three main types of graphite and their relative abundance and value.

The Warrior deposit is unique in that it has characteristics of all three types of graphite due to it’s depositional style which makes it problematic to characterise in a traditional sense. Table 1: Graphite Types Type Amorphous Flake Crystalline / Vein Quality Low High Highest Occurrence Abundant common rare Size >37µm 100 to 177 µm >177µm Grade 20 – 40 % Cg 85 – 95 % Cg >90% Cg Purity 70 – 80 % C 85 – 95 % C 95 – 99 % C Price USD $600 - $800 /t $950 - $3000 /t > $3500 /t

5. TENURE

The tenement holder is Touchstone Resources Pty Ltd a 100% owned subsidiary of Metallica Minerals Ltd (ASX Code MLM). Esmeralda West comprises 54 Sub Blocks and details of which are tabulated in Table 2 Table 2: Sub blocks in EPM BLOCK BLOCK SUB-BLOCKS TOTAL NUMBER NORM 2426 N,O,P,R,S,T,U,W,X,Y,Z 11 NORM 2427 V,W,X,Y,Z 5 NORM 2428 R,V,W 3 NORM 2498 C,D,E,H,J,K,N,O,P 9 NORM 2499 A,B,C,D,E,F,G,H,J,K,L,M,N,O,P,R,S,T,U,X,Y,Z 22 NORM 2500 A,B,Q,V 4 Total 54

Tenement restrictions

There are no tenement restrictions identified.

Relinquished Sub Blocks

No Sub Blocks were relinquished within the first year of tenure.

Native Title

The relevant Native Title Parties are the Tagalaka People #2 Tagalaka Aboriginal Corporation RNTBC (Registered Native Title Claimant) QCD2012/013 (Native Title Tribunal Number) QUD6020/2001 (Federal Court Number)

Pursuant to s 17.1 of the Native Title Protection Conditions, the first year’s annual Administration fee of $1,211 was paid to The Tagalaka Aboriginal Corporation RNTBC in February 2016

Figure 3: Sub Block Location Map

15 6. GEOLOGICAL SUMMARY

Regional Located within the Georgetown Inlier in Norther Queensland, the project areas cover the Proterozoic Croydon Province which predominantly comprises the Croydon Volcanics and the Esmeralda Supersuite. The Esmeralda Supersuite Granites contain unusually abundant graphite (~2%). As the interpreted Esmeralda Supersuite is concealed between Cainozoic and Mesozoic sediments to the west, detailed investigations of the geology is limited to the eastern areas of the region.

The Esmeralda Supersuite has traditionally been categorised as an S-Type granites including the targeted Esmeralda Granite. The Esmeralda Granite (GSQ Record 1997/1) is a coarse grained biotite granite containing inclusions of graphite and xenoliths of graphitic meta-sedimentary rocks. More recently in 2002 Geoscience Australia has proposed that the Esmeralda Granite could potentially be actually an I- Type granite based on the hypothesis that the abundant graphite has reduced the oxidation state of the granite where it assimilates with the country rock to that of a S- Type granite. Other I-Type features of the granites is the presence of magnetite which demonstrates an oxidised nature to the granite. Geoscience Australia even categorised the Esmeralda granite as a Hiltaba Type granite highly prospective for gold. As only the granite margins are exposed in outcrop and therefore the only areas studied, the original source rocks could be a combination of lithology’s.

Mackenzie (1988) noted that “parts of the granite are extremely rich in graphite,” observing at Croydon tabular zones 120m thick and several kilometres long are packed with graphitic metasedimentary enclaves and masses of almost pure graphite set in a matrix of intensely hydrothermally altered granite.

Table 3: Geological Sequence in the North Western Georgetown Inlier UNIT AGE LITHOLOGY Quaternary Sand, gravel, silt & mud – alluvial and channel deposits Tertiary-Quaternary Residual and alluvial sands, gravels, silt and soil Tertiary-Quaternary Ferricrete, alluvium and colluvium Wallumbulla Cretaceous Sandstone and mudstone Formation Gilbert River Jurassic-Cretaceous Dominantly sandstones, lesser finer clastics Formation Eulo Queen Group Jurassic Sandstones and siltstones and minor conglomerates Permian Rhyolites, local andesites and granodiorites Inorunie Group Mid to Late Proterozoic Dominantly sandstones and orthoquartzites, minor siltstones and mudstones Esmeralda Granite Middle Proterozoic Dominantly biotite granites, some with (& minor granites) muscovite, garnet Croydon Volcanic Middle Proterozoic Dominantly rhyolites and dacites, minor Group sediments and andesites Forest Home Middle Proterozoic Biotite trondhjemite Trondhjemite Langlovale Group Middle Proterozoic Sandstone overlain by finer clastics Etheridge Group Middle Proterozoic Dominantly fine clastics including carbonaceous shales

Local Geology

The entire Warrior tenement is concealed under Cainozoic and Mesozoic cover sequences and is therefore relatively unknown with the only data available from interpretation of geophysical data and some water bore logs and drill core from reconnaissance drill holes. Basement within the application area and the area is currently mapped as “unknown basement”. This basement is currently interpreted to be the Esmeralda Supersuite granites.

The target area isn’t readily identifiable from the geological map, but it’s located west of an interpreted Early Permian Gabbro. Figure 5 shows the basement geology of the project area with only major units outlined based on magnetic interpretation and some drill core data. Most of the application area is mapped as “Unknown Basement”, with minor coverage of Early Permian Gabbro and Mesoproterozoic Granites.

Sub surface geological maps have been prepared by the department for the 1:100,000 Prospect 7360 Map Sheet (see Figure 4), and due to limiting factors such as reliance on drill hole data and geophysics, detail is poor.

Figure 4: EPM 25779 Geology

18 Mineralisation Graphitic granite is interpreted to be the remnants of predominantly assimilated carbonaceous sediment protolith. Figure 5: Graphite in Core Magmatic assimilation and differentiation appears to have concentrated residual carbon in possible cupola structures in the roof sequence the Esmeralda Granite. Subsequent reworking and hydrothermal alteration have resulted in exotic graphite granites with xenoliths of remnant protolith and aggregations of hydrothermal graphite into blebs.

Mineralisation appears to be consistent and pervasive within the graphitic granite unit and aerially large.

7. PREVIOUS EXPLORATION

Summary As the entire tenement is covered by Mesozoic and Cainozoic cover, the area was not significantly prospected until the 1970s. The geology of the area was relatively unknown other than a few drill cuttings noted in water bore drillers logs. The nearby Croydon Goldfields (70km to the north) would have attracted prospectors to the area, but it wasn’t until 1971 when modern exploration commenced with Ford, Bacon & Davis followed up a very high fluorine anomaly noted in groundwater from station bores. The availability of geophysical techniques such as aero-magnetics followed and the ability to define potential targets initiated exploration drilling through the cover.

Historic drilling generally targeted magnetic anomalies such as magnetic and in 2006, Metallica Minerals conducted the first aerial electromagnetic survey to target potential massive sulphide conductors.

The magnetic image in Figure 6 reveals significantly more detail than the basement geology map. The Warrior project area is at the northern end of the tenement and the coincident EM anomaly highlights where the 2006 MLM drilling occurred. This magnetic anomaly can be seen in the magnetic image an east west trend of subtle magnetic highs with historic drill holes drilled along it. At the southern end of the tenement is the Prospect Bore Gabbro anomaly that has had some historic drilling completed.

Table 5 summarises work completed by the different companies exploring in the region.

Figure 6: Warrior Magnetics, EM & Historic Drilling

Details of past exploration are summarized in Table 4. Table 4: Warrior Previous Exploration EPM(s) Company CRs Dates Notes

953 & Ford, Bacon & 3957, Jul 1971 These tenements were part of a large group of 954 Davis P Inc 3960, to Apr tenements acquired to look for the source of the 4445 1973 enigmatic regional fluorine anomaly of 32 ppm within the groundwater at the base of the Mesozoic cover. FBD wanted to investigate the source of this fluorine as it could be associated with economic mineralisation. FBD drilled four (4) BQ core holes proximal to the Nara Bore on Prospect Station looking for mineralisation to explain the fluorine anomaly. All holes intersected quartz porphyry with varying degrees of alteration. The source of the Fluorine was hypothesized but never explained. Analysis of the drill core indicated it was anomalous in tantalum and niobium 2872, Strategic 9684, Feb In 1981 EPMS 2872 & 3647 were granted to Strategic 4429, Metals Corp 10629, 1981 to Metals Corporation (Strategic) who followed up the 4785 & Pty Ltd 11197, Feb tantalum-niobium anomaly at Prospect (Nara) Bore 4786 (Initially, then 11514, 1987 and drilled 2 NQ core holes to test the tantalum- JV with) 12650, niobium anomaly. The tantalum-niobium anomaly Golden 12976, was not repeated but Strategic did take the Plateau NL 13387, opportunity to do a ground magnetic study in the area 14168, and identified a magnetic high 600m away. This 15693, target was also known as Prospect Bore which can 16049, cause confusion.

21 EPM(s) Company CRs Dates Notes

In 1982 Strategic drilled two percussion holes (PB1 & PB2) into the magnetic target with only PB2 successfully targeting the Proterozoic basement. The magnetic high was explained by a titano-magnetite layered gabbro which with a reported intersected a 98m interval averaging 15% TiO 2. (CR 11514) In 1983 a major aeromagnetic survey was flown as well as a Landsat imagery interpretation which produced several anomalies marked C for carbonatite, K for kimberlite, G for gabbro. In 1984 the ground magnetics were completed over the C2 anomaly was drilled and intersected an unmineralised gabbro. EPM 4429 was added in 1986 and an additional 7 holes were completed with a failed attempt to re-drill the C2 target. No kimberlites or Carbonatites were intersected. EPMs 4785 & 4786 were added in 1987. All sub- blocks were then amalgamated in 1987 into EPM 4853. 3647 Strategic 13387, May Overlapped northern portion of the Warrior Tenement Metals Corp 14693, 1984 to and tenure. EPMs 2872 & 3647 were initially acquired Pty Ltd 16050, Aug to evaluate tantalum-niobium anomalies. These (Initially, then 16051, 1987 tenements were explored together and work JV with) 16052, completed is described above in EPM 2872. Golden 16663, Plateau NL 16664 3805 Strategic 14574, Sep Magnetic results from an adjacent tenements Metals Corp 14747 1984 to indicated potential targets. The magnetic targets were Pty Ltd Aug re-assessed following drilling in the nearby tenements 1985 and the targets were downgraded. 3806 Strategic 14531, Sep Magnetic results from an adjacent tenement indicated Metals Corp 14746 1984 to that a potential interpreted carbonatite extended into Pty Ltd Aug EPM 3805 from the west. Only field work completed 1985 (reported) was general reconnaissance for potential drilling activities. Drilling of that target (C2) identified a (layered?) gabbro and no further work was completed. 4853 Strategic 17174, Aug EPM 4853 was an extraordinarily large EPM covering Metals Corp 21053 1987 to all of the Warrior project area and is an amalgamation Pty Ltd Aug and consolidation of several EPMs 2872, 3647, 4429, (Initially, then 1989 4785 & 4786. A large drilling program was completed JV with) with 26 open percussion holes (PB 1 to PB 26) Golden totalling 2,110m Holes PB 1 to PB 18 had diamond Plateau NL tails added for 933m of core. Hole PB2 was cored to test the high titanium results reported from the percussion hole (98m @ 15%) which was not repeated and it is interpreted to be a decimal point error on the original assay certificates Three (3) holes (PB16 to PB 18) were drilled along an east west structure of subtle magnetic highs and all intersected graphitic granite breccia (see Figure 4). These holes were part cored and qualitative estimates of 30% graphite over an interval of 20 to 40m is recorded. These core holes aren’t with the State Core Library for review . Strategic identified elevated PGE values in the gabbros and Au values associated with low temperature epithermal quartz-carbonate veins. Petrology work was completed predominantly on gabbroic holes, but not on the graphitic holes. Strategic & JV partners planned to continue follow

22 EPM(s) Company CRs Dates Notes

exploration but poor market conditions prevented the raising of capital to pursue. 8818, North Mining 24719, Jun In 1992 EPMs 8815 and 8836 which overlapped most 8817 & Ltd (nee 26170, 1992 to of Warrior were granted to Geopeko. Geopeko 8836 Geopeko) Jun conducted review of previous explorations and 1994 planned to do a gravity survey, gridded ground magnetic over known mag targets, Reconnaissance surface EM where drilling planned and reconnaissance stratigraphic drilling to test depth of basement and cause of magnetic anomalies and test structural interpretation. Initial work was a regional groundwater study conducted by CSIRO, re- interpretation of available aeromagnetics and completion of ground magnetics and gravity survey. Geopeko drilled 9 holes for 782m mainly to the south of the Warrior EPM without intersecting significant mineralisation. Geopeko concluded Cainozoic and Mesozoic sediments overlay Proterozoic Croydon Volcanics and Lower Proterozoic metamorphics. Groundwater chemistry was usual pathfinder tool along with air and ground magnetics. Gravity didn’t add anything to magnetics and drilling confirmed previous workers view of the geology. One (1) percussion hole was drilled along the Warrior east west structure into another subtle magnetic high. Geopeko logged the basement as Felsic Intrusive with 10 to 50% graphite, but did note it was probably the same graphitic breccia intersected in the Strategic / Golden Plateau JV holes. 10327 Western 27460, Oct 1994 WMC were targeting IOCG (Cu-Au) mineralisation in Mining 28953 to Oct the Proterozoic basement similar to the Eastern Corporation 1996 Succession of the Mt Isa Inlier. The EPM covered the Ltd western half of Warrior and extended south. Work completed included a thorough review of previous exploration and drilling results, ground reconnaissance, review of historic aeromagnetic data and further acquisition and a regional gravity survey. All the acquired data was reviewed and the coincident mag/gravity highs were considered to be mafic intrusives and not metasomatic magnetite indicative of large IOCG system like Olympic Dam. 14018 Rusina Mining Jul 2003 Ltd to Jan 2004 14023 Rusina Mining Jul 2003 Ltd to Jan 2004 14025 Rusina Mining Jul 2003 Ltd to Jan 2004 14406 Metallica 40386, Dec Metallica conducted a literature review and in 2004/05 Minerals Ltd 40880, 2004 to completed an airborne EM survey over the eastern 46261, Jan portion of the tenement. Three high priority targets 51286, 2009 were identified and in 2006 ground EM surveys were 56519, completed over the priority targets. Four RC holes were completed for 756m to test the anomalies. At the completion of drilling, all holes were temporarily cased with 40mm PVC for downhole EM surveys with results indicating drilling intersected the conductor. Holes RC-001, RC002 & RC002A intersected the Warrior EM anomaly and the anomaly was explained by highly graphitic granites. 23 EPM(s) Company CRs Dates Notes

15416 & Independence 57207, Mar “Empress Springs” was a JV between Independence 15414 Group Ltd 51954 2007 to Group and Avalon Minerals Ltd. Only EPM 15416 Jul 2009 was granted which is to the north of the Warrior area, buts it’s ‘sister’ application EPM(A) 15414 which overlaps the Warrior area was included within the CR report. Initial works completed by Avalon Minerals before grant of tenure consisted of open file exploration, concentrating on exploration potential and target generation from available geophysical data. Avalon Minerals commissioned SRK to undertake these initial desktop works which was a structural interpretation of aeromagnetic and gravity data combined with a historical exploration review to generate conceptual targets. Targets generated were tested within EPM 15416 with Soil MMI (Mobile Metallic Ions) and Leaf ‘Phyto’ geochemical sampling. Anomalies were identified using these techniques and a 3,500m bedrock drilling program was proposed and government funding available through the Collaborative Drilling Imitative was sought and approved. Subsequently the JV ended and Independence relinquished the tenement with no drilling completed. 19002 Oldfield June Exploration 2012 to Pty Ltd July 2014 EPM Independence Aug EPM forms the northern boundary of Warrior project 25210 Newsearch 2014 to and is currently being explored with no work reported Pty Ltd Current to date. The tenement is part of a package of EPM (Independence which overlap historic EPMs 15414 & 15416 which the Group Ltd) Independence Group re-applying for the area again.

24 8. TECHNICAL SUMMARY OF WORK COMPLETED IN THE FIRST YEAR

Compliance Statement for Program of Activities Touchstone Resources Pty Ltd has complied with the ‘Program of Activities’ it outlined in the EPM Application. Approved Work Program for Year 1 The following is the work program that has been approved by the department. Table 5: Year 1 Approved Program Activity 1 Review previous exploration activities data Completed & Ongoing 2 Geological & geophysical review Completed & Ongoing 3 Technical study Completed & Ongoing 4 Magnetic data reprocessing 5 Mapping 6 Magnetics survey (40 line-km) Open file data adequate 7 RC drilling (5 holes for 500m) 8 Diamond drilling (2 holes for 100m) Completed 9 Downhole EM 10 Mineralogy/petrology (50 samples) Completed

Data Review A review of historic exploration has been completed and a summary was outlined in Section 7 of this report. Details of historic regional drilling are tabulated in Appendix 1 summarising drill hole location, company, depth to basement and basement lithology.

Historic Percussion Drill Chips Chip trays containing percussion drill chips from the 2006 exploration program were located and reviewed. Hole RC002A showed graphitic mineralisation through the Proterozoic interval. Some samples were collected and despatched to Canada for some preliminary Mineral Liberation Analysis and petrography work (See Appendix 6).

As drill chips samples collected in chip trays are not truly representative of the sample interval, they were considered qualitative and indicative for review purposes.

25 Drilling A Core drilling was completed in September and Figure 7: Drill Rig October 2015 and two holes were completed for 309.8 meters. The aim of the program was to collect core samples from known graphite occurrences at historic holes RC-002A & PB18. These samples were submitted for geochemical analysis and preliminary metallurgical assessment. The first hole was designed to twin hole RC-002A which intersected significant (10 to 30%) crystalline graphite mineralisation in RC drilling in 2006. The second hole was also proposed to twin hole PB 18 drilled by Strategic in 1996 which intersected a “graphitic granite breccia.”

Drilling Contractor

Ryan Drilling was selected from a short list of 3 North Queensland drilling companies taking into account experience drilling in the remote areas of the Croydon region and drilling equipment suitable for accessing the proposed drill sites across sandy creek beds.

Field Logistics

The proposed drill sites were readily accessible but relatively remote and isolated. Access from the nearest town of Croydon was excellent with bitumen road for most of the way to Esmeralda Homestead. Dirt road were in good condition to the turnoff onto station tracks.

The station tracks on Esmeralda are generally very good, being regularly trafficked and generally flat.

The biggest access issues are the presence of braided rivers and creeks, with multiple channels, sandy creek beds and steep creek banks. Access tracks across these creeks needed to be well considered with its construction and levelled and compacted to minimise the likelihood of bogging.

26 Access Tracks & Drill Pad Preparation

The landholder had been retained to refurbish access tracks, clear drill pads and excavate drill sumps. The landholder utilised a front end loader. There was problems excavating sumps, as the top 1m was a sandy soil, but below that was a cemented sandstone resulting in larger and shallower drill sumps.

Accommodation

The drill sites were a two (2) hour drive from the nearest town of Croydon, and one (1) hour from the Esmeralda homestead which was considered too far for daily commuting.

A camp was established near a small farm dam near the Rowe 3 Bore about 2 to 3 kilometres from the drill holes. The location was ideal as all grass was removed by the cattle which reduced the hazard of uncontrolled grass fires prevalent in the region in the spring months.

Drill Hole Details

Figure 8: Drill Hole Plan 1

1 For MLM Corporate purposes, WD002 which was a twin of RC002, was renamed WD001 and WD003 was renamed WD002 for ASX reporting.

Table 6: Drill Hole Details

Total Interpreted Mineralised Zone Drill Easting 2 Northing 1 Depth Dip Hole (MGA) (MGA) From To Interval (m) (m) (m) (m) WD002 628,395 7,918,508 189.4 -90° 68 189.4 120 WD003 627,238 7,918,957 120.4 -90° 71.9 120.4 48.5 Total 309.8 168.5

Hole WD002

Hole WD002 was collared next to historic hole RC-002A and the 59.6m of cover sequence was mostly cored. All holes were drilled vertically to ensure the likelihood of pre-collar collapse was reduced. After each 3m core run of HQ3, 3m of HWT casing was reamed in behind the HQ strings to stabilise the hole as pre-collar collapse was a known problems highlighted in historic drilling reports. Initially the pre-collar was to be rotary drilled with a blade bit, but the drill rig didn’t have the appropriate gear available. As the pre-collar was never planned to be cored, the resultant core was an added bonus, but recovery was neglected in pursuit of fast penetration. Core recovery was probably 70% from 15.4 when rotary drilling was abandoned. The cover sequence of the mottled and laterised Quaternary sands and Tertiary sediments, had alternating porous and non- porous horizons and different strengths observed.

At 39.5m a grey coloured siltstone with thin blebby sandstone interbeds was intersected and similar in texture and facies seen in Jurassic sequences elsewhere. This was interpreted to be the Gilbert River Formation. These siltstones were occasionally finer grained and appeared carbonaceous. Additionally the facies also graded into abrasive sandstones and grits.

2 Preliminary results as determined by a handheld GPS

28 The granite basement (target) was intersected at 59.6m depth and the HWT casing was reamed to a final depth of 60m.

Initially drilling was with a HQ3 as there was concern that the relative hardness of the hard silicates of the granite and the soft nature of the graphite might be difficult to core and get good recovery. Once the weathered (decomposed) granite was drilled, and fresh granite intersected at 70m, there was none of the expected problems and rock quality from then on was excellent with a high RQD.

The silicates formed a hard matrix and the soft graphite occurred as clots/blebs within the matrix. The drilling averaged 30m of core a day whilst drilling and 100% recovery once in fresh rock.

The drill hole was arbitrarily terminated at 189.4 in grey granite similar in texture to outcropping Esmeralda Granites observed in the region. Graphite mineralisation was still present in core, and a decision was to abandon the hole to allow time and budget to complete the second hole. At the end of the hole all but the bottom 3 lengths of HWT casing was not recovered. It is suspected a thread fitting failed when the rig ‘pulled’ the casing. The lost rods were abandoned as the time, expense and the likelihood of failure didn’t warrant the ‘’fishing’’ required.

Hole WD003

Proposed hole W2 was designed to twin historic hole PB18 drilled in 1987. Locating the remnant drill pad and collar of PB 18 proved problematic as there was no evidence of drilling within 50m of the estimated coordinates. Evidence of flooding and fire had obliterated any remnants. The proposed collar was located within a braided creek system which made heavy vehicle access difficult due the necessity of traversing soft sand.

After failing to find the original collar, and difficult ground conditions on and around the estimated collar location, it was decided to relocate the collar of proposed hole W2 150m to the north side of ”Sandy Creek” where access was better. Like WD002, the hole was pre-collared using HQ3 coring due to the drillers lack of appropriate equipment for rotary blade drilling.

29 Drilling of the hole was very similar to WD002 and very similar lithology’s were intersected.

The hole was completed at 120.4m when the grey graphitic granite transitioned into a coarse pink coloured granite.

Hole Completion

At cessation of drilling, both holes were grouted with concrete and left for rehabilitation.

Figure 9: Rowe Bore Camp

30 Core Handling Initially Upon retrieval of the core barrel, core was be pumped into ‘splits’ where it was measured up and reconciled for any core loss on a ‘Recovery’ sheet. Core loss can then be attributed to core being dropped from the bottom of the barrel or in areas of obvious fracturing. Figure 10: Core Handling Once the core was recovered then it was measured and marked with permanent meter marks for geological logging.

As the core quality was better than anticipated, the core was transported to a temporary core processing facility at camp for marking up, photography and logging.

The core was then be placed into correctly marked and identified core trays for transport and storage. As graphite and granite are relatively unreactive, and a lack of sulphides, it was considered appropriate there be no special storage requirements.

Core Transport

As the drill site is remote, core was loaded and secured to the Project Geologists light vehicle and carefully driven back to Terrasearch in Townsville for temporary storage and processing.

Figure 11: Core Transport

31 Core Cutting

Terrasearch have fully equipped facilities with core saws and trained staff for processing of core. The Project Geologist identified intervals and Terrasearch personnel ½ cored the core for analysis. Samples were bagged and delivered to SGS Townsville for geochemical analysis.

Core Logging All drill core was logged geologically, and had specific gravity measurements estimated as well as magnetic susceptibility and conductivity.

Geological Geological logging was completed by a geologist on the core at a temporary core processing location at camp. Logging sheets were based on logging sheets used historically at Croydon, designed to capture lithology, alteration and graphite percentages. A summary log of main geological units is detailed below in Table 6, with full English Logs in the Appendices. Table 7: Summary Drill Log Graphite From To Int Strat Rock Type Comment (%) WD02 Sandstone/ 0 15.4 15.4 Quaternary Sandy young cover sequence Claystone Mottled and Laterised horizon, Tertiary/ Sandstone/ 15.4 39.5 24.1 interbedded porous and non- Cretaceous Claystone porous horizons Siltstone/ Unconformable cover 39.5 59.6 20.1 Jurassic Sandstone sequence Graphitic Chlorite Altered with 59.6 73.8 14.2 Proterozoic >5 Granite BX weathering affects Graphitic Fresh Graphitic Mineralised 73.8 97 23.2 Proterozoic 10 Granite BX Zone Gradational change where Graphitic 97 131.3 34.3 Proterozoic 5 graphitic blebs/clots change to Granite BX MS xenoliths Granite More meta-sediment xenoliths 131.3 158.3 27 Proterozoic <5 Breccia and chlorite/epidote alteration Granite 158.3 189.4 31.1 Proterozoic <5 Siliceous alteration Breccia WD03 Siltstone/ Unconformable cover 63.4 71.9 8.5 Jurassic 0 Sandstone sequence Graphitic 71.9 90.2 18.3 Proterozoic 10 Paleo weathering affects Granite BX Graphitic Fresh Graphitic Mineralised 90.2 92.72 2.52 Proterozoic 10 Granite BX Zone Graphitic More meta-sedimentary 92.72 99.9 7.18 Proterozoic 5 Granite BX xenoliths Granite Mixing Zone between granite 99.9 104.6 4.7 Proterozoic <5 Breccia and granite breccia Crystalline massive granite 104.6 120.4 15.8 Proterozoic Granite <2 with numerous xenoliths

Magnetic Susceptibility The Warrior Prospect was originally identified as a coincident magnetic high and EM anomaly. The drill core was logged using a hand held magnetic susceptibility meter on one piece of core every one meter with details tabulated in the Appendices. Petrology indicated the graphite appears to be associated with some opaque oxide (probably magnetite) with crystal shapes suggestive of former pyrite. The magnetite also forms in micro-cracks along grain boundaries in the rock.

With magnetite associated with the graphite, magnetics can be a valuable tool to target graphitic mineralisation.

This is also confirmed by the historic drilling completed by Strategic, where drill holes PB 16, 17 & 18 targeted magnetic highs and all intersected what they logged as “graphitic breccia. “ Specific Gravity Along with magnetic susceptibility, core was also quantified with dry and wet weight measurements which were used to calculate a Specific Gravity and are tabulated in the Appendices. The specific gravity was relatively constant between 2.6 & 2.7 and reflected the massive nature of the granite. Of interest was a correlation between lower SG (<2.5) and lower Total Sulphur between the granite roof (60m) and 87m. This appears to reflect the effects of paleo weathering of the granite before the inundation of the Mesozoic.

Petrology

Six representative sliced core samples ranging in size from 4cm-12cm in length were collected from the graphite mineralised zone from both drill holes and submitted to Geochempet Services based in Clontarf, Queensland. Petrographic investigation (using polished thin section under microscope) was then undertaken to define the mineralogy and interpretation of the graphite mineralisation and alteration. Table 6 provides a breakdown on the petrographic study’s key observations.

The host rock of the graphite mineralisation is predominantly light grey, fine to medium grained porphyritic biotite granite which contains darker partly rounded altered blebs (having appearance of xenoliths) along with clots or blebs of graphite up to 2cm. Unusually, this altered graphitic granite appears to have assimilated variable amounts

33 of graphite (possibly after altered and sheared carbonaceous xenoliths) and as abundant clots and grains predominantly of reactivated and/or remobilised graphite from pervasive hydrothermal alteration.

Table 8: Petrology Petrology WD001 WD001 WD 001 WD002 WD002 WD002 Sample 75.0m 88.8m 110.5m 76.62m 87.5m 88.58m Name Simple Altered Altered Altered Altered Altered Medium Grey Rock Graphitic Graphitic Graphitic Graphitic Graphitic granite, strongly description Granite Granite Granite Granite Granite altered brecciated – foliated graphitic recrystallised rock of likely of metamorphic origin Mineral % * Quartz 25-30% 25-30% 25-30% 25-30% 25-30% 10-15% K-Feldspar 25-35% 25-35% 25-35% 25-35% 25-35% - Albite (Na - - - - - 15-20% Feldspar) Graphite 5-10% 5-10% 5-10 % 10-20% 15-20% 25-35% ** Sericite 15-20% 15-20% 15-20% 20-30% 20-30% - Biotite 10-15% 3-5% 3-5% 3-5% <1% 10-15% Epidote 3-5% 3-5% 3-5% 3-5% - -% Chlorite 1-2% 1-2% 1-2% 1-2% 3-5% 10-15% Magnetite <1% 3-5% 3-5% 1-2% - - Apatite <1% <1% <1% <1% <1% - Opaque <1% <1% <1% <1% Oxide (Magnetite and/or Ilmenite) Cordierite - - - - - 15-20% Notes: - * Visual modal % estimate ** abundant graphite veins, clots and Schlieren textures *** Italiced noted differences

Generalised Hydrothermal Alteration Assemblage • Major alteration: Graphite and Sericite • Medium to weak alteration: Biotite-Chlorite-Epidote-Magnetite +/- Cordierite Commonly former Plagioclase feldspar has completely altered to graphite and sericite. Former mafic silicates are now altered to graphite, biotite, chlorite and epidote – now seen as dark blebs or clots.

Graphite Mineralisation origin There appears at least two modes of generation of the graphite mineralisation: 1. Assimilated xenoliths of carbonaceous meta-sediments; and 2. Hydrothermal-structural impacts to produce secondary or reactivated enrichment of the graphite including hydrothermal veining.

Petrologist’s Comments;

In total, eight exploration sample were received at Geochempet Services on 10/11/15; one is a rock sample (121038) and the remainder are drill core sample from two drill holes (WD002 and WD003) from the Croydon area. The bulk of the samples are considered to be fine to medium-grained, porphyritic, biotite granite (using both IUGS and British/Australian classification systems) composed of orthoclase, Plagioclase, quartz, biotite and opaque oxides; they are overlain unconformably by Jurassic sediments. Sample WD003 at 111.40-111.45m is considered to represent the “normal granite” with slight levels of alteration.

Samples WD002 at 75.00-75.06m WD002 at 88.80-88.90m, WD002 at 110.5m, WD003 at 76.62-76.66m and WD003 at 87.50-87.62 m is interpreted to represent the “graphitic granite”, an altered and sheared granite. The granite is unusual in that it contains graphite which is suspected to be sourced from carbonaceous shale protolith in the surrounding country rock. This altered and sheared granite is interpreted to be from the Proterozoic Esmeralda Granite Supersuite which appears to have assimilated graphitic enclaves/xenoliths though to be derived from carbonaceous meta-sediments. Samples WD002 at 88.80-88.90m and WD003 at 87.50-87.62 m both contains larger corroded xenoliths of altered and sheared material that display schlieren, lenses and veins of reactivated graphite which indicates a much more complex situation for the enrichment of graphite into clots.

Apparently related, but more altered, recrystallized, metamorphic rock (see sample WD003 88.58-88.62m) has been substantially modified by reactivated graphite and biotite replacement by probably hydrothermal and/or structural effects which has significantly changed its final composition to an altered assemblage of graphite- epidote-biotite-sericite and possibly some cordierite. The alteration is suspected to include magnetite obscured by graphite.

The micro-granite is interpreted to be from the Esmeralda Granite Supersuite which has assimilated abundant graphitic xenoliths, though to be derived from carbonaceous meta-sediments. It is thought to represent S-type granitic rock and to have been probably emplaced in a mesozonal setting, in this case, into the Croydon Volcanic Group.

The alteration in the Croydon Province has been linked to Proterozoic volcanism as it is a considerable distance from Palaeozoic igneous rocks, but other studies have suggested a Permo-Carboniferous date for alteration. Gold deposits in the Croydon field occur in the volcanics but the bulk of the gold was produced from deposits in a narrow belt of biotite granite. The lodes are mainly located in quartz reefs in sheared graphitic granite which contained graphite, arsenopyrite, pyrite, galena, sphalerite and traces of gold, silver and copper.

Some of more altered, recrystallized, micro-granitic rock has been substantially modified by assimilating xenoliths of carbonaceous meta-sediments which has significantly changed its final composition to an altered assemblage of graphite- magnetite-biotite-chlorite-epidote-sericite and possibly some cordierite. There appears to be at least two mode of generation of graphite mineralisation (one within xenoliths of carbonaceous meta-sediments and the other appears to have occurred during hydrothermal-structural impacts). Thermal metamorphism of the xenoliths and quite altered and sheared has produced a complex mechanism of secondary enrichment of the graphite including hydrothermal veining. It has also altered pyrite in the original sediment to magnetite which is mixed into the graphitic clots along with scattered inclusions of the alteration minerals.

Geochemistry

All drill core was despatched to SGS in Townsville for core sample preparation where a subsample was split and samples were sent to SGS Perth for analysis. The following analysis was completed:

Table 9: Analysis Details Analysis SGS Code SGS Lower Upper Method Detection Detection Limit (%) Limit (%) Preparation PRP88 Carbonate Carbon CO3_C CSA02V 0.01 60 Non Carbonate Carbon NON CO3_C CSA02V 0.01 30 Graphitic Carbon Cg CSA05V 0.01 30 Total Carbon TC CSA06V 0.005 100 Total Sulphur TS CSA06V 0.005 40

No other elemental analysis was completed for precious or base metals as these holes are twins of historic holes and previously assayed. All results are detailed in the Appendices. As the project and data set is relatively new and small, no detailed geostatistics have been completed. Table 10 details some broad mineralisation zones using an arbitrary 3% Cg cut-off grade

Table 10: Graphitic Carbon Intervals Hole From Interval Cg (%) Cg (%) (m) (m) Average Cut off WD002 71 95 6.58 3 WD003 71.9 29.1 7.83 3 including 71.9 7.05 12.09 10

A review of results indicates that graphite mineralisation is continuous through the granite sequence and is pervasive in nature.

Preliminary Metallurgy

MLM completed preliminary metallurgical analysis on a mineralised composite of hole WD002. The entire mineralised intersection was composited and a series of metallurgical test works was completed to attain a high purity and recovery.

Metallurgy was considered to be an important early stage of exploration for graphite, as graphite recovery is important to determine before any economic analysis or assumptions can be made to warrant further exploration and drilling. Nagrom Laboratories based in Brisbane completed the test work and have reported and achieved a recovery and purity of _% using basic flotation and one caustic wash.

37 These results indicated that the graphite can be upgraded to desirable quality at minimal processing.

Details of the preliminary Metallurgy are available in Appendix 4.

Geological Model A geological model has yet to be developed for EPM 25779 as exploration is at the preliminary stage only. A conceptual model has been proposed and further work will be required

Resources & Reserves Not Applicable

Economic Potential of EPM 25779 Warrior

Graphite is an Industrial Mineral and as such there is no Benchmark price or transparent and open market from which to determine potential economics of a deposit and determine its resource without determining the quality of the graphite and potential market.

As there are no resource identified there is nothing to assess economic potential at this stage.

Hydrothermal graphite with the correct quality has an inherently high value which makes it an attractive exploration target.

Drilling results indicate that the mineralisation is relatively deep for open cut mining, but, significant thicknesses and continuity of mineralisation indicate a potentially low stripping ratio with respect to a larger resource.

38 9. PROPOSED EXPLORATION PROGRAMME FOR YEAR 2

The following table details the work program that has been approved by the department for year 2 Table 11: Year 2 Approved Program Activity Expenditure 1 Technical studies 2 Interpretation studies 3 Geological & geophysical Review 4 RC drilling (5 holes for 1,000m) $105,000 5 Diamond drilling (4 holes for 200m) 6 Downhole EM 7 Mineralogy/petrology (50 samples)

To meet the requirements, Touchstone has established a 800m grid over the Warrior prospect and is planning to complete a drilling program to find the full extent of the graphite mineralisation along the Warrior Structure within the permit. This will be a combination of RC and Diamond core drilling.

10. REFERENCES

1. Queensland QME QDEX Exploration Reports https://qeri.dme.qld.gov.au/qeri/controller/Home 2. SHERATON, J.W., LABONNE, B., 1978: Petrology & Geochemistry of Acid Igneous Rocks of North East Queensland, Bureau of Mineral Resources Bulletin 169. 3. MACKENZIE, D.E., HENDERSON, G.A.M, WARNICK, J.V. & BAIN, J.H.C 1985: Geology of the Croydon Region, Queensland, 1:250 000 Geological Special Map. Bureau of Mineral Resources, Canberra. 4. DENARO, T.J., WHITNALL, I.W., BAIN, J.H.C. & MACKENZIE, D.E. 1997: Mineral Resources Assessment Georgetown – Croydon. Queensland Minerals & Energy Review Series 1997. 5. BUDD, ANTHONY R., LESLEY LESLEY A.I. & BASTRAKOVA, IRINA V., 2001: The Metallogenic Potential of Australian Proterozoic Granites, Geoscience Australia Record 2001/12. 6. WALLIS, D.S., DRAPER, J.J. & DENATO, T,J., 1992: Palaeo- and Mesoproterozoic Mineral Deposits in Queensland. AGSO Journal of Australian Geology & Geophysics, 7(3), 47-59. 7. WARNICK, J., 1985: Mines & Mineral Deposits of the Croydon Region. GSQ Record 1985/42 8. Van ECK, M., 1990: Authorities to Prospect 5091M, 5200M, 5362M & 5716M Combined Exploration Report for the Twelve Months Ended 31 st December 1989. Central Coast Exploration NL. (QDEX Report CR 22839) 9. MACKENZIE, D.E., 1988: Graphite-bearing ignimbrites and granites at Croydon, Queensland, and their relationship to gold mineralisation. BMR Research Newsletter, 8, 1-2. 10. DENARO, T.J. & MORWOOD, D.A., 1997: Geology, Mineralisation and Company Exploration in the Croydon 1:250,000 and Gilbert River and Esmeralda 1:100,000 Sheet Areas, North Queensland. GSQ Geological Record 1997/1 11. DENARO, T.J., 2011: A Review of Queensland’s Non-Energy Mineral Deposits & Resources. GSQ Record 2011/10 12. WHITEHOUSE, J., 2007: Industrial Minerals Opportunities in New South Wales (Geology Bulletin 33) 13. ZENYATTA Ventures Ltd (TSX.V: ZEN) : http://www.zenyatta.ca 14. PLUMBAGO Refining Corporation http://www.plumbagographite.com

Table 12: EPMs 25779 Warrior Historic Exploration Report Permit CR Report Title Type EPMs 3957 PROGRESS REPORT ON A-P 952M, CROYDON AREA, QLD. 953 & 3960 PROGRESS REPORT ON A-P 952M, CROYDON AREA, QLD. 954 4445 A-P 940M, 952M, 953M, 954M, 1063M, 1067M, 1068M, CROYDON

AREA-PROGRESS REPORT 19.01.73. EPMs 9684 HALF YEARLY REPORT TO 01.08.81, A-P 2872M, CROYDON, N. 6MTH 2872, QLD. 4429, 10629 HALF YEARLY REPORT TO 1.02.82, A-P 2872M CROYDON, N. 6MTH 4785 & QLD. 4786 11197 HALF YEARLY REPORT, 2.02.82-1.08.82, A-P 2872M, CROYDON, 6MTH N. QLD. 11514 HALF YEARLY REPORT, 2.08.82-1.02.83, A-P 2872M, CROYDON, 6MTH N. QLD. 12650 HALF YEARLY REPORT, 2.02.83-1.08.83, A-P 2872M, CROYDON, 6MTH N. QLD. 12976 HALF YEARLY REPORT 2.08.83-1.02.84, A-P 2872M, CROYDON, ANNUAL N. QLD. 14168 HALF YEARLY REPORT, A-P 2872M, 2.02.84-1.08.84, CROYDON, 6MTH N. QLD. 15693 HALF YEARLY REPORT 2.08.84-1.02.85, A-P 2872M, CROYDON, 6MTH N. QLD, (COY NO. 4011/47/LR/LK). 16049 PROSPECT BORE PROJECT, HALF YEARLY REPORT 02.02.86- 6MTH 01.08.86, A-P 2872M, CROYDON, N. QLD. EPM 13387 HALF YEARLY REPORT, 16.12.83-15.06.84, AP 3647M, 6MTH 3647 CROYDON, N. QLD, (4011/34). 14693 HALF YEARLY REPORT 16.6.84 TO 15.12.84, A-P 3647M, 6MTH CROYDON, NORTH QLD. 16050 HALF YEARLY REPORT 16.06.85-15.12.85, A-P 3647M, CROYDON 6MTH AREA. 16051 PROSPECT BORE PROJECT, HALF YEARLY REPORT 16.12.85- 6MTH 15.06.86, A-P 3647M, CROYDON, N. QLD. 16052 REPORT ON DRILLING ON A'S - P 2872M & 3647M, CROYDON, N. ANNUAL QLD (REPORT NO. A/189). 16663 SIX MONTHLY REPORTS FOR: A-P 3647M, FOR PERIOD 11.06.86-15.12.86: A-P 2872M, FOR PERIOD 02.08.87-01.02.87: A- 6MTH P 4429M, FOR PERIOD 25.09.86- 24.03.87. 16664 FINAL REPORT FOR A TO P 2872M, 3647M, 4429M, 4785M & FINAL 4786M, FEBRUARY 1987-AUGUST 1987. EPM 14574 HALF YEARLY REPORT, 17.08.84-16.02.85, A-P 3805M, 6MTH 3805 CROYDON, N. QLD. 14747 HALF YEARLY AND FINAL RELINQUISHMENT REPORT, A-P BRS 3805M CROYDON, NORTH QLD. EPM 14531 HALF YEARLY REPORT, 17.08.84-16.02.85, A-P 3806M, 6MTH 3806 CROYDON, N. QLD. 14746 HALF YEARLY AND FINAL RELINQUISHMENT REPORT A-P 6MTH 3806M CROYDON, NORTH QLD. EPM 17174 HALF-YEARLY REPORT ON A-P 4853M, PROSPECT BORE 6MTH 4853 PROJECT, CROYDON, QLD, PERIOD 06.08.87-06.02.88. 21053 A-P 4853M, FINAL AND ANNUAL REPORT FINAL EPMs 24719 EPM 8815 (CLARA NORTH), 8817 (CLARA SOUTH), 8836 (CLARA 6MTH 8815, CENTRAL), ANNUAL REPORT FOR PERIOD ENDING 21/6/93 8817 & 26170 EPM 8815 (CLARA NORTH), 8817 (CLARA SOUTH), 8836 (CLARA 6MTH & 8836 CENTRAL), ANNUAL & FINAL REPORT FOR PERIOD ENDING FINAL 21/6/94 EPM 27460 EPM 10327, CLARA RIVER, ANNUAL REPORT FOR THE PERIOD 6MTH 10327 31/10/94 TO 30/10/95 28953 EPM 10327, CLARA RIVER, ANNUAL AND FINAL REPORT FOR FINAL THE PERIOD 31/10/95 TO 30/10/96

41 Report Permit CR Report Title Type EPMs NA No Reports 10535, 14018, 14023, 14025 EPM 40386 EPM 14406, PROSPECT PROJECT, ANNUAL REPORT FOR THE ANNUAL 14406 FIRST YEAR OF TENURE 12/12/04 TO 11/12/05 40880 EPM 14406, PROSPECT, PARTIAL RELINQUISHMENT REPORT RELINQ FOR PERIOD ENDING 12/12/05 46261 EPM 14406, PROSPECT, ANNUAL REPORT FOR PERIOD 12/12/05 ANNUAL TO 11/12/06 51286 EPM 14406, PROSPECT, ANNUAL REPORT FOR THE YEAR ANNUAL 12/12/06 TO 11/12/07 56519 EPM 14406, PROSPECT PROJECT, ANNUAL/FINAL REPORT FOR ANNUAL PERIOD 12/12/07 TO 11/12/08 56519 EPM 14406, PROSPECT PROJECT, ANNUAL/FINAL REPORT FOR FINAL PERIOD 12/12/07 TO 11/12/08 EPMs 51954 EPM 15416, EMPRESS SPRINGS, ANNUAL REPORT FOR THE PE ANNUAL 15414, RIOD 2/3/07 TO 1/3/08 15416 57207 EPM 15416, ANNUAL/FINAL REPORT FOR PERIOD 2/3/08 TO 1/3/ ANNUAL 09 & FINAL

42 11. ATTACHMENTS

Attachment 1

Drill Hole Plan 1:50,000

12. APPENDICES

44 TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 1

Warrior Historic Drilling

Table 13: Warrior Historic Drilling Details Company Year Easting Northing TD Dip / B’ment Hole ID CR Core Basement Lithology Drilled (MGA) (MGA) (m) Azi Depth Ford, FBD- 1971 3957 632186 7910365 34.1 0/-90° 8.2 25.3 Quartzite Bacon & DH1 Davis P Inc FBD- 1971 3957 632410 7910191 83.2 0/-90° 29.9 48.8 (granophyric) quartz porphyry DH2 FBD- 1971 3957 632353 7910171 133.7 0/-90° 64.6 49.1 Quartz porphyry DH3 FBD- 43.6 1971 3957 632208 7910108 78.2 067/-50° 37.3 Quartzite DH4 (58?) Strategic PRO- 1981 10629 632324 7910193 108.8 0/-90° 49 57 Quartzite Minerals DDH1 Corporation PRO- 1981 10629 632295 7910110 129.9 0/-90° 84.1 45.8 Quartzite Pty Ltd DDH2 PB1 180°/- 1982 11514 631837 7909950 24 0 >24 Unknown (1983) 60° PB2 1982 11514 631860 7909905 132 0/-90° 0 34 Gabbro (1983) 1984 C2/1 15693 0 0 136 0/-90° 0 96 Gabbro PB3 1986 16052 631860 7909924 100 0/-90° 0 35 Gabbro (1986) 1986 C1/1 16052 618115 7919236 156 0/-90° 0 126 Granitic Intrusive 1986 G2/1 16052 627623 7918197 84 0/-90° 0 60 Rhyolite ? 1986 G5/1 16052 629557 7916988 66 0/-90° 0 48 Gabbro 1986 K3/1 16052 616600 7924285 130 0/-90° 0 >130 Unknown Strategic 1987 PB1 17174 631677 7910413 159.75 0/-90° 109.95 42 Magnetite gabbro Minerals 1987 PB2 17174 631783 7910150 166.1 0/-90° 126.4 32 Gabbro Corporation 1987 PB3 17174 631545 7910176 179 0/-90° 126 40 Gabbro

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Company Year Easting Northing TD Dip / B’ment Hole ID CR Core Basement Lithology Drilled (MGA) (MGA) (m) Azi Depth Pty Ltd / 1987 PB4 17174 639458 7899235 68 0/-90° 18.4 42 Magnetite gabbro Golden 1987 PB5 17174 640939 7896236 115 0/-90° 30 79 Porphyritic felsic intrusive Plateau NL 1987 PB6 17174 640304 7896078 128 0/-90° 36.5 85 Magnetite gabbro Joint 1987 PB7 17174 639828 7895683 131 0/-90° 49 73 Sandstone Venture 1987 PB8 17174 641785 7894973 134 0/-90° 35.1 94 Magnetite gabbro 1987 PB9 17174 639485 7901393 101 0/-90° 18 77 Gabbro Gabbro + Porphyritic felsic 1987 PB10 17174 641258 7905183 125 0/-90° 32.5 89 intrusive 1987 PB11 17174 636733 7907154 118.2 0/-90° 24.6 55 Quartzite 1987 PB12 17174 627944 7912382 179 0/-90° 93.9 79 Gabbro 1987 PB13 17174 641098 7899920 94.75 0/-90° 17.75 72 Porphyritic felsic intrusive 1987 PB14 17174 641256 7896631 97 0/-90° 15 77 Porphyritic felsic intrusive 1987 PB15 17174 630778 7907807 110 0/-90° 32 78 Gabbro / pyroxenite 1987 PB16 17174 622141 7918953 143 0/-90° 45 95 Graphitic Breccia 1987 PB17 17174 623915 7918955 149 0/-90° 66 78 Graphitic Bre ccia 1987 PB18 17174 627252 7918801 128 0/-90° 55 69 Graphitic Breccia 1987 PB19 17174 643821 7893606 109.6 0/-90° 0 108 Graphitic felsic intrusive 1987 PB20 17174 643423 7891921 88.75 0/-90° 0 >89 Unknown 1987 PB21 17174 619493 7918159 98.2 0/-90° 0 98 Sandstone 1987 PB22 17174 631598 7907992 55.7 0/-90° 0 51 Quartz diorite 1987 PB23 17174 639457 7895394 86 0/-90° 0 79 Porphyritic granite 1987 PB24 17174 641916 7893737 101.4 0/-90° 0 95 Micaceous Shale 1987 PB25 17174 643450 7892763 94 0/-90° 0 ? Unknown 1987 PB26 17174 646465 7892632 84 0/-90° 0 77 Porphyritic granite Geopeko CLC.P- 1994 26170 630821 7907100 98 0/-90° 0 68 Gabbro (Peko S/1 Wallsend CLC.P- 1994 26170 631334 7906446 68 0/-90° 0 38 Gabbro Ltd) S/2 CLC.P- 1994 26170 632275 7907646 86 0/-90° 0 62 Gabbro S/3 CLN.P - 1994 26170 626090 7918760 90 0/-90° 0 70 Graphitic felsic Intrusive? S/1 2006 RC -001 46261 628308 7919000 131 352/-75° 0 62 Graphitic Granite 2006 RC -002 46261 628300 7918490 90 352/-75° 0 60 Graphitic Granite

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Company Year Easting Northing TD Dip / B’ment Hole ID CR Core Basement Lithology Drilled (MGA) (MGA) (m) Azi Depth RC - 2006 46261 628292 7918513 198 0/-90° 0 56 Graphitic Granite Metallica 002A Minerals 2006 RC-003 46261 633341 7906478 192 0/-90° 0 48 Quartzite Ltd (MLM) 2006 RC-004 46261 631500 7910550 175 0/-90° 0 0 0 Metallica 2015 WD002 TBA 628,395 7,918,508 189.4 0/-90° 189.4 59.6 Graphitic Granite Minerals 2015 WD003 TBA 627,238 7,918,957 120.4 0/-90° 120.4 71.9 Graphitic Granite Ltd (MLM)

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 2

Detailed Geological Logs

WD002 Interval Lithology Alteration Fro To Str Description / m at Comment Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other Type Rock Min 1 Min 2 Min 3 Colour Graphite % Grain Size Weathering 0 3 3 Sand Quartz White 0 Sand Extrem Y Quat Quaternary quartz e sands, poorly consolidated 3 3.2 0.2 Conglomer Clay White 0 Highly Y Quat Clayey sandstone ate with gravel fragments 3.2 5.4 2.2 Claystone Kaolin Quartz White 0 Highly Y Quat Clayey sandstone, laterised and limonite staining 5.4 6.1 0.7 Sandstone Quartz Kaolin White/ 0 Highly Y Quat Clayey Brown sandstone, laterised and limonite staining, competent 6.1 15.4 9.3 Core Loss - extra 3m drill rod counted accidently 15.4 17.9 2.5 Claystone Kaolin Quartz Limonit Orang 0 Highly Mottled Y Ter Laterised clayey e e/ sandstone, Brown mottled, alternating hard & soft bands 17.9 21.5 3.6 Claystone Kaolin Quartz Limonit Orang 0 Highly Mottled Y Ter Laterised clayey e e/ sandstone, Brown mottled, harder

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD002 Interval Lithology Alteration Fro To Str Description / m at Comment Type Rock Min 1 Min 2 Min 3 Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other than previous interval 21.5 23.6 2.1 Claystone Kaolin Quartz Limonit Orang 0 Highly Mottled Y Ter Laterised clayey e e/ sandstone, Brown mottled, softer than previous interval 23.6 24.9 1.3 Claystone Kaolin Quartz Limonit Brown 0 Highly Mottled Y Ter Brown Clayey e / sandstone Orang e 24.9 27.4 2.5 Claystone Kaolin Quartz Limonit White/ 0 Highly Mottled Y Ter Claystone e Orang e 27.4 29.2 1.8 Claystone Kaolin Quartz Limonit Orang 0 Highly Mottled Ter Sandy Claystone e e/ - Laterised Brown 29.2 32.4 3.2 Sandstone Quartz Kaolin Limonit Grey/ 0 Highly Mottled Ter Clayey Sandstone e Brown 32.4 32.9 0.5 Sandstone Ter

32.9 38.1 5.2 Sandstone Quartz Kaolin Limonit Orang 0 Modera Mottled Ter Laterised Clayey e e/ te Sandstone Brown 38.1 38.6 0.5 Sandstone Quartz Kaolin Limonit Grey/ 0 Modera Ter Laterised Clayey e Brown te Sandstone 38.6 39.3 0.7 Sandstone Quartz Kaolin Limonit Grey/ 0 Modera Ter Coarser e Brown te Sandstone, still Clayey 39.3 39.5 0.2 Sandstone Quartz Limoni Ter Coarse te Sandstone, marginal facies, base of Tertiary? 39.5 40.7 1.2 Siltstone Quartz Orang 0 Modera Laminat Jur Jurassic e/ te ed Sandstone, White laminated grey siltstone with

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD002 Interval Lithology Alteration Fro To Str Description / m at Comment Type Rock Min 1 Min 2 Min 3 Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other blebs of cross bedded sandstone 40.7 41.3 0.6 Siltstone Quartz Grey 0 Slightly Laminat Jur Laminated ed siltstone with carbonaceous (?) clays 41.3 41.6 0.3 Siltstone Quartz White 0 Slightly Jur Bleached Siltstone 41.6 42.3 0.7 Conglomer Quartz Orang 0 Modera Jur Coarse marginal ate e/ te facies Brown 42.3 42.4 0.1 Sandstone Quartz Grey 0 Slightly Y Jur Hard horizon

42.4 45.4 3 Jur Re-adjustment of hole depth as there was missing 3m rod between 6 & 15m 45.4 46 0.6 Sandstone Quartz Kaolin Brown 0 Sand Modera Y Jur Hard abrasive te sandstone, aquifer 46 48.4 2.4 Jur Core Loss

48.4 48.5 0.1 Sandstone Quartz Brown 0 Jur Sandstone grading to grey siltstone 48.5 49.9 1.4 Jur Core Loss

49.9 50 0.1 Siltstone Quartz Clay Grey 0 Slightly Laminat Y Jur Fine grey siltstone ed grading towards sandstone 50 51.4 1.4 Sandstone Quartz Limoni Brown 0 Slightly Jur Sandstone, te porous aquifer 51.4 53.4 2 Jur Core Loss

53.4 54.3 0.9 Sandstone Quartz Brown 0 >2m Slightly Gritty Jur Porous abrasive m sandstone

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

55.7 55.8 0.1 Siltstone Quartz Grey 0 Slightly Y Jur Siltstone with blebs of cross bedded sandstone 55.8 55.9 0.1 Sandstone Quartz Brown 0 Slightly Jur Porous abrasive sandstone 55.9 57.2 1.3 Siltstone Quartz Grey 0 Fresh Jur Mainly laminated siltstone, interbedded with thin sandstone layers 57.2 58.3 1.1 Sandstone Quartz Grey 0 >2 Fresh Gritty Jur Coarse mm Sandstone, looks like weathered decomposed granite, porous and gritty 58.3 59.6 1.3 Siltstone Quartz Kaolin Grey 0 Fresh Jur Siltstone with (?) blebs of cross bedded sandstone, Low energy deposition on contact 59.6 60 0.4 Granite Quartz Clay Grey Tr Y Y Tr Prot Decomposed granite, possibly colluvial 60 60.3 0.3 Granite Quartz Clay Chlorit Grey/ 2 Y Y Y Prot Decomposed e Clay Green granite, some chloritic/graphitic slickensides observed 60.3 61 0.7 Prot Core Loss

61 63.4 2.4 Granite Quartz Clay Grey/ Tr Modera Granitic Y Y Y Prot Decomposed Green te granite,

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD002 Interval Lithology Alteration Fro To Str Description / m at Comment Type Rock Min 1 Min 2 Min 3 Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other Plagioclase altered to clays, quartz grains visible 63.4 64 0.6 Granite Quartz Clay Chlorit Grey/ 2 Modera Granitic Y Y Y Prot Granite, vague e Clay Green te foliation, quartz grains up to 2mm 64 65.1 1.1 Granite Quartz Chlorit Smecti Grey/ 5 Slightly Granitic Y 20 Prot Chlorite replacing e Clay te Green % granite, weak foliation 65.1 66.1 1 Granite Quartz Chlorit Smecti Green 5- Slightly Breccia Y 30 Y Prot Breccia texture e Clay te / Grey 10 % becoming apparent, 10cm xenolith of graphite, chlorite after graphite 66.1 67.05 0.9 Micro- Quartz Plag Chlorit Grey/ 5 Fine Slightly Massive Y Y Y Tr Prot Xenolith of micro- 5 Granite e Clay Green granite (?) with calcite veining 67.05 67.9 0.8 Granite Quartz Chlorit Smecti Green 5 Slightly Breccia Y 30 Y Prot Weathered 5 e Clay te / Grey % granite breccia, chlorite replacing graphite 67.9 69.9 2 Granite Quartz Chlorit Smecti Green 5- Slightly Breccia Y 30 Y Prot chloritic graphitic e Clay te 10 % granite breccia, blebs of purer graphite 69.9 70.2 0.3 Granite Quartz Chlorit Smecti Green 5- Slightly Breccia Y 30 Y Y Prot Green chloritic e Clay te 10 granite with micro-granite (?) xenoliths 70.2 70.3 0.1 Granite Chlorite Quartz Smecti Green <5 Modera Shear Y 40 Y Prot Horizontal shear Clay te te zone ? 70.3 71.8 1.5 Granite Quartz Chlorit Plag Green 5- Slightly Breccia Y 30 Y Y Prot Chlorite e Clay 10 Alteration, fresh graphite blebs/clots,

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD002 Interval Lithology Alteration Fro To Str Description / m at Comment Type Rock Min 1 Min 2 Min 3 Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other carbonate veining within xenoliths 71.8 73.8 2 Granite Quartz Chlorit Plag Green 10 Slightly Breccia Y 25 Y Prot Base of chlorite e Clay alteration, chlorite around graphite clots 73.8 77 3.2 Granite Quartz Plag Graphi Grey/ >3 Breccia Y 5 Y Tr Prot Fresh graphitic te White 0 granite, matrix supported Breccia, graphite looks pure 77 80.5 3.5 Granite Quartz Plag Graphi White/ 30 Breccia Y Tr Y Tr Prot Graphite te Grey fragments, round edged, weak foliation, graphite are blebs or clots 80.5 80.6 0.1 Micro- Quartz Plag Chlorit Grey 5 Massive Y 10 ? Y Prot Micro-granite (alt Granite e Clay meta-sediment?) xenolith, chlorite alteration 80.6 83.2 2.6 Granite Quartz Plag Graphi White/ 20 Breccia Y Y Prot Graphitic granite, te Grey - graphite and 30 metased xenoliths 83.2 83.3 0.1 Micro- Quartz Plag Grey 5 Breccia Y Y ? Y Prot Micro-granite (?) Granite xenolith oriented like a intrusive vein 83.3 85 1.7 Granite Quartz Plag Graphi White/ 10 Breccia Y Y Prot Xenoliths showing te Grey - biotite/epidote/chl 20 orite alteration 85 85.8 0.8 Granite Quartz Plag Grey 10 Breccia Y 5 Y Y Prot Xenolith - dominated 20 interval, chlorite alteration within Xenolith with Calcite veining

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD002 Interval Lithology Alteration Fro To Str Description / m at Comment Type Rock Min 1 Min 2 Min 3 Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other 85.8 86.3 0.5 Granite Quartz Plag Graphi White/ 25 Breccia Y 5 Prot Slightly clay te Grey altered zone 86.3 88.4 2.1 Granite Quartz Plag Graphi White/ >3 Breccia Y Y Prot Graphitic interval, te Grey 0 clots/blebs ~1cm 88.4 92.8 4.4 Granite Quartz Plag Graphi White/ 30 Breccia Prot Driller noted the te Grey ground hardened, the graphite blebs/clots increased in size 92.8 93.4 0.6 Micro- Quartz Plag Chlorit Grey 5 Massive 10 Y Prot Xenolith of highly Granite e Clay altered meta- sediment 93.4 96 2.6 Granite Quartz Plag White/ 20 Breccia Y 5 Y Tr Prot Graphitic Grey clots/blebs, the larger clots show chlorite clay minerals within 96 97 1 Granite Quartz Plag White/ 20 Breccia Y 5 Y Tr Prot Xenoliths of meta- Grey sediments with chlorite/graphite 97 97.1 0.1 Granite Quartz Plag Chlorit Grey 10 Breccia Y 10 Y Y Prot Xenoliths of meta- e Clay sediments showing remnant foliation (bedding?) 97.1 99 1.9 Granite Quartz Plag White/ 10 Breccia Y 5 Y Tr Prot Grey - 20 99 101.9 2.9 Granite Quartz Plag White/ 10 Breccia Y 5 Y Tr Prot More xenoliths Grey - that are non- 20 graphitic 101.9 103.3 1.4 Granite Quartz Plag White/ 10 Breccia Y 5 Y Tr Prot Grey - 20 103.3 105 1.7 Granite Quartz Plag White/ 10 Breccia Y 10 Y Tr Prot More chlorite Grey alteration of xenoliths

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD002 Interval Lithology Alteration Fro To Str Description / m at Comment Type Rock Min 1 Min 2 Min 3 Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other 105 107 2 Granite Quartz Plag White/ 10 Breccia Y 10 Y Tr Prot Grey - 15 107 108.2 1.2 Granite Quartz Plag White/ 10 Breccia Y 5 Y Tr Prot Grey - 15 108.2 111.2 3 Granite Quartz Plag White/ 10 Breccia Y 5 Y Tr Prot Grey 111.2 111.5 0.3 Micro- Quartz Plag Dark <2 Vein Y Prot Micro-granite vein Granite Grey (?), cross cutting with carbonate contacts and containing scapolite (?) 111.5 111.7 0.2 Granite Quartz Plag White <5 Breccia Y 5 Y Prot Non graphite 5 5 zone, contact feature / 111.7 115.8 4.0 Granite Quartz Plag White/ 10 Massive Y 5 Y Tr Tr Prot Xenoliths of 5 5 Grey - graphitic meta- 15 sediments (with carbonate) 115.8 116.5 0.7 Granite Quartz Plag White/ <2 Breccia Y 10 Prot Graphite reduced Grey zone 116.5 116.7 0.2 Meta- Quartz Plag Grey/ <5 Y 15 Y 5 Prot Meta-sedimentary sediment Green xenolith showing box-work carbonate veining 116.7 119.1 2.4 Granite Quartz Plag White/ 10 Breccia Y 10 Y Tr Prot Granite breccia 5 5 Grey with xenoliths of Meta-sediments 119.1 120.0 0.9 Granite Quartz Plag White/ >1 Breccia Y 5 Y Tr Prot Few more 5 5 Grey 0 xenoliths, carbonate veining in metasediment xenoliths 120.0 123.7 3.7 Granite Quartz Plag White/ >1 Breccia Y 5 Prot 5 5 Grey 0

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD002 Interval Lithology Alteration Fro To Str Description / m at Comment Type Rock Min 1 Min 2 Min 3 Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other 123.7 123.8 0.0 Vein Calcite Chlorit White/ <5 Vein Y Y Y Prot Flat fragment of 5 5 e Clay Green Metasediment but looks like a vein 123.8 125.1 1.3 Granite Quartz Plag White/ >1 Breccia Y Y Y Tr Prot Grey 0 125.1 125.2 0.1 Granite Quartz Plag White/ <5 Vein Tr Y Y Tr Prot Small greisen (?) Green like feature 125.2 125.9 0.7 Granite Quartz Plag White/ >1 Breccia Tr Y Y Tr Prot Grey 0 125.9 126.1 0.2 Granite Quartz Plag Grey <2 Massive Y ? Prot Xenolith

126.1 127.6 1.5 Granite Quartz Plag White/ >1 Breccia Y Y Y Tr Prot Grey 0 127.6 129.2 1.6 Granite Quartz Plag Dark <5 Massive ? Y Y 1 Prot Micro granite Grey xenolith, calcite veining, calcite vugh with pyrite 129.2 131.3 2.1 Granite Quartz Plag White/ >1 Breccia Y Y Y Tr Prot Some xenoliths Grey 0 have graphitic halo (ring) 131.3 131.8 0.5 Micro- Quartz Plag Chlorit Dark <5 Massive Y Y Y Y Tr Prot xenolith with white Granite e Clay Grey granite contact zone 131.8 133.6 1.8 Granite Quartz Plag White/ 10 Breccia Y Y Y Tr Tr Prot Meta-sedimentary Grey xenolith 133.6 134.3 0.7 Micro- Quartz Plag Chlorit Grey/ <5 Massive ? Y Y Y Tr Prot Micro-granite (?) Granite e Clay Green or metasedimentary (?) xenolith 134.3 140 5.7 Granite Quartz Plag White/ 10 Breccia Y Y Y Tr Prot Smaller breccia Grey fragments are graphite, larger ones are meta- sediments 140 142.1 2.1 Granite Quartz Plag White/ 10 Breccia Y Y Y Tr Prot Breccia fragments Grey are meta-

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD002 Interval Lithology Alteration Fro To Str Description / m at Comment Type Rock Min 1 Min 2 Min 3 Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other sediments in in the centre 142.1 149.3 7.2 Granite Quartz Plag White/ 10 Breccia Y Y Y Tr Prot Breccia fragments Grey are meta- sediments in in the centre 149.3 151.9 2.6 Granite Quartz Plag White/ 5- Breccia Y Y Y Tr Prot Meta-sediments Grey 10 xenoliths showing remnant foliation 151.9 156.3 4.4 Granite Quartz Plag White/ 5 Breccia Y Y Y Tr Prot Fewer graphite Grey clots/blebs, more matrix & Meta- sediment xenoliths 156.3 157.9 1.6 Granite Quartz Plag White/ 5- Breccia Y Y Y Tr Prot Grey 10 157.9 158.3 0.4 Meta- Quartz Plag Chlorit Grey/ <5 Y Y Y Y Prot Meta-sediment sediment e Clay Green xenolith (?) with carbonate veining 158.3 165.2 6.9 Granite Quartz Plag White/ 5- Breccia Y Y Y Y Tr Prot Siliceous 5 5 Grey 10 alteration first apparent with lesser graphite 165.2 165.5 0.2 Meta- Quartz Plag Chlorit Grey/ <5 Massive Y Y Y Y Tr Prot Meta-sediment 5 5 sediment e Clay Green xenolith, altered and veined 165.5 166.2 0.7 Granite Quartz Plag White/ 5- Breccia Y Y Y Y Tr Prot Grey 10 166.2 166.5 0.3 Meta- Quartz Plag Chlorit Grey/ <5 Y Y Y Y Tr Prot Xenolith of meta- sediment e Clay Green sediment 166.5 166.9 0.4 Granite Quartz Plag White/ 5- Breccia Y Y Y Y Tr Prot Grey 10 166.9 167.3 0.4 Micro- Quartz Plag Chlorit Grey/ <5 Y Y Y Y Tr Prot Granite e Clay Green 167.3 168 0.7 Granite Quartz Plag White/ 5- Breccia Y Y Y Y Tr Prot Grey 10

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD002 Interval Lithology Alteration Fro To Str Description / m at Comment Type Rock Min 1 Min 2 Min 3 Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other 168 168.4 0.4 Meta- Quartz Plag Chlorit Grey/ <5 Massive Y Y Y Y Tr Prot Large xenolith, 5 5 sediment e Clay Green carbonate veining on contact 168.4 169.4 0.9 Granite Quartz Plag White/ 5 Breccia Y Y Y Y Tr Prot Larger than usual 5 5 Grey meta-sedimentary xenoliths 169.4 173.7 4.3 Granite Quartz Plag White/ <5 Breccia Y ? Y Y Tr Prot Siliceous Breccia, Grey graphite percentage reducing 173.7 173.9 0.2 Vein Chlorite Calcite Green <5 Vein ? Y Y Y Prot Low angle Clay / Grey vein/shear zone - Driller noted significant loss in fluid circulation 173.9 178.6 4.7 Granite Quartz Plag White/ 5 Breccia Y Y Y Y Tr Prot Meta-sedimentary Grey xenoliths with graphitic halos 178.6 178.9 0.3 Micro- Quartz Plag Dark 5 Massive Y Y Prot Xenolith of Granite Grey granitised (meta- sediment) with scapolite ghosts 178.9 183 4.1 Granite Quartz Plag White/ 5 Breccia Y Y Y Y Tr Prot Siliceous Granite Grey Breccia 183 183.3 0.3 Micro- Quartz Plag Dark <5 Massive Y Y Y Prot Xenolith of Micro- Granite Grey granite 183.3 185.3 2 Granite Quartz Plag White/ <5 Breccia Y Y Y Y Tr Prot Graphitic halos Grey around meta- sediment xenoliths 185.3 185.8 0.5 Micro- Quartz Plag Dark <5 Y Y Y Y Prot Veined micro- Granite Grey granite - no meta- sediment texture 185.8 189.4 3.6 Granite Quartz Plag White/ <5 Breccia Y Y Y Y Tr Prot More meta- Grey sedimentary xenoliths with thin graphitic halos.

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD003 Interval Lithology Alteration Fro To Stra Description m t / Comment Rock Type 1Min 2Min 3Min Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other 63.4 65.35 1.9 Siltstone Quartz Feldspar Grey 0 Fresh Laminate Jur Flat lying cross 5 (?) d bedded siltstone / fine sandstone / mudstone horizon 65.35 65.8 0.4 Grit Quartz Grey 0 2- Slightl Gritty Jur Coarse 5 5m y sandstone/grit m horizon, porous aquifer 65.8 66.53 0.7 Siltstone Quartz Feldspar Grey 0 Fresh Laminate Jur Interbedded 3 (?) d Siltstone / fine sandstone 66.53 67.09 0.5 Grit Quartz Grey 0 2- Slightl Gritty Jur Coarse porous 6 5m y horizon, minor m siltsone bands 67.09 67.76 0.6 Siltstone Quartz Feldspar Grey 0 Fresh Laminate Jur Interbedded 7 (?) d coarse siltstone 67.76 68.33 0.5 Silt/Mud Quartz Feldspar Grey 0 Slightl Laminate Y Jur Mustone clay 7 Stone (?) y d rich siltstone horizon 68.33 70.6 2.2 Sandston Quartz Grey 0 1- Slightl Massive Jur Massive, 7 e 2m y porous m sandstone, well sorted, carbonaceous wisps 70.6 71.8 1.2 Jur Core Loss - Poorly cement coarse griity sandstone (?) washed away

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD003 Interval Lithology Alteration Fro To Stra Description m t / Comment Rock Type 1Min 2Min 3Min Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other 71.8 71.9 0.1 Sandston Quartz Tr 1- Slightl Gritty Jur Basin marginal e 2m y facies, m carboaceous wisps 71.9 73 1.1 Granite Quartz Plag Graphit White/ 30 Slightl Breccia ? Y Prot Paleo e Grey y weathering affected (?), large 1-2cm graphite fragments 73 73.9 0.9 Granite Quartz Plag Graphit White 30 Slightl Breccia ? Y Prot Sacharine e & y quartz, no Black chlorite/epidote alteration, all breccia fragments are graphite 73.9 75.15 1.2 Granite Quartz Plag Graphit White >3 Slightl Breccia ? Y Prot Occasional 5 e & 0 y xenolith, Black graphite silver/black 75.15 75.4 0.2 Granite Quartz Plag Graphit White 30 Slightl Breccia ? Y Prot Broken ground 5 e & y Black 75.4 77 1.6 Granite Quartz Plag Graphit White >3 Slightl Breccia ? Y Prot e & 0 y Black 77 77.2 0.2 Granite Graphit Quartz Black 50 Slightl Breccia ? Y Prot Massive e y graphite horizon - broken ground 77.2 77.7 0.5 Prot Soft graphite washed away 77.7 79.95 2.2 Granite Quartz Plag Dark 30 Slightl Breccia ? Y Prot Slightly 5 Grey y decomposed graphitic granite breccia

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD003 Interval Lithology Alteration Fro To Stra Description m t / Comment Rock Type 1Min 2Min 3Min Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other 79.95 80.3 0.3 Micro- Quartz Graphite White 20 Slightl Massive Y ? W W Prot Graphitised 5 granite & y k k microgranite Black xenolith (?), graphitic slickensides 80.3 80.8 0.5 Prot

80.8 81 0.2 Micro- Quartz Graphite Dark 20 Slightl Massive Y ? W W Prot Minor graphitic granite Grey y k k granite 81 82.2 1.2 Granite Quartz Plag Graphit Grey/ 20 Slightl Breccia Y ? W W Prot Decomposed e White y k k (?) graphitic granite, some xenoliths 82.2 83.45 1.2 Granite Quartz Plag Graphit Grey/ 20 Slightl Massive Y ? W W Prot Decomposed 5 e White y k k (?) broken ground 83.45 83.8 0.3 Prot Soft ground - 5 washed away 83.8 85.6 1.8 Granite Quartz Plag Graphit Grey 20 Slightl Breccia Y W W Prot Decomposed e y k k (?) graphite, clayey graphite 85.6 86.4 0.8 Micro- Quartz Plag Graphit Dark 20 Slightl Massive Y Y Y Prot Large granite e Grey y graphitised xenoliths 86.4 88.3 1.9 Granite Quartz Plag Graphit Grey/ 20 Slightl Breccia Y Y Y Prot More xenolithic e White y 88.3 88.92 0.6 Micro- Quartz Plag Dark 20 Slightl Massive Y Y Y Tr Prot Large 2 granite Grey y graphitised meta-sediment 88.92 90.2 1.2 Granite Quartz Plag Graphit Grey/ 20 Slightl Breccia Y Y Y Prot Xenoliths, 1- 8 e White y 2cm, graphitised 90.2 90.65 0.4 Meta- Quartz Plag Dark 10 Fresh Massive Y Y Y Prot Xenolith, calcite 5 Sediment Grey veining 90.65 91.2 0.5 Granite Quartz Plag Graphit Grey/ 20 Fresh Breccia Y Y Y Prot 5 e White

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD003 Interval Lithology Alteration Fro To Stra Description m t / Comment Rock Type 1Min 2Min 3Min Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other 91.2 91.6 0.4 Granite Quartz Plag Graphit Dark 20- Fresh Breccia Y Y Y Prot More graphitic e Grey 30 xenolithic horizon 91.6 92.72 1.1 Granite Quartz Plag Graphit Grey/ 10- Fresh Breccia Y Y Y Prot Larger 2 e White 20 xenoliths 92.72 92.8 0.0 Micro- Quartz Plag Dark 10 Fresh Vein Y Y Y Y Prot Vein like 8 granite Grey xenolith - coincident orientation and contact (?) 92.8 93.95 1.1 Granite Quartz Plag Graphit Grey/ >1 Fresh Breccia Y Y Y Prot Getting less 5 e White 0 graphitic as higher in the hole 93.95 94.25 0.3 Micro- Quartz Plag Dark 10 Fresh Massive Y Y Y Y Prot Graphitised granite Grey meta-sediment 94.25 96.3 2.0 Granite Quartz Plag Grey/ 10 Fresh Breccia Y Y Y Prot Larger 5 White xenoliths 96.3 96.5 0.2 Meta- Quartz Plag Dark <5 Fresh Laminate Y Y Y Y Prot Meta- Sediment Grey d sedimentary xenoliths with chlorite/epidote alteration 96.5 99.9 3.4 Granite Quartz Plag Grey/ 10 Fresh Breccia Y Y Y Prot Smaller breccia White fragments, graphitic, plus large meta- sediment fragments 99.9 101.0 1.1 Granite Quartz Plag White/ <1 Fresh Breccia Y Y Y Prot Breccia is 2 2 Grey 0 mostly meta- sedimentary xenoliths, with epidote/chlorite alteration 101.0 102.6 1.5 Granite Quartz Plag White/ 5 Fresh Breccia W Y Y Y Prot Fewer breccia 2 8 Grey k fragments,

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD003 Interval Lithology Alteration Fro To Stra Description m t / Comment Rock Type 1Min 2Min 3Min Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other most of which are meta- sediments 102.6 104.1 1.5 Granite Quartz Plag White/ <5 Fresh Breccia W Y Y Y Prot More Grey k Chlorite/Epidot e alteration 104.1 104.6 0.5 Meta- Quartz Plag Chlorite Dk <5 Fresh ? Y Y Y Prot Calcite veined Sediment Grey/ xenolith, Green chlorite shera on top contact 104.6 105.5 0.9 Granite Quartz Plag Chlorite Grey/ <5 Fresh Breccia W Y Y Y Prot Gradational Green k contact zone / Pink between Granite Breccia and massive granite 105.5 108.7 3.2 Granite Quartz Plag Biotite Grey/ <5 Fresh Massive ? ? Tr Tr Prot Brecciated Pink foliated granite 108.7 109.1 0.4 Micro- Quartz Plag Dark <5 Fresh Massive Y Y Y Tr Prot Carbonate granite Grey veined xenolith 109.1 110.5 1.4 Granite Quartz Plag Chlorite Grey/ <5 Fresh Massive Y Y 2- Tr Prot Calcite veining, 5 5 Pink 5 chlorite/epidote % alteration around xenoliths 110.5 113.4 2.8 Granite Quartz Plag Chlorite Grey/ <5 Fresh Massive Y Y Y 2 Prot Epidote/chlorite 5 5 Pink alteration of meta-sediment xenoliths 113.4 113.8 0.4 Micro- Quartz Plag Dark <5 Fresh Massive Y ? Y Y Y Tr Prot Xenolith granite Grey 113.8 117.6 3.8 Granite Quartz Plag Dark <5 Fresh Massive ? Y Y Y 2 Prot Fe dusted Plag, 5 5 Green biotite (chlorite altered), trace base metal sulpides (?)

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

WD003 Interval Lithology Alteration Fro To Stra Description m t / Comment Rock Type 1Min 2Min 3Min Colour Graphite % Grain Size Weathering Texture Silica Sericite Kaolin Chlorite Epidote Carbonate Pyrite Other 117.6 118.1 0.4 Micro- Quartz Plag Chlorite Dk <5 Fresh Massive Y Y Y Y 5 Prot Large xenolith, 5 5 granite Green altered, trace / Grey base metal sulpides (?) 118.1 120.4 2.3 Granite Quartz Plag Grey/ <5 Fresh Massive Y Y Y 2 Prot Fewer Pink xenoliths, texturally similar to Esmeralda Granite EOH

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 3

Drill Hole Assays

NON CO3_C Cg TC TS Mass CO3_C As CSA02V CSA02V CSA05V CSA06V CSA06V Received Lower Det Limit 0.01 0.01 0.01 0.005 0.005 Upper Det Limit 60 30 30 0 40 UNITS % % % % % grams WD002 59.0 - 59.6 <0.01 1.01 <0.01 1.01 0.044 1403 WD002 59.6 - 60.3 1.95 1.48 0.16 3.44 0.05 1834 WD002 061.0 - 062.0 2.56 1.58 0.08 4.14 0.023 2549 WD002 062.0 - 063.0 0.91 0.9 0.09 1.81 0.042 2313 WD002 063.0 - 064.0 0.72 0.84 0.12 1.56 0.015 2400 WD002 064.0 - 065.0 0.95 1.26 0.48 2.21 0.005 3062 WD002 065.0 - 066.0 0.36 1.86 1.12 2.22 0.009 2267 WD002 066.0 - 067.0 1.33 2.07 0.99 3.4 0.013 2920 WD002 067.0 - 068.0 <0.01 1.72 1.48 1.72 0.016 2563 WD002 068.0 - 069.0 <0.01 2.23 2.06 2.23 0.014 2768 WD002 069.0 - 070.0 0.86 3.42 2.47 4.29 0.01 2522 WD002 070.0 - 071.0 0.54 3.32 2.83 3.86 0.01 2553 WD002 071.0 - 072.0 1.29 5.02 4.58 6.31 0.02 3068 WD002 072.0 - 073.0 1.53 6.39 5.96 7.91 0.01 2836 WD002 073.0 - 074.0 1.24 6.33 5.77 7.57 0.147 2777 WD002 074.0 - 075.0 1.02 7.83 7.89 8.85 1.2 - WD002 075.0 - 076.0 0.99 7.63 7.84 8.62 1.41 - WD002 076.0 - 077.0 0.56 6.22 6.71 6.78 1.2 2852 WD002 077.0 - 078.0 0.43 4.88 5.28 5.31 0.986 2717 WD002 078.0 - 079.0 0.89 5.27 6.11 6.16 0.753 2812 WD002 079.0 - 080.0 0.37 6.07 6.35 6.44 0.674 2920 WD002 080.0 - 081.0 0.45 5.67 5.97 6.12 1.08 3120 WD002 081.0 - 082.0 0.34 5.2 5.46 5.55 0.822 3064 WD002 082.0 - 083.0 0.46 4.59 4.84 5.06 0.732 3122 WD002 083.0 - 084.0 0.24 3.26 3.2 3.5 0.748 3420 WD002 084.0 - 085.0 0.54 4.89 5.1 5.43 1.38 3288 WD002 085.0 - 086.0 0.85 7.65 8.15 8.5 1.17 3126 WD002 086.0 - 087.0 1.02 7.93 8.41 8.94 2.09 2961 WD002 087.0 - 088.0 1.57 8.53 8.6 10.1 2.07 - WD002 088.0 - 089.0 1.04 6.88 7.02 7.92 1.71 - WD002 089.0 - 090.0 0.82 5.61 5.48 6.43 1.61 - WD002 090.0 - 091.0 0.32 5.58 5.56 5.9 1.49 3824

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

NON CO3_C Cg TC TS Mass CO3_C WD002 091.0 - 092.0 0.5 4.81 4.95 5.31 1.33 3598 WD002 092.0 - 093.0 0.61 5.09 5.2 5.7 0.954 3588 WD002 093.0 - 094.0 0.29 4.8 4.87 5.09 0.993 3525 WD002 094.0 - 095.0 0.39 6.11 5.94 6.5 1.57 3618 WD002 095.0 - 096.0 0.63 6.81 6.89 7.44 1.87 3584 WD002 096.0 - 097.0 0.6 7.27 7.49 7.87 1.88 3562 WD002 097.0 - 098.0 0.71 6.05 6.33 6.77 1.57 3658 WD002 098.0 - 099.0 0.18 6.49 6.34 6.67 1.63 3684 WD002 099.0 - 100.0 0.42 6.37 6.57 6.8 1.71 3728 WD002 100.0 - 101.0 0.49 7.65 7.9 8.15 1.85 3696 WD002 101.0 - 102.0 0.49 7.44 7.58 7.93 2.35 3894 WD002 102.0 - 103.0 0.36 7.99 8.14 8.35 2.22 3288 WD002 103.0 - 104.0 0.22 5.46 5.26 5.68 1.49 3484 WD002 104.0 - 105.0 0.45 5.38 5.33 5.83 1.93 3770 WD002 105.0 - 106.0 0.74 6.09 6.36 6.83 2.04 3720 WD002 106.0 - 107.0 0.68 6.96 7.15 7.63 2.1 3594 WD002 107.0 - 108.0 0.77 7.1 6.39 7.87 2.31 3614 WD002 108.0 - 109.0 0.91 8.05 8.65 8.96 1.96 3608 WD002 109.0 - 110.0 0.87 7.21 7.81 8.08 2.69 3658 WD002 110.0 - 111.2 1.44 10.5 11.5 11.9 2.07 3564 WD002 111.2 - 111.75 0.17 4.09 4.13 4.26 0.382 2185 WD002 111.75 - 113.0 0.72 7.52 8.26 8.24 1.41 4282 WD002 113.0 - 114.0 0.65 7.04 7.72 7.69 2.1 3730 WD002 114.0 - 115.0 0.89 8.5 9.39 9.39 2.24 3713 WD002 115.0 - 115.8 1.02 6.65 7.71 7.67 2.22 3296 WD002 115.8 - 117.0 <0.01 2.75 2.8 2.75 1.58 4312 WD002 117.0 - 118.0 0.6 6.29 7.14 6.89 2.05 3634 WD002 118.0 - 119.0 0.53 6.65 7.26 7.18 1.77 3784 WD002 119.0 - 120.0 0.79 7.19 7.66 7.98 1.14 3650 WD002 120.0 - 121.0 0.49 7.23 7.5 7.71 1.81 3812 WD002 121.0 - 122.0 0.9 7.3 8.34 8.2 1.85 3778 WD002 122.0 - 123.0 0.71 7.59 7.97 8.3 1.38 3646 WD002 123.0 - 124.0 1.26 7.22 6.49 8.48 0.186 3414 WD002 124.0 - 125.0 0.52 7.99 7.81 8.51 1.32 3690 WD002 125.0 - 126.0 0.99 7.82 8.44 8.82 1.31 3760 WD002 126.0 - 127.0 0.68 7.64 8.32 8.32 1.92 3740 WD002 127.0 - 128.0 0.49 7.41 7.31 7.9 1.31 3782 WD002 128.0 - 129.0 0.49 7.66 7.73 8.15 1.89 3804 WD002 129.0 - 130.0 0.79 7.13 7.87 7.92 1.86 3836 WD002 130.0 - 131.0 0.51 7.58 7.92 8.1 2.4 3702 WD002 131.0 - 132.0 0.63 9.21 9.05 9.84 1.06 3692 WD002 132.0 - 133.0 0.04 5.31 4.88 5.34 1.21 3676 WD002 133.0 - 134.0 0.51 5.09 5.32 5.59 1.73 3750

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

NON CO3_C Cg TC TS Mass CO3_C WD002 134.0 - 135.0 0.8 5.64 6.08 6.45 3.35 3824 WD002 135.0 - 136.0 0.47 7.46 7.67 7.94 2.05 3714 WD002 136.0 - 137.0 0.39 7.54 7.68 7.94 1.81 3666 WD002 137.0 - 138.0 0.45 7.95 7.79 8.4 0.674 3678 WD002 138.0 - 139.0 0.18 7.73 7.54 7.9 1.41 3680 WD002 139.0 - 140.0 0.44 7.55 7.6 7.99 1.72 3730 WD002 140.0 - 141.0 0.3 7.06 7.08 7.35 0.675 3564 WD002 141.0 - 142.0 0.49 6.28 6.53 6.77 0.743 3494 WD002 142.0 - 143.0 0.74 7.64 8.13 8.39 1.48 3604 WD002 143.0 - 144.0 0.69 7.64 8.04 8.33 1.96 3550 WD002 144.0 - 145.0 0.51 7.97 8.21 8.47 1.83 3644 WD002 145.0 - 146.0 1.3 7.6 8.68 8.9 1.99 3646 WD002 146.0 - 147.0 1 7.8 8.48 8.8 2.15 3682 WD002 147.0 - 148.0 0.67 7.36 7.88 8.03 1.88 3726 WD002 148.0 - 149.0 0.59 5.72 6.17 6.32 1.78 3554 WD002 149.0 - 150.0 0.34 3.53 3.92 3.87 0.827 3662 WD002 150.0 - 151.0 0.37 4.55 4.77 4.92 1.16 3756 WD002 151.0 - 152.0 0.23 3.3 3.3 3.53 1.2 3758 WD002 152.0 - 153.0 <0.01 4.08 3.93 4.01 1.24 3606 WD002 153.0 - 154.0 0.11 3.63 3.73 3.75 1.15 3552 WD002 154.0 - 155.0 0.06 3.65 3.7 3.71 1.2 3576 WD002 155.0 - 156.0 0.17 3.82 3.85 3.98 1.27 3512 WD002 156.0 - 157.0 0.51 6.09 6.6 6.61 1.84 3472 WD002 157.0 - 158.0 0.88 6.2 7.18 7.08 2.04 3584 WD002 158.0 - 159.0 0.16 5.33 5.53 5.49 1.28 3613 WD002 159.0 - 160.0 0.22 5.68 5.6 5.9 0.975 3442 WD002 160.0 - 161.0 0.12 5.52 5.44 5.64 0.882 3622 WD002 161.0 - 162.0 0.39 5.28 5.48 5.67 0.067 3546 WD002 162.0 - 163.0 0.56 5.89 5.9 6.45 0.052 3462 WD002 163.0 - 164.0 0.42 4.99 5.05 5.41 0.198 3632 WD002 164.0 - 165.0 0.28 4.56 4.46 4.84 0.477 3530 WD002 165.0 - 166.0 0.36 3.41 3.57 3.77 0.032 3394 WD002 166.0 - 167.0 0.28 3.42 2.97 3.7 0.067 3388 WD002 167.0 - 168.0 0.11 3.17 2.82 3.27 0.098 3494 WD002 168.0 - 169.0 <0.01 2.5 2.19 2.51 0.133 3528 WD002 169.0 - 170.0 0.14 1.94 1.95 2.08 0.473 3498 WD002 170.0 - 171.0 <0.01 1.4 1.34 1.4 0.177 3484 WD002 171.0 - 172.0 <0.01 1.74 1.51 1.74 0.196 3274 WD002 172.0 - 173.0 0.27 1.79 1.47 2.06 0.977 3706 WD002 173.0 - 174.0 <0.01 1.63 1.58 1.63 1.18 3772 WD002 174.0 - 175.0 <0.01 1.41 1.3 1.41 1.26 3868 WD002 175.0 - 176.0 0.25 1.97 2.16 2.22 1.18 3836 WD002 176.0 - 177.0 <0.01 2.17 2.21 2.17 0.805 3534

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

NON CO3_C Cg TC TS Mass CO3_C WD002 177.0 - 178.0 0.28 3.14 3.37 3.42 1.49 4056 WD002 178.0 - 179.0 0.12 2.02 2.09 2.14 0.836 4202 WD002 179.0 - 180.0 0.08 2.79 2.42 2.88 0.982 4164 WD002 180.0 - 181.0 0.21 3.56 3.54 3.77 1.11 4260 WD002 181.0 - 182.0 0.65 2.45 2.97 3.1 0.963 4188 WD002 182.0 - 183.0 0.06 2.73 2.58 2.79 0.879 4202 WD002 183.0 - 184.0 0.21 2.49 2.47 2.7 0.548 4202 WD002 184.0 - 185.0 0.31 3.83 4.04 4.14 1.34 4310 WD002 185.0 - 186.0 0.52 3.12 3.45 3.64 1.04 4144 WD002 186.0 - 187.0 0.37 3.94 3.94 4.31 1.29 4240 WD002 187.0 - 188.0 0.24 5.08 5.07 5.32 1.66 4190 WD002 188.0 - 189.4 0.46 3.87 4.14 4.33 1.25 7185

WD003 71.8 - 71.9 <0.01 1.97 1.54 1.98 0.022 253 WD003 71.9 - 72.0 0.84 14 14.2 14.8 0.914 300 WD003 072.0 - 073.0 1.03 13.9 14.7 15 1.25 2564 WD003 073.0 - 074.0 0.62 12.7 12.3 13.3 0.721 2548 WD003 074.0 - 075.0 1.01 11.8 12.4 12.8 1.06 2229 WD003 075.0 - 076.0 0.61 12.7 13.2 13.3 1.25 2413 WD003 76.0 - 77.2 1.11 12.9 13.3 14 1.61 2246 WD003 77.7 - 78.95 0.49 12.3 12.2 12.8 1.22 2777 WD003 79.0 - 80.0 0.45 5.5 5.72 5.95 0.537 3120 WD003 080.0 - 081.0 0.59 3.79 3.83 4.39 1.42 976 WD003 081.0 - 082.0 0.95 11.1 11.5 12.1 1.75 2677 WD003 082.0 - 083.0 0.54 6.42 6.34 6.95 0.735 2377 WD003 083.0 - 084.0 0.4 8.02 8.36 8.42 1.51 2019 WD003 084.0 - 085.0 0.48 5.25 5.47 5.73 0.431 2492 WD003 085.0 - 086.0 0.65 7.49 7.83 8.14 0.481 2476 WD003 086.0 - 087.0 0.76 7.5 7.38 8.26 1.7 2253 WD003 087.0 - 088.0 0.67 8.48 8.64 9.14 2 2834 WD003 088.0 - 089.0 0.76 9.03 9.05 9.79 1.93 2900 WD003 089.0 - 090.0 0.35 7.19 7.31 7.54 1.88 3158 WD003 090.0 - 091.0 0.67 4 4.07 4.67 0.558 3454 WD003 091.0 - 092.0 1.16 8.14 8.67 9.29 2.08 3346 WD003 092.0 - 093.0 0.7 6.63 6.99 7.33 1.73 3540 WD003 093.0 - 094.0 0.47 4.62 4.87 5.09 1.19 3502 WD003 094.0 - 095.0 0.4 4.95 5.01 5.35 0.666 3430 WD003 095.0 - 096.0 0.31 3.07 3.04 3.38 0.393 3546 WD003 096.0 - 097.0 0.51 4.54 4.74 5.05 0.868 3600 WD003 097.0 - 098.0 0.6 5.9 6.18 6.5 1.53 3904 WD003 098.0 - 099.0 0.98 6.76 7.24 7.74 1.94 4108 WD003 99.0 - 99.9 0.83 6.84 7.22 7.67 1.83 3132 WD003 99.9 - 101.0 0.2 3.35 3.37 3.55 0.655 4008

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

NON CO3_C Cg TC TS Mass CO3_C WD003 101.0 - 102.0 0.22 2.67 2.76 2.9 0.79 3368 WD003 102.0 - 103.0 0.04 2.14 2.04 2.18 0.423 3408 WD003 103.0 - 104.0 0.29 1.24 1.31 1.53 0.408 3496 WD003 104.0 - 105.0 0.5 2.72 2.45 3.22 0.037 3556 WD003 105.0 - 106.0 0.3 1.99 2.13 2.29 0.352 3466 WD003 106.0 - 107.0 0.29 1.55 1.53 1.84 0.39 3540 WD003 107.0 - 108.0 0.08 1.53 1.44 1.62 0.629 3818 WD003 108.0 - 109.0 0.46 2.31 2.4 2.76 0.339 3588 WD003 109.0 - 110.0 0.53 2.23 2.21 2.76 0.448 3630 WD003 110.0 - 111.0 0.92 1 0.83 1.92 0.438 3560 WD003 111.0 - 112.0 0.64 0.48 0.37 1.11 2.43 3432 WD003 112.0 - 113.0 0.26 1.23 1.14 1.48 0.409 3626 WD003 113.0 - 114.0 0.21 2.44 2.43 2.65 0.253 3916 WD003 114.0 - 115.0 0.09 1.47 1.37 1.56 0.233 3676 WD003 115.0 - 116.0 0.27 2.55 2.57 2.82 0.995 3608 WD003 116.0 - 117.0 0.34 2.55 2.67 2.89 0.844 3586 WD003 117.0 - 118.0 0.46 5.44 5.49 5.9 1.1 3936 WD003 118.0 - 119.0 0.21 2.56 2.64 2.78 1.04 3686 WD003 119.0 - 120.2 0.14 0.96 0.97 1.09 0.742 4558

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 3A

WD002 Assay Certificates

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 3B

WD003 Assay Certificates

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 3C

Assay Data

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 4

Specific Gravity & Magnetic Susceptibility

Magnetic Specific Susceptibility Gravity Hole ID From To Mag From To Int Dry Wet SG WD002 59.0 59.6 0.137 59.23 59.33 0.10 0.190 0.115 2.53 WD002 59.6 60.3 0.165 60.25 60.32 0.07 0.185 0.120 2.85 WD002 61.0 62.0 1.01 61.30 61.50 0.20 0.570 0.320 2.28 WD002 62.0 63.0 4.73 62.00 62.11 0.11 0.340 0.195 2.34 WD002 63.0 64.0 0.445 63.02 63.15 0.13 0.380 0.210 2.24 WD002 64.0 65.1 0.765 64.08 64.29 0.21 0.745 0.420 2.29 WD002 65.1 66.0 0.739 65.03 65.12 0.09 0.240 0.135 2.29 WD002 66.0 67.0 0.909 66.00 66.09 0.09 0.270 0.145 2.16 WD002 67.0 68.0 0.346 67.35 67.60 0.25 0.840 0.475 2.30 WD002 68.0 69.0 0.449 68.10 68.25 0.15 0.465 0.255 2.21 WD002 69.0 70.0 0.894 69.05 69.31 0.26 0.830 0.470 2.31 WD002 70.0 71.0 0.4 70.00 70.27 0.27 0.720 0.390 2.18 WD002 71.0 72.0 0.662 71.07 71.20 0.13 0.465 0.275 2.45 WD002 72.0 73.0 0.423 72.03 72.28 0.25 0.795 0.455 2.34 WD002 73.0 73.8 0.987 73.02 73.15 0.13 0.425 0.240 2.30 WD002 73.8 75.0 0.257 74.02 74.30 0.28 0.855 0.510 2.48 WD002 75.0 76.0 0.219 75.06 75.19 0.13 0.365 0.210 2.35 WD002 76.0 77.0 0.324 76.00 76.09 0.09 0.280 0.160 2.33 WD002 77.0 78.0 0.62 77.00 77.28 0.28 0.980 0.575 2.42 WD002 78.0 79.0 0.102 78.00 78.12 0.12 0.410 0.245 2.48 WD002 79.0 80.0 0.15 79.20 79.47 0.27 0.830 0.485 2.41 WD002 80.0 81.0 0.151 80.00 80.11 0.11 0.370 0.220 2.47 WD002 81.0 82.0 0.161 81.12 81.26 0.14 0.420 0.245 2.40 WD002 82.0 83.0 0.127 82.16 82.35 0.19 0.645 0.380 2.43 WD002 83.0 84.0 0.145 83.00 83.17 0.17 0.565 0.340 2.51 WD002 84.0 85.0 0.154 84.05 84.28 0.23 0.840 0.505 2.51 WD002 85.0 86.0 0.319 85.10 85.21 0.11 0.400 0.235 2.42 WD002 86.0 87.0 0.318 86.22 86.39 0.17 0.605 0.365 2.52 WD002 87.0 88.0 0.224 87.00 87.21 0.21 0.655 0.405 2.62 WD002 88.0 89.0 0.167 88.00 88.26 0.26 0.780 0.480 2.60 WD002 89.0 90.0 0.273 89.10 89.21 0.11 0.465 0.285 2.58 WD002 90.0 91.0 0.301 90.29 90.41 0.12 0.445 0.275 2.62 WD002 91.0 92.0 0.241 91.00 91.10 0.10 0.395 0.245 2.63 WD002 92.0 93.0 0.414 92.04 92.16 0.12 0.390 0.240 2.60 WD002 93.0 94.0 0.252 93.54 93.72 0.18 0.625 0.385 2.60 WD002 94.0 95.0 0.275 94.00 94.15 0.15 0.555 0.345 2.64 WD002 95.0 96.0 0.323 95.00 95.12 0.12 0.430 0.265 2.61

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Magnetic Specific Susceptibility Gravity Hole ID From To Mag From To Int Dry Wet SG WD002 96.0 97.0 0.267 96.00 96.10 0.10 0.360 0.225 2.67 WD002 97.0 98.0 0.245 97.00 97.14 0.14 0.510 0.320 2.68 WD002 98.0 99.0 0.386 98.00 98.19 0.19 0.705 0.440 2.66 WD002 99.0 100.0 0.282 99.00 99.18 0.18 0.650 0.405 2.65 WD002 100.0 101.0 0.224 100.00 100.17 0.17 0.600 0.375 2.67 WD002 101.0 102.0 0.25 101.00 101.12 0.12 0.425 0.260 2.58 WD002 102.0 103.0 0.272 102.00 102.13 0.13 0.480 0.300 2.67 WD002 103.0 104.0 0.097 103.37 103.65 0.28 1.035 0.650 2.69 WD002 104.0 105.0 0.304 104.00 104.23 0.23 0.855 0.535 2.67 WD002 105.0 106.0 0.345 105.34 105.47 0.13 0.485 0.305 2.69 WD002 106.0 107.0 3.97 106.00 106.08 0.08 0.300 0.190 2.73 WD002 107.0 108.0 9.82 107.00 107.23 0.23 0.880 0.555 2.71 WD002 108.0 109.0 4.38 108.00 108.20 0.20 0.785 0.490 2.66 WD002 109.0 110.0 10.09 109.00 109.18 0.18 0.650 0.410 2.71 WD002 110.0 111.2 9.63 110.00 110.22 0.22 0.660 0.410 2.64 WD002 111.2 111.75 0.19 111.00 111.20 0.20 0.760 0.475 2.67 WD002 111.75 113.0 0.384 112.35 112.55 0.20 0.725 0.445 2.59 WD002 113.0 114.0 10.8 113.00 113.17 0.17 0.630 0.395 2.68 WD002 114.0 115.0 13.4 114.00 114.14 0.14 0.490 0.305 2.65 WD002 115.0 115.8 11.5 115.00 115.22 0.22 0.735 0.460 2.67 WD002 115.8 117.0 0.405 116.00 116.14 0.14 0.475 0.310 2.88 WD002 117.0 118.0 7.94 117.00 117.20 0.20 0.900 0.565 2.69 WD002 118.0 119.0 6.34 118.00 118.18 0.18 0.635 0.395 2.65 WD002 119.0 120.0 0.541 119.02 119.30 0.28 0.975 0.585 2.50 WD002 120.0 121.0 10.07 120.00 120.14 0.14 0.475 0.295 2.64 WD002 121.0 122.0 10 121.00 121.10 0.10 0.345 0.215 2.65 WD002 122.0 123.0 10.8 122.05 122.26 0.21 0.735 0.460 2.67 WD002 123.0 124.0 0.506 123.06 123.28 0.22 0.735 0.455 2.63 WD002 124.0 125.0 0.43 124.05 124.27 0.22 0.715 0.445 2.65 WD002 125.0 126.0 5.84 125.00 125.08 0.08 0.295 0.185 2.68 WD002 126.0 127.0 8.29 126.00 126.19 0.19 0.685 0.435 2.74 WD002 127.0 128.0 9.38 127.00 127.23 0.23 0.810 0.515 2.75 WD002 128.0 129.0 3.62 128.00 128.22 0.22 0.770 0.490 2.75 WD002 129.0 130.0 8.47 129.03 129.13 0.10 0.390 0.245 2.69 WD002 130.0 131.0 7.24 130.02 130.16 0.14 0.505 0.315 2.66 WD002 131.0 132.0 0.728 131.00 131.13 0.13 0.480 0.305 2.74 WD002 132.0 133.0 0.986 132.00 132.13 0.13 0.455 0.285 2.68 WD002 133.0 134.0 6.14 133.26 133.43 0.17 0.615 0.385 2.67 WD002 134.0 135.0 8.76 134.00 134.10 0.10 0.380 0.250 2.92 WD002 135.0 136.0 4.69 135.00 135.20 0.20 0.735 0.465 2.72 WD002 136.0 137.0 3.89 136.00 136.19 0.19 0.695 0.435 2.67 WD002 137.0 138.0 2.5 137.00 137.29 0.29 0.830 0.520 2.68 WD002 138.0 139.0 3.08 138.04 138.15 0.11 0.390 0.245 2.69

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Magnetic Specific Susceptibility Gravity Hole ID From To Mag From To Int Dry Wet SG WD002 139.0 140.0 5.49 139.00 139.14 0.14 0.515 0.325 2.71 WD002 140.0 141.0 4.33 140.07 140.29 0.22 0.820 0.520 2.73 WD002 141.0 142.0 0.41 141.04 141.19 0.15 0.560 0.350 2.67 WD002 142.0 143.0 9.43 142.00 142.20 0.20 0.720 0.450 2.67 WD002 143.0 144.0 5.55 143.00 143.17 0.17 0.650 0.410 2.71 WD002 144.0 145.0 2.21 144.00 144.16 0.16 0.580 0.365 2.70 WD002 145.0 146.0 3.93 145.00 145.14 0.14 0.515 0.330 2.78 WD002 146.0 147.0 7.14 146.00 146.18 0.18 0.275 0.175 2.75 WD002 147.0 148.0 6.24 147.00 147.22 0.22 0.805 0.505 2.68 WD002 148.0 149.0 3.69 148.00 148.16 0.16 0.570 0.360 2.71 WD002 149.0 150.0 1.9 149.00 149.14 0.14 0.480 0.300 2.67 WD002 150.0 151.0 0.938 150.00 150.12 0.12 0.430 0.270 2.69 WD002 151.0 152.0 1.55 151.05 151.28 0.23 0.870 0.555 2.76 WD002 152.0 153.0 1.95 152.00 152.31 0.31 1.110 0.695 2.67 WD002 153.0 154.0 2.73 153.00 153.08 0.08 0.300 0.190 2.73 WD002 154.0 155.0 6.48 154.00 154.23 0.23 0.740 0.470 2.74 WD002 155.0 156.0 1.3 155.00 155.23 0.23 0.835 0.525 2.69 WD002 156.0 157.0 12.6 156.00 156.21 0.21 0.755 0.475 2.70 WD002 157.0 158.0 6.37 157.17 157.30 0.13 0.460 0.295 2.79 WD002 158.0 159.0 7.68 158.00 158.10 0.10 0.340 0.210 2.62 WD002 159.0 160.0 0.284 159.00 159.10 0.10 0.335 0.210 2.68 WD002 160.0 161.0 0.368 160.00 160.24 0.24 0.855 0.535 2.67 WD002 161.0 162.0 0.536 161.13 161.28 0.15 0.585 0.365 2.66 WD002 162.0 163.0 0.252 162.00 162.25 0.25 0.690 0.430 2.65 WD002 163.0 164.0 2.18 163.00 163.27 0.27 0.900 0.560 2.65 WD002 164.0 165.0 0.274 164.00 164.19 0.19 0.735 0.455 2.63 WD002 165.0 166.0 0.373 165.00 165.19 0.19 0.650 0.400 2.60 WD002 166.0 167.0 0.335 166.00 166.18 0.18 0.675 0.415 2.60 WD002 167.0 168.0 0.18 167.00 167.10 0.10 0.335 0.205 2.58 WD002 168.0 169.0 0.222 168.00 168.20 0.20 0.710 0.440 2.63 WD002 169.0 170.0 0.078 169.00 169.09 0.09 0.310 0.195 2.70 WD002 170.0 171.0 0.209 170.00 170.22 0.22 0.835 0.525 2.69 WD002 171.0 172.0 0.226 171.00 171.19 0.19 0.720 0.460 2.77 WD002 172.0 173.0 1.98 172.15 172.32 0.17 0.595 0.360 2.53 WD002 173.0 174.0 2.11 173.00 173.14 0.14 0.500 0.320 2.78 WD002 174.0 175.0 1.89 174.00 174.07 0.07 0.245 0.150 2.58 WD002 175.0 176.0 5.52 175.00 175.08 0.08 0.300 0.190 2.73 WD002 176.0 177.0 2.35 176.01 176.13 0.12 0.390 0.245 2.69 WD002 177.0 178.0 17 177.03 177.20 0.17 0.640 0.395 2.61 WD002 178.0 179.0 7.16 178.00 178.16 0.16 0.585 0.365 2.66 WD002 179.0 180.0 4.62 179.00 179.23 0.23 0.900 0.575 2.77 WD002 180.0 181.0 0.612 180.00 180.17 0.17 0.645 0.405 2.69 WD002 181.0 182.0 2.84 181.00 181.18 0.18 0.665 0.420 2.71

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Magnetic Specific Susceptibility Gravity Hole ID From To Mag From To Int Dry Wet SG WD002 182.0 183.0 2.35 182.00 182.09 0.09 0.360 0.225 2.67 WD002 183.0 184.0 1.03 183.00 183.12 0.12 0.470 0.295 2.69 WD002 184.0 185.0 5.43 184.00 184.10 0.10 0.375 0.230 2.59 WD002 185.0 186.0 0.092 185.00 185.16 0.16 0.610 0.385 2.71 WD002 186.0 187.0 8.5 186.02 186.29 0.27 1.025 0.640 2.66 WD002 187.0 188.0 7.96 187.00 187.16 0.16 0.630 0.395 2.68 WD002 188.0 189.4 4.52 188.06 188.19 0.13 0.570 0.375 2.92 WD002 189.00 189.12 0.12 0.480 0.300 2.67

WD003 71.8 71.9 0.116 71.94 72 0.06 0.130 0.070 2.17 WD003 71.8 71.9 0.125 72.1 72.32 0.22 0.595 0.320 2.16 WD003 71.9 72 0.145 73.06 73.23 0.17 0.430 0.225 2.10 WD003 72 73 0.083 74.48 74.55 0.07 0.185 0.105 2.31 WD003 73 74 0.122 75.05 75.15 0.10 0.245 0.135 2.23 WD003 74 75 0.112 76.35 76.44 0.09 0.190 0.105 2.24 WD003 75 76 0.145 77.7 77.8 0.10 0.255 0.140 2.22 WD003 76 77.2 0.108 78.2 78.34 0.14 0.330 0.185 2.28 WD003 77.7 78.95 0.155 79.3 79.38 0.08 0.180 0.105 2.40 WD003 78.95 80 0.076 80.02 80.06 0.04 0.125 0.070 2.27 WD003 80 81 0.142 81.32 81.4 0.08 0.235 0.135 2.35 WD003 81 82 0.154 82.4 82.57 0.17 0.380 0.215 2.30 WD003 82 83 0.139 83 83.07 0.07 0.160 0.095 2.46 WD003 83 84 0,074 84.5 84.63 0.13 0.315 0.175 2.25 WD003 84 85 0.27 85.6 85.81 0.21 0.415 0.215 2.08 WD003 85 86 0.37 86.05 86.25 0.20 0.425 0.225 2.13 WD003 86 87 0.346 87 87.12 0.12 0.290 0.165 2.32 WD003 87 88 0.32 88 88.12 0.12 0.295 0.165 2.27 WD003 88 89 0.325 89 89.1 0.10 0.255 0.150 2.43 WD003 89 90 0.329 90.12 90.22 0.10 0.325 0.195 2.50 WD003 90 91 0.594 91.08 91.18 0.10 0.295 0.165 2.27 WD003 91 92 0.349 92 92.1 0.10 0.260 0.155 2.48 WD003 92 93 0,298 93.02 93.14 0.12 0.365 0.220 2.52 WD003 93 94 0.453 94 94.13 0.13 0.360 0.210 2.40 WD003 94 95 0.352 95 95.1 0.10 0.300 0.170 2.31 WD003 95 96 0.349 96.1 96.27 0.17 0.525 0.315 2.50 WD003 96 97 0.528 97.38 97.62 0.24 0.745 0.455 2.57 WD003 97 98 0.392 98 98.18 0.18 0.575 0.355 2.61 WD003 98 99 0.433 99 99.25 0.25 0.770 0.475 2.61 WD003 99 99.9 0.713 100 100.27 0.27 0.915 0.560 2.58 WD003 99.9 101 0.394 101 101.29 0.29 1.060 0.650 2.59 WD003 101 102 0.697 102.09 102.29 0.20 0.690 0.420 2.56 WD003 102 103 0.281 103.56 103.74 0.18 0.680 0.415 2.57 WD003 103 104 0.461 104.4 104.54 0.14 0.510 0.315 2.62 WD003 104 105 0.667 105 105.11 0.11 0.405 0.245 2.53 WD003 105 106 0.321 106.05 106.3 0.25 1.035 0.635 2.59 WD003 106 107 0.313 107.35 107.54 0.19 0.720 0.445 2.62 WD003 107 108 0.669 108 108.18 0.18 0.690 0.425 2.60 WD003 108 109 0.349 109 109.22 0.22 0.840 0.515 2.58 WD003 109 110 0.271 110.04 110.24 0.20 0.830 0.510 2.59

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Magnetic Specific Susceptibility Gravity Hole ID From To Mag From To Int Dry Wet SG WD003 110 111 0.582 111 111.25 0.25 0.985 0.620 2.70 WD003 111 112 0.606 112 112.25 0.25 0.940 0.570 2.54 WD003 112 113 0.348 113.3 113.46 0.16 0.600 0.375 2.67 WD003 113 114 0.338 114.28 114.4 0.12 0.505 0.310 2.59 WD003 114 115 0.325 115.08 115.25 0.17 0.720 0.445 2.62 WD003 115 116 0.363 116 116.26 0.26 1.085 0.675 2.65 WD003 116 117 0.688 117 117.16 0.16 0.670 0.425 2.73 WD003 117 118 1.35 118 118.27 0.27 1.120 0.710 2.73 WD003 118 119 0.476 119 119.15 0.15 0.560 0.350 2.67 WD003 119 120.2 0.551 120 120.17 0.17 0.665 0.420 2.71

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 5

Preliminary Metallurgical Report

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 6

RC002A Drill Chip (Historic) Mineral Liberation Report

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 7

Petrology Report Geochempet Services

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 8A

WD002 Core Tray Photography

TOUCHSTONE RESOURCES PTY LTD ACN 126 306 018

Appendix 8B

WD003 Core Tray Photography