Announcement PDF 2 September 2026 ASX ANNOUNCEMENT A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 1 FURTHER COMPELLING GOLD TARGETS EMERGE IN THE WESTERN ZONE OF MT TURNER PROJECT HIGHLIGHTS • Two new gold targets defined within the 5km-long Western Zone at Lightning’s flagship Mt Turner Gold Project, materially advancing a previously conceptual structural corridor. • Large northern target consists of a 1000m-long gold anomaly associated with a broader 1,400m-long multi-element anomaly, a potential “hydrothermal footprint”. • Northern gold anomaly remains open to the south and east with potential to expand the target area. • Southern gold in soil anomalies identified as four sub-parallel trends extending 200– 300m along strike, with peak gold in soil value of 330 ppb Au. • Rock-chips collected during 2026 soil sampling program, include 1.19 g/t Au and 38.80 g/t Ag from a mineralised rhyolite breccia. • Historical reconnaissance rock chip sampling has returned individual values of up to 15.35 g/t Au, 198 g/t Ag and 22% Cu, confirming the multi-element nature of the mineralisation and potential prospectivity of the structure. • Western Zone represents a second major gold bearing structural corridor within the Mt Turner Project, complementing the Company’s initial drilling exploration success along the 14km Drummer Fault. • Soil and Rock chip results indicate the potential scale and prospectivity of the broader Mt Turner Project • A low-cost follow-up program is planned during this exploration season window. Lightning Minerals Limited (ASX: L1M or “the Company”) is pleased to report that interpretation of results from the recently completed Western Zone soil geochemistry program has defined two compelling gold target areas at the Company’s wholly owned Mt Turner Project in northern Queensland. The results materially advance the Western Zone from a conceptual structural target to a priority, multi-target exploration corridor. In the north, geochemical zonation delineates a potential intrusion-related hydrothermal footprint with gold concentrated along its western edge, a potential transition-zone. In the south, multiple discrete gold-arsenic anomalies are interpreted to represent separate mineralised rhyolite dykes, likely associated with higher- level epithermal-style mineralisation. A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 2 Managing Director Troy Brice commented: “These results represent an important step forward in our systematic evaluation of the broader Mt Turner Gold and Copper Project, defining two significant gold target areas within the five-kilometre Western Zone corridor. The scale and coherence of the northern target is particularly encouraging, with a continuous one-kilometre gold anomaly adjacent to a larger 1.4-kilometre multi-element interpreted hydrothermal footprint, additionally, multiple, parallel, gold anomalies have been defined in the south. These results are supported by highly anomalous rock chip results, importantly, the gold anomaly and hydrothermal footprint target in the north remain open. The Western Zone provides Lightning with another major gold exploration opportunity alongside the 14-kilometre-long Drummer Fault target and further strengthens our view of the broader district scale potential at Mt Turner. Our next phase of work will focus on extending and refining these anomalies through targeted soil and rock chip sampling and trenching, with the objective of defining priority targets for initial drill testing. With multiple gold targets now emerging across Mt Turner, we are excited by the opportunity ahead and look forward to systematically advancing the Project.” Figure 1 - Location Map – Mt Turner Project. Next Steps – Advancing Targets Toward Drill Definition The Company proposes a staged, low-cost follow-up program designed to validate the surface response and generate drill-ready targets: • Complete approximately 100 additional soil samples to refine the northern thermal vector anomaly to the east and the gold anomaly to the south. A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 3 • Excavate five trenches to bedrock across the northern >20 ppb Au trend at approximately 200m spacing, subject to access, heritage, environmental and regulatory requirements. • Use trench exposures to test bedrock gold tenor and continuity, obtain structural measurements and refine initial drill-hole orientations. • Undertake systematic rock-chip sampling along the southern gold trends and exposed mineralised rhyolite dykes. • Progress priority southern anomalies toward trenching if surface sampling confirms continuity and tenor. • Integrate the Western Zone results with mapping, LiDAR, historical datasets and the broader Mt Turner structural model to rank the new targets against the broader district-wide current target pipeline. The timing and scale of follow-up activities remain subject to technical reviews, permitting, access and capital allocation. Western Zone Results – Two Distinct Gold Target Areas The following section is supported by relevant figures, tables and Appendices. The Western Zone is a five-kilometre-long arcuate feature, NNE-trending in the south, turning NNW further to the north. It is interpreted as a structural corridor on the western margin of the Mt Turner porphyry system. The corridor comprises faulted Proterozoic metasediments and granite intruded by rhyolite dykes, a priority target as the focus for precious-metal-bearing hydrothermal fluids, Figure 2. In July 2026 a total of 551 soil samples were collected on nominal 200m-spaced lines at 20m sample intervals. The results were interpreted using gold and pathfinder-element distributions, including a (Cu×Bi/As) thermal vector ratio used by the Company to assist in identifying a higher-temperature core of the hydrothermal system. A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 4 Figure 2. Western Zone structural setting and soil sampling blocks (Western Zone Analysis Report, August 2026) over LiDAR (Digital Elevation Model). Northern Target – Large Zoned Hydrothermal System Interpretation of Blocks 1 and 2 has outlined a large and coherent geochemical footprint with strong structural and lithological control: • A high-temperature thermal vector ratio (Cu×Bi/As) anomaly extends approximately 1,400m along strike and is up to 140m wide. It is closed to the northwest and southeast but remains open to the east. A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 5 • Along a 1,000m section there is a continuous >20 ppb Au anomaly along the western margin of the thermal vector anomaly and ranges from approximately 20m to 80m wide. It remains open to the south. • Coherent metal zonation: Gold overlaps an arsenic-bearing interpreted transition zone, while arsenic-lead-zinc anomalism extends northwest into the interpreted distal portion of the system. • Supporting field evidence: Gossanous breccia float and a narrow siliceous gossan containing bismutite and cuprite occur within the anomalous corridor and are interpreted as indications of potential higher-temperature feeder structures. The Company interprets the integrated pattern as consistent with an intrusion-related gold system (“IRGS”), with the highest-priority target located along the interpreted western transition zone where the >20 ppb Au contour overlaps the high-temperature vector (Cu×Bi/As) anomaly. The interpretation is preliminary and requires confirmation by additional surface sampling, trenching, and drilling. Northern Geochemical Zonation The northern results display a systematic metal distribution from a hotter, interpreted proximal domain in the southeast towards a cooler, more distal domain to the northwest, Figure 3. The high-temperature vector contour forms the core of the interpreted hydrothermal system. Gold is concentrated along its western flank, where it overlaps a narrow arsenic and zinc response. Further northwest, beyond Dingo Hill, arsenic transitions into a broader lead- zinc zone of anomalism. The arsenic anomaly exceeds 30 ppm over approximately 1,400m and is contiguous with the >20 ppb Au anomaly for approximately 600m in the southeast. The more distal lead- zinc response extends for approximately 1,000m and remains open to the northwest. Although this distal base-metal zone is not considered the primary gold target, its position and continuity support the interpretation of an organised, laterally extensive hydrothermal system rather than isolated geochemical highs. The linear character of the gold and pathfinder responses indicates strong structural control. Importantly, the gold anomaly is positioned at the interpreted thermal transition rather than at the centre of the high-temperature response. This relationship provides a well-defined target zone for trench orientation and subsequent drill design. A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 6 Figure 3. Western Zone - Northern soil geochemistry. Gold >20 ppb is shown in yellow. Southern Target – Multiple Epithermal-Style Gold Trends Within southern Blocks 3 and 4 the company has defined a different style of gold in soil anomalism potentially associated with rhyolite dykes. See Figure 4: • Four parallel gold trends: Four, sub-parallel, north-trending anomalous gold zones delineated, up to 40m wide and extend 200–300m along strike. A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 7 • Gold response: Soil assays exceed 20 ppb Au and peak at 330 ppb Au (sample 106663) in southern Block 4. • Geological association: The gold trends are closely associated with anomalous arsenic and are spatially associated with altered, brecciated and mineralised rhyolite dykes observed in rock chip sampling. • A Supporting rock-chip result: 2026 rock-chip sample #106064 (Lab Cert TV26251464) of silicified and brecciated rhyolite returned 1.19 g/t Au, 38.80 g/t Ag, 5,540 ppm As, 1.32% Pb and 903 ppm Sb The Au-Ag-As-Sb association, together with comparatively low copper and bismuth, is interpreted to indicate a lower-temperature, epithermal-style environment distinct from the northern target. Systematic surface sampling is required to determine whether the mineralisation has sufficient continuity and tenor to justify drill testing. Southern Target Geometry and Interpretation The four, sub-parallel gold trends are oriented broadly north-south and oblique to the main north-northeast Western Zone structural trend, Figure 4. This geometry is consistent with the development of en-echelon tensional zones developed during movement on the principal structure. Altered rhyolite dykes occupy several of these trends and may have provided fracture and a mineralising fluid pathway. A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 8 Figure 4. Western Zone - Southern soil geochemistry integrated with LiDAR terrain, showing multiple sub-parallel gold trends. Structural and Geological Framework Mt Turner is interpreted as a large intrusive-centered “Back Arc Copper Gold Porphyry” mineral system overprinted by multiple structural events. Regionally, several major structural orientations are recognised from LiDAR, dyke distribution and field mapping: • The northwest-trending Dingo Hill trend; • Northeast-trending Western Zone, Red Hills and Dinki Di trends; • North to north-northeast trends including the Cobar Line and northern Western Zone; • The east-west Drummer Fault corridor. A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 9 These intersecting structures are interpreted to represent an early conjugate fault system that localised late-stage felsic intrusions and associated dyke swarms. Later, north-south extension and structural reactivation created brittle fracture pathways capable of focusing hydrothermal fluids.This model provides a geological basis for the development of sheeted veins, breccias and subsidiary stockwork zones, particularly at structural intersections, bends and lithological contacts. Program Design and Data acquisition and integration This announcement integrates 3 datasets as summarised in Table 1. See Appendices for Lab Assay certificates as well as a selection of anomalous summary tables. Exploration Program data collected Certificate Numbers # samples Soil Samples 2026 TV26251540 551 Rock Chip Samples 2026 TV26251464 27 Historical Reconnaissance Rock Chips 2019-2022* 8 Certificates 99 Total 677 Table 1. Summary of Data Acquisition, also see Appendices In 2026, soil geochemistry was selected as the primary reconnaissance method because substantial areas of the Western Zone contain outcrop and residual soils. At each site the field team recorded location, soil type, colour and evidence of basement exposure. Samples were screened to 180 microns and the fine fraction was submitted to ALS Townsville for low-level gold and multi-element analysis. The interpretation recognises that gold and copper may be mobile in deeply weathered, high-rainfall environments. Accordingly, the Company assessed gold together with less- mobile pathfinder elements. Bismuth is used as an indicator of higher-temperature, magmatic-derived fluids, while arsenic, lead, zinc and antimony assist in identifying transitional and lower-temperature parts of the system. For the purpose of this reconnaissance interpretation, 20 ppb Au was adopted as the anomalous contour, representing approximately four to five times interpreted local background. A thermal vector ratio (Cu×Bi/As) greater than 100 was used to map the interpreted higher-temperature core. Rock-Chip Results Support the Geochemical Model Twenty-seven reconnaissance rock-chip samples were collected during the 2026 soil program, of which five returned anomalous gold, Table 2. The results are selective samples of outcrop, float, veins, gossans and rhyolites (Figure 5). The rock chip results are not considered representative of average grade or true width of bedrock mineralisation. No estimate of mineralised width can be made from these samples. A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 10 Sample Easting Northing Au g/t Ag g/t As ppm Bi ppm Cu ppm Pb ppm Lithology 106051 756178 7979292 0.53 0.99 966 464 1,290 266 Quartz gossan vein 106058 755691 7978869 0.13 7.60 21 73 2,230 271 Gossanous breccia 106064 755811 7979257 1.19 38.8 5,540 55 208 13,150 Rhyolite breccia 106065 755835 7979131 0.37 4.02 337 12 307 584 Brecciated vein quartz 106073 756132 7982545 1.02 0.99 1,820 411 508 299 Gossanous breccia Table 2. 2026 Reconnaissance 5 rock-chip samples containing anomalous gold (lab certificate #TV26251464) subject to rounding. Figure 5. Western Zone – Recent and Historic Rock Chip Gold Results over LiDAR terrain model A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 11 Figure 6. Silicified and brecciated rhyolite, Rock Chip sample 106064, lab certificate #TV26251464 The July 2026 data analysis also integrated 99 historic reconnaissance rock-chip samples collected between 2019–2022 (refer to Figure 6 for example). Twenty four samples were anomalous in gold, silver and/or copper, with individual values up to 15.35 g/t Au, 198 g/t Ag and 22% Cu (sample DW1, Lab certificate #TV21179719, see Appendix). These historical samples are selective and spatially dispersed; they should not be interpreted as representing average grade, continuity or mining width. Distribution of Rock-Chip Anomalism When viewed spatially, the current and historical reconnaissance rock-chip results show a distribution broadly consistent with the soil geochemistry. The August 2026 data analysis identified four principal clusters or associations: • Northern soil corridor: Sporadic anomalous gold and silver samples occur within the NNW-trending Blocks 1 and 2 corridor, locally coincident with the northern soil anomaly and distal base-metal zonation. • Dingo Hill rhyolite breccia: Strong Au-As-Sb-Pb values occur within a narrow, north-trending rhyolite breccia zone west of Dingo Hill. • Central copper-gold association: A cluster of moderate to high gold values is associated with elevated copper near the central NNE Western Zone structure around 756250E, 7980100N. • Southern anomaly support: Moderate rock-chip gold values coincide with the en- echelon Au-As soil trends in southern Block 4. Overall, higher copper-bismuth associations dominate the northern and central parts of the corridor, consistent with a hotter magmatic environment. Gold-arsenic-antimony associations become more prominent in the south, consistent with the interpreted lower- temperature setting. This systematic change in metal association supports the broader zonation model but does not, by itself, establish grade continuity or economic mineralisation. Target Comparison and Priority Assessment A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 12 Attribute Western Zone - North Western Zone - South Primary target style Zoned, intrusion-related hydrothermal / IRGS-style system Rhyolite-associated, lower-temperature epithermal-style system Surface gold expression Continuous >20 ppb Au anomaly over approximately 1,000m; 20– 80m wide Four sub-parallel >20 ppb Au trends, each approximately 200–300m long and up to 40m wide Peak soil gold Continuous anomaly is the principal feature; individual maximum not stated in the source report 330 ppb Au Key pathfinders Bi-Cu thermal vector with transitional As and distal Pb-Zn zonation Au-Ag-As-Sb association; comparatively low Cu and Bi Structural control NNW corridor, granite- metasediment contact and Dingo Hill intersection N-trending tensional structures oblique to the main NNE corridor Current extent Gold opens south; thermal vector open east Multiple defined trends; continuity and wall-rock tenor require testing Priority follow-up Extension soils, five bedrock trenches, structural measurements and initial drill design Systematic rock-chip traverses followed by trenching where continuity is confirmed Table 3. Comparative summary of the two Western Zone gold target areas. Dimensions relate to surface geochemical anomalies, not mineralised widths. Figure 7 - Mt Turner Location Map – District Targets over LiDAR terrain model includes the Western Zone A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 13 Exploration Significance The Western Zone program (Figure 7) has delivered several outcomes relevant to the broader Mt Turner exploration strategy which consists of multiple target areas. • Target definition: The results convert a five-kilometre conceptual structural corridor into two defined target areas with measurable surface dimensions and a clear follow- up program. • Geological coherence: The northern response displays internal metal zonation expected from an organized large hydrothermal system, strengthening confidence in the target model. • Dataset integration: The combination of soil anomalies, altered intrusive rocks, gossanous breccias and reconnaissance rock-chip anomalism provides multiple independent results which re-affirm the geological model. • Capital efficiency: Both principal targets remain amenable to relatively low-cost surface work before committing to drilling. • District potential: The distinct elemental associations and interpreted mineralisation styles interpreted in the Western zone, northern and southern anomalies, indicate that the broader Mt Turner porphyry system is likely to host mineralisation formed at specific and different structural and thermal levels. References in the technical analysis to the potential scale of the targets are conceptual only. There has been insufficient exploration to determine whether a mineral deposit is present, and no assessment of reasonable prospects for eventual economic extraction has been completed. The immediate objective is to confirm bedrock mineralisation, continuity, geometry and tenor through staged surface exploration. References to Previous ASX Announcements • 16 April 2026 – Strategic Plan and Portfolio Simplification. • 26 May 2026 – Investor Presentation – Unlocking a New District-Scale Gold System. • 19 June 2026 – Drummer Fault Soil Sampling Delivers Multiple Phase 2 Drill Targets. • 22 June 2026 – Lightning Advances Second Major Gold Exploration Program at Mt Turner Ahead of Planned July Drilling. • 7 July 2026 – Lightning Completes Western Zone Soil Program, Advancing Phase 3 Drill Targeting. ~ Ends ~ This announcement has been authorised for release by the Board of Lightning Minerals Limited. For more information, please visit: lightningminerals.com.au Enquiries in relation to the announcement, please contact: Lightning Minerals Ltd (ASX: L1M) Corporate Storytime Troy Brice Paul Berson Managing Director Investor & Media Relations Phone +61 8 9429 8806 Phone +61 421 647 445 admin@lightningminerals.com.au paul@corporatestorytime.com A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 14 About Lightning Minerals Ltd (ASX: L1M) Lightning Minerals Limited is an Australian exploration and development company focused on advancing a portfolio of gold and copper assets in Tier 1 mining jurisdictions. The Company’s flagship asset is the wholly owned Mt Turner Gold Project in northern Queensland, which hosts a large-scale gold system extending over approximately 14km of strike along the prospective Drummer Fault. Mt Turner is the primary focus of exploration, with ongoing drilling aimed at progressing the project toward resource definition and development. Lightning Minerals also holds a pipeline of gold and copper projects across Australia, including assets in the Lachlan Fold Belt in New South Wales and the Eastern Goldfields of Western Australia, providing additional exploration upside and growth opportunities. The Company’s objective is to create long-term shareholder value through disciplined exploration, resource growth and the development of high-quality mineral assets. Location of Lightning Minerals Australian Gold and Copper Projects A. 32 Harrogate Street, West Leederville Perth, WA 6007 T. +61 (08) 9429 8806 E. admin@lightningminerals.com.au lightningminerals.com.au 15 FORWARD LOOKING STATEMENTS Information included in this release constitutes forward-looking statements. Often, but not always, forward looking statements can generally be identified by the use of forward-looking words such as “may”, “will”, “expect”, “intend”, “plan”, “estimate”, “anticipate”, “continue”, and “guidance”, or other similar words and may include, without limitation, statements regarding plans, strategies and objectives of management, anticipated production or construction commencement dates and expected costs or production outputs. Forward looking statements inherently involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance and achievements to differ materially from any future results, performance or achievements. Relevant factors may include, but are not limited to, changes in commodity prices, foreign exchange fluctuations and general economic conditions, increased costs and demand for production inputs, the speculative nature of exploration and project development, including the risks of obtaining necessary licences and permits and diminishing quantities or grades of reserves, political and social risks, changes to the regulatory framework within which the Company operates or may in the future operate, environmental conditions including extreme weather conditions, recruitment and retention of personnel, industrial relations issues and litigation. Forward looking statements are based on the Company and its management’s good faith assumptions relating to the financial, market, regulatory and other relevant environments that will exist and affect the Company’s business and operations in the future. The Company does not give any assurance that the assumptions on which forward looking statements are based will prove to be correct, or that the Company’s business or operations will not be affected in any material manner by these or other factors not foreseen or foreseeable by the Company or management or beyond the Company’s control. Although the Company attempts and has attempted to identify factors that would cause actual actions, events or results to differ materially from those disclosed in forward looking statements, there may be other factors that could cause actual results, performance, achievements or events not to be as anticipated, estimated or intended, and many events are beyond the reasonable control of the Company. Accordingly, readers are cautioned not to place undue reliance on forward looking statements. Forward looking statements in these materials speak only at the date of issue. Subject to any continuing obligations under applicable law or any relevant stock exchange listing rules, in providing this information the Company does not undertake any obligation to publicly update or revise any of the forward-looking statements or to advise of any change in events, conditions or circumstances on which any such statement is based. COMPETENT PERSONS STATEMENT The information contained herein that relates to exploration results is based on information compiled or reviewed by Mr Lee Spencer, who is a Competent Person and a member of the Australasian Institute of Mining and Metallurgy. Mr Spencer is a Director of TRS Management Pty Ltd, a contractor to the Company. Mr Spencer, B.Sc. (Hons) M.Sc. M.AusIMM, has sufficient experience which is relevant to the style of mineralisation and types of deposits under consideration and to the activity which he is undertaking to qualify as a Competent Persons as defined in the 2012 Edition of the ‘Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves’. Mr Spencer consents to the inclusion of his name in the matters based on the information in the form and context in which it appears. REFERENCES TO PREVIOUS ANNOUNCEMENTS The Company confirms that it is not aware of any new information or data that materially affects the information included in the original market announcements, and that all material assumptions and technical parameters have not materially changed. The Company also confirms that the form and context in which the Competent Person’s findings are presented have not been materially modified from the original market announcement. APPENDICES APPENDIX 1 – DATA SETS AND ALS CERTIFICATE NUMBERS Exploration Program data collected Certificate Numbers # samples Soil Samples 2026 TV26251540 551 Rock Chip Samples 2026 TV26251464) 27 Historical Reconnaissance Rock Chips 2019-2022* 8 Certificates (see below) 99 Total 677 Historical Certificate Numbers* TV 20095473 TV 21155167 TV 22164621 TV19152010 TV20095473 TV21179719 TV21271201 TV22142792 APPENDIX 2 - SUMMARY OF HISTORIC ANOMALOUS ROCK CHIP SAMPLES APPENDIX 3 – 2026 SOIL SAMPLES (COMPRISING 551 SAMPLES). NOT NECESSARY OR PRACTICAL TO LIST THESE. Certificate Sample No. Au Ag As Bi Cu Mo Pb Sb V W Zn Lithology 756353 7980173 TV21271201 104138 0.78 33 2530 318 1660 2 2540 157 20 10 2370 Breccia 755954 7980053 TV21271201 104140 1.12 5 3880 22 522 4 3600 99 10 5 2760 gossan 756253 7980165 TV21271201 104141 1.93 138 1860 5920 30400 7 13850 138 14 10 1020 gossan 756253 7980165 TV21271201 104142 1.34 130 1160 3610 9740 6 10850 94 20 10 1120 gossan 756119 7979872 TV22142792 104941 0.42 12.7 135 313 1695 1 4010 47 133 5 1355 gossan in granite 756245 7980103 TV22142792 104944 0.32 125 1100 667 16,400 2 1780 94 30 5 3050 gossan qtz vein 756253 7980162 TV22142792 104945 0.63 83.9 912 4150 21,500 4 3230 59 25 10 932 gossan. Qtz vein 756521 7981347 TV 22164621 104983 1.24 2.5 5810 154 934 6 198 44 7 10 593 gossan vein 755948 7980045 TV22142792 104938 5.51 15.7 2660 730 5510 6 14,400 163 7 5 2980 altered veined granite 756247 7980145 TV21271201 104133 0.83 44.9 1885 4620 1160 10 4140 50 19 50 97 quartz vein 756283 7980243 TV21271201 104134 0.16 1.9 1080 112 321 1 419 68 22 10 239 quartz vein 756228 7980052 TV21271201 104136 1.48 7.9 2030 694 1330 4 1360 50 73 20 1875 quartz vein 755829 7979449 TV21179719 DH 18 3.43 126 505 522 220000 4 19 24 70 10 146 quartz vein 756626 7981038 TV 21155167 MT 17 0.05 10.8 887 416 1470 29 948 25 7 20 294 quartz vein in schist 756115 7979551 TV22142792 104931 0.68 1.7 6720 154 792 3 29 31 142 5 196 breccia vein in schist 755406 7978852 TV22142792 104913 0.36 1.2 446 27 280 2 179 7 36 10 439 gossan vein in schist 755192 7982688 TV21179719 DW 1 15.35 13.1 10000 114 351 1 2900 140 15 5 988 polymict g-rBreccia 756208 7981999 TV 22164621 104986 1.03 29.3 8420 973 1320 1 14850 64 106 110 564 breccia 755202 7982331 TV21179719 DW 3 0.72 13.4 2750 150 578 3 3430 137 2 5 1250 rhyolite Breccia 755909 7982216 TV20095473 DF4 0.13 28.6 1080 2660 661 1 14100 11 3 20 207 gossan breccia; dingo hill 756067 7982144 TV21179719 DH 8 0.36 10.8 5770 153 4260 7 757 93 6 10