Announcement PDF ASX Announcement 1 July 2026 ASX: OD6 1 MULTIPLE NEW HIGH-PRIORITY DRILL TARGETS AT QUINN Outstanding Fluorine in soils confirm extensive mineralisation HIGHLIGHTS • Multiple new high-priority drill targets identified at Quinn Fluorspar • Exceptional fluorine-in-soil values of up to 31,800ppm F (~6.5% CaF₂) at North Horseshoe Canyon • Soil geochemistry now defines a fertile mineralised corridor extending more than 8 km with the Horseshoe to Spar corridor potentially linked over >1.5km core target area North Horseshoe Canyon - Newly discovered anomalies • Standout fluorine (F)-in-soil anomaly across a 150m strike length • Five soil samples >20,000ppm F, peaking at a standout 31,800ppm F indicating an immediate high-grade source proximal to the results. • Interpreted asa directcontinuation ofthe Big Jim occurrence on the SWside ofthe Lithocap, opening up a substantial >750m dip zone for testing North Horseshoe - Newly discovered anomalies • Strong fluorspar pathfinder anomalies pointing to continuations of the high-grade Horseshoe deposit beneath a silica cap, a compelling >400m target zone Big Jim to Spar Ridge Prospect • Robust fluorspar pathfinders defining an extensive >600m target zone Dress Circle Prospect • Newly identified epithermal alteration with high fluorspar pathfinder anomalies spanning a ~1000m target zone Frontispiece – see also Figure 2 for enlarged version. Cross-section from Horseshoe-Spar corridor 2 Managing Director Brett Hazelden, commented: "These results are a great outcome for OD6 and underscore the growing scale of our Quinn Fluorspar Project and demonstrate that mineralisation extends well beyond the historically mined deposits. The exceptional fluorine values at North Horseshoe Canyon, up to a 6.5% CaF2 peak in soils is interpreted as a continuation of the Big Jim occurrence over a substantial >750m target zone. These are well above grades you would expect to see a soil sampling program and strongly suggest the presence of a nearby high-grade source. Strong fluorspar pathfinders are also extending the high-grade Horseshoe deposit beneath the silica cap over 400m, providing multiple compelling drill targets. A ~1,000m epithermal corridor at Dress Circle and a >600m zone from Big Jim to Spar Ridge defines further large scale target zones. With multiple compelling targets now defined, we are building real momentum in our exploration program and look forward to unlocking further value for shareholders." OD6 Metals Limited (ASX: OD6) (“OD6” or “the Company”) is pleased to report the results of recent soil geochemistry focussed along the regional target alteration zone from Dress Circle to Mammoth at the Quinn Fluorspar Project located in Nevada, USA. About Quinn Fluorspar Project On 9 June 2026 the Company announced the exercise of the option agreement to acquire the Quinn Fluorspar Project, located approximately 220km north of Las Vegas, Nevada. The project offers very high-grade fluorspar mineralisation (>40% CaF2) identified at the Mammoth and Horseshoe Projects in replacement / breccia style mineralisation mapped out over large 9,000m2 and 3,000m2 areas respectively. In addition, a number of other fluorspar occurrences are noted in the wider project area with reported historic rock chip results up to 98.6% CaF2 (refer announcement 12 May 2026). Preliminary work by the Company has revealed Mammoth, Horseshoe and Big Jim to be very high grade and potentially significant deposits of fluorspar (refer presentation 20 May 2026 for summary and therein, a list of material announcements). The United States is currently 100% reliant on imports of fluorspar highlighting the strategic importance of domestic supply. Fluorspar is listed on the US Critical Minerals list with applications in battery technologies, AI chip manufacture, nuclear fuels industry, aerospace and defence technologies. The project is located ~300km by road from the US Strategic Minerals Reserve at Hawthorne, Nevada (refer to previous Company announcements) Recent soil sampling results As part of exploration surrounding the significant prospects at Horseshoe, Mammoth and Big Jim, the Company recently collected 320 soil samples at the Quinn Project. The soil program was designed to target areas outside of the main deposits in areas of epithermal alteration noted in satellite imagery. The key marker for fluorspar (CaF2) is assaying of fluorine (F) - CaF2 contains 48.9% fluorine by weight - with anomalism proximal to known and outcropping deposits such as Horseshoe and Mammoth ranging from 2,000 to 16,000 ppm fluorine. Results greater than 1,500ppm F are considered anomalous and worthy of follow up work. At Horseshoe, the fluorspar lies beneath a hard, largely barren “silica cap” — a layer of altered rock that formed above the fluorspar-rich zone. While this cap holds little fluorspar itself, it carries tell-tale traces of other elements that were left behind when the fluorspar formed in the rock below. The Company used a statistical method called principal component analysis (PCA) to combine eleven of these trace elements — rubidium, lithium, tin, thorium, yttrium, beryllium, barium, lanthanum, cerium, tungsten and fluorine — into a single score it calls “F-PC1”. A high F-PC1 score flags soil that is enriched in this whole “fingerprint” of fluorspar-related elements at the same 3 time. These elements are typically enriched in evolved acidic magmatic derived epithermal systems. This gives the Company a way to rank ground and pinpoint where fluorspar may be hidden beneath the surface. Surface soil results show an epithermal footprint extending for over 8 kilometres. A central zone, stretching from Horseshoe Mine through North Horseshoe and to Big Jim presents a highly prospective target area over 1.5km in strike length (Figure 1 & Figure 2). Figure 1 Fluorine in soils over regional geological mapping ASX Announcement 1 July 2026 ASX: OD6 4 Figure 2 Interpretative targeting cross-section from Horseshoe to Big Jim / Spar area showing the principal target zones over this highly fertile Fluorspar Corridor with conceptual drill plan. 5 Figure 3 Horseshoe to Big Jim – close up of soil results. Left image is F in soils, right image is F pathfinders in soils (F PC1). ASX Announcement 1 July 2026 ASX: OD6 6 North Horseshoe Canyon (NHC) and the importance of the Saw Mill Thrust North Horseshoe Canyon (NHC) is a narrow valley with exposed jasperoid (a highly silicified rock) on the south western side. There are historic reports of fluorspar occurrences in the canyon, though there is little evidence of historic workings. The fluorine in soils is likely derived from mineralized zones at the base of the jasperoid. The fluorine in soils in the NHC is remarkably high, and exceeds values recorded in the immediate vicinity of even the Horseshoe and Mammoth deposit areas. A zone of five samples recorded >20,000ppm F with a peak value of 31,800ppm F (Figure 3 & Figure 4). This area is slated for immediate follow up work. The jasperoid unit is considered to be a key marker of the Saw Mill Thrust (Figure 1 & Figure 2). The Saw Mill Thrust is a regional tectonic structure in the Central Nevada Thrust Belt (Bartley & Gleason, 1990). Whilst the thrust is considerably older than the mineralizing event, it acts as an aquitard restricting flow of epithermal fluids during mineralization and resulting in potential pooling of fluorspar beneath it. This is an analogous structure to the famous Roberts Mountain Thrust on the Carlin Gold Trend, which is a key control on Tertiary Carlin style gold deposits. The NHC jasperoids are very similar to those seen above the Big Jim prospect, and mineralization at Big Jim is now inferred to continue as a single target zone, beneath the Lithocap, through to North Horseshoe Canyon. This presents as a 750m shallowly dipping target zone, that potentially continues farther to the SW. North Horseshoe – high pathfinders and intrusions The North Horseshoe area represents a potential northerly continuation of the Horseshoe High-Grade Fluorspar occurrence and is located SW of the NHC. This region is characterized by significant alteration and a felsic intrusion has been noted on preliminary field excursions. Fluorine in soils range from 1000 to 1500ppm, however, the pathfinder elements (F PC1) are very strong and indicate the potential for mineralized continuations beneath the silica cap. The Saw Mill Thrust projects as 100 to 150m beneath the surface in this area and provides additional targets for continued mineralization from the North Horseshoe Canyon. Big Jim to Spar Ridge A soil line followed a ridge immediately north of the Big Jim prospect area towards the historic Spar Mine. The soil line was very strong in pathfinder elements, and is being prioritized for mapping and surface sampling. Dress Circle The Dress Circle area is a largely un-explored target area. Aerial and satellite imagery indicates considerable alteration associated with circular features resembling a potential intrusive centre or collapse caldera zone. Strong pathfinder anomalies in this area confirm the alteration, and expanded soil sampling is being planned. Horseshoe and Mammoth Soil lines, used to develop base-lines and to understand the relative magnitude of F in soils proximal to known deposits, were conducted over the Horseshoe and Mammoth areas. Both areas showed strong F in soil anomalies as well as the pathfinders. At Mammoth and Horseshoe, the fluorine anomalism ranged from 8,000ppm to >16,000ppm F. 7 Figure 4. Very high fluorine in soils in the North Horseshoe Canyon 8 Regional Setting, mineralization styles The Quinn Fluorspar deposits are part of the Great Basin (Basin and Range) of Nevada. The deposits are hosted in Paleozoic sediments including the Pogonip Limestone Formation and the Simonson Dolomite. Mesozoic to Cenozoic (Tertiary) intrusions and volcanism resulted in a significant epithermal event through the district. Fluorspar (CaF₂) is deposited in epithermal breccias, veins and as replacement deposits parallel to the bedding in the limestone. Figure 5 Quinn Fluorspar Project location in Nevada Next Steps • Finalise shareholder approval process • Receive pending assay results • Complete geological modelling and drill targeting • Integration into permitting activities • Lodge bulk sample permit applications • Commence metallurgical testwork programs • Prepare maiden drilling program 9 References Bartley, J.M., & Gleason, G., (1990). Tertiary normal faults superimposed on Mesozoic thrusts, Quinn Canyon and Grant Ranges, Nye County, Nevada. Geological Society of America, Memoir 176 (Chapter 9). Forward Looking Statements Certain information in this document refers to the intentions of OD6 Metals, however these are not intended to be forecasts, forward looking statements, or statements about the future matters for the purposes of the Corporations Act or any other applicable law. Statements regarding plans with respect to OD6 Metals projects are forward looking statements and can generally be identified by the use of words such as ‘project’, ‘foresee’, ‘plan’, ‘expect’, ‘aim’, ‘intend’, ‘anticipate’, ‘believe’, ‘estimate’, ‘may’, ‘should’, ‘will’ or similar expressions. There can be no assurance that the OD6 Metals plans for its projects will proceed as expected and there can be no assurance of future events which are subject to risk, uncertainties and other actions that may cause OD6 Metals actual results, performance, or achievements to differ from those referred to in this document. While the information contained in this document has been prepared in good faith, there can be given no assurance or guarantee that the occurrence of these events referred to in the document will occur as contemplated. Accordingly, to the maximum extent permitted by law, OD6 Metals and any of its affiliates and their directors, officers, employees, agents and advisors disclaim any liability whether direct or indirect, express or limited, contractual, tortuous, statutory or otherwise, in respect of, the accuracy, reliability or completeness of the information in this document, or likelihood of fulfilment of any forward-looking statement or any event or results expressed or implied in any forward-looking statement; and do not make any representation or warranty, express or implied, as to the accuracy, reliability or completeness of the information in this document, or likelihood of fulfilment of any forward-looking statement or any event or results expressed or implied in any forward-looking statement; and disclaim all responsibility and liability for these forward-looking statements (including, without limitation, liability for negligence). Competent Persons Statement Information in this report relating to field observations and soil sample results is based on information compiled by Dr Darren Holden who is a Fellow of the Australasian Institute of Mining and Metallurgy. Dr Holden is an employee of GeoSpy Pty Ltd and is a geological advisor to the Company and has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Personas defined by the 2012 Edition of the Australasian Code for reporting of Exploration Results, Mineral Resources and Ore Reserves. Dr Holden owns shares in the Company and participates in the Company’s employee securities incentive plan. Dr Holden consents to the inclusion of the data in the form and context in which it appears. No new information Except where explicitly stated, this announcement contains references to prior exploration results, all of which have been cross-referenced to previous market announcements made by the Company. The Company confirms that it is not aware of any new information or data that materially affects the information included in the relevant market announcements. The information in this report relating to the Mineral Resource estimate for the Splinter Rock Project is extracted from the Company’s ASX announcements dated 18 July 2024. OD6 confirms that it is not aware of any new information or data that materially affects the information included in the original announcement and that all material assumptions and technical parameters underpinning the Mineral Resource estimate continue to apply. This announcement has been authorised for release by the Board of OD6 Metals Limited. 10 About OD6 Metals OD6 Metals Ltd is an Australian critical minerals exploration and development company with projects spanning fluorspar, rare earth elements and copper across the United States and Australia. OD6 aims to position itself as an emerging supplier of strategically important critical minerals required for next-generation industrial, defence and energy technologies. Quinn Fluorspar Project – Nevada, USA OD6 is advancing the Quinn Fluorspar Project located in Nevada, USA, one of the world’s premier mining jurisdictions and currently ranked second globally in the Fraser Institute 2025 Mining Attractiveness Index. Quinn hosts multiple high-grade fluorspar deposits including Horseshoe, Mammoth and Big Jim, with historical drilling, channel sampling and testwork confirming significant high-grade mineralisation and potential for both Metspar and premium Acidspar products. Fluorspar is classified as a critical mineral in the United States, which currently imports 100% of all Fluorspar consumed domestically with >60% of all global supply sourced from China. It is essential in hydrofluoric acid production, AI semiconductor manufacturing, advanced battery technologies, uranium enrichment, defence systems and refrigerants. Splinter Rock Rare Earth Project – Western Australia OD6’s 100% owned Splinter Rock Rare Earth Project in Western Australia hosts one of Australia’s largest and highest-grade clay-hosted rare earth deposits, with a Mineral Resource Estimate of: • Indicated: 119Mt @ 1,632ppm TREO • Inferred: 563Mt @ 1,275ppm TREO OD6 is advancing an innovative processing flowsheet utilising heap leaching, nanofiltration and ion exchange technologies designed to achieved ~75% Nd & Pr overall recovery plus produce a high-quality Mixed Rare Earth Carbonate/Hydroxide product of ~56-59% TREO with low impurity levels Gulf Creek Copper Project – New South Wales OD6 is also advancing the Gulf Creek Copper-Zinc VMS Project in New South Wales, a historically high-grade copper mining district with significant exploration upside. Recent drilling and geophysical programs have confirmed high-grade copper mineralisation and identified multiple large- scale exploration targets along more than 10km of prospective strike. Corporate Directory Managing Director Non-Executive Chairman Non-Executive Director Financial Controller/ Joint Company Secretary Joint Company Secretary Technical Advisor to the Board Contact OD6 Metals Ltd ACN 654 839 602 www.od6metals.com.au Mail to: info@od6metals.com.au Phone: +61 8 6189 8515 Level 1, 1 Alvan Street, Subiaco, WA 6008 Corporate Directory Mr Brett Hazelden Mr Piers Lewis Dr Mitch Loan Mr Troy Cavanagh Mr Joel Ives Dr Darren Holden Investor Relations Investor Relations Lucas Robinson Corporate Storytime lucas@corporatestorytime.com Phone: +61 408 228 889 11 Appendix 1: results Table 1 Quinn Fluorspar Project Soil Sample Results (results >1000ppm F presented; all results shown on the figures). Coordinates in NAD83 Zone 11. Sample ID East North Rb ppm Li ppm Sn ppm Th ppm Y ppm Be ppm Ba ppm La ppm Ce ppm W ppm F ppm F_PC1 (score) 90637 615797 4220997 64.7 40.2 1.5 7.8 26.7 1.68 240 26.6 48.6 1.54 31800 9.81 90635 615803 4220983 65.3 48.9 1.5 8.8 20.5 1.6 230 24.1 44.7 1.22 28300 9.18 90638 615794 4221007 56.9 42.2 1.5 6.5 21.1 1.59 240 25.1 48.7 1.36 26400 7.76 90633 615815 4220959 59.5 38.2 1.3 8.2 16.6 1.34 290 24.6 45.3 1 21400 6.21 90634 615811 4220969 61.3 39.7 1.3 9.2 17.5 1.37 260 24.4 47.5 1.04 20800 6.50 113953 617872 4223651 65.9 47.5 1.3 10.8 22.6 2.18 200 31.3 56.2 0.92 16450 6.93 113951 617840 4223644 58.4 41.1 1.2 6.9 21 1.9 150 30.3 55.2 1.95 13150 6.17 113952 617858 4223643 60.5 32.8 1.1 8.1 16.65 1.7 190 24.2 51.6 0.71 11200 3.86 113701 615583 4220435 46.8 33.1 1.1 6.1 17.4 1.59 160 28.6 58.1 0.67 9920 2.90 113954 617907 4223669 60.8 31.8 1.2 10.2 17.85 1.2 200 28.3 57.5 0.94 8380 4.42 90552 615610 4220564 52.8 32.1 1.1 4.2 16.7 1.41 170 22.9 48.4 0.73 8090 2.22 90639 615782 4221019 42.4 33.7 1 4.5 15.2 1.19 170 21.2 41.3 0.89 7250 1.91 113718 615653 4220280 39.6 28.6 0.9 3.7 13.85 1.48 150 20.1 46.6 0.6 6900 0.73 113702 615567 4220419 48.8 32.1 1.2 7.1 16.6 1.48 170 25.5 59.3 0.78 6280 3.02 113717 615633 4220295 40.2 31.8 1.1 2.5 13.95 1.5 140 20.3 44.8 0.72 5860 1.03 113716 615624 4220299 48.3 35.3 1.3 6.6 18 1.76 170 25.7 60 0.64 5450 3.29 90558 615629 4220511 51.8 34.8 1.1 7 14.9 1.6 170 23 51.9 0.58 4900 2.26 90559 615618 4220518 48.4 36.3 1.1 3.1 16.1 1.47 160 22.9 52.9 0.8 4650 1.83 90646 615786 4221079 37.8 32.3 1.2 4.1 18.45 1.26 150 23.2 45.7 0.82 4440 1.91 90641 615772 4221048 40.9 29.6 0.9 3.8 15.9 1.2 170 21.1 41.9 0.65 3760 0.67 90632 615822 4220947 46 38.6 1 7.3 14.55 1.26 220 23.4 44.1 0.59 3440 2.47 90584 616160 4221602 27.2 27.5 1 3.1 13.6 1.17 120 18.8 41.2 0.47 3090 -0.91 90589 616205 4221676 34.6 28.6 1.3 4.1 19.7 1.72 110 28.4 61.2 0.6 3070 1.97 90631 615833 4220939 40.9 36.5 1 6.6 14.75 1.25 220 23.7 43.3 0.55 2820 1.90 113714 615591 4220329 45.7 31.9 1.1 8 15.45 1.53 190 24.8 63.1 0.62 2770 2.34 90648 615788 4221058 36.1 27.5 1 5.7 20.4 1.2 150 24.5 47.7 0.67 2700 1.26 90642 615771 4221059 40.5 28.8 0.9 3.2 15.55 1.21 160 21.3 41.8 0.56 2660 0.35 113715 615609 4220314 40.8 36.9 1.2 5.6 21.8 1.79 180 28.9 62 0.54 2590 2.87 113703 615555 4220407 42 31.3 1 2.9 12.35 1.15 150 20.3 50.4 0.79 2560 0.97 90647 615788 4221068 24.1 21.1 0.8 3.9 25.3 0.92 90 23.5 45.4 1.1 2550 0.40 90551 615606 4220567 44.8 29.2 1 4.4 17.25 1.36 170 24.1 52.9 0.6 2540 1.23 113866 615144 4218238 29.8 21.3 0.7 2.8 13.3 1.27 120 18.9 43.7 0.59 2540 -1.58 90560 615643 4220503 42.9 29.5 0.9 3.1 13.7 1.29 150 21.4 48.6 0.54 2520 0.25 113854 615834 4220984 32.4 23.3 0.8 1.1 10.2 0.91 120 15.3 32.3 0.52 2390 -2.11 113851 615813 4221017 44.1 27.7 1 3.4 13.65 1.15 190 21.6 45.3 0.47 2090 0.42 90586 616222 4221596 35.2 29 3.1 4.7 20.3 1.29 140 20.1 42.2 0.64 2020 2.79 90640 615777 4221037 36.2 26.6 0.9 3.3 16.4 1.18 160 22.7 44.1 0.6 1980 0.11 113957 617970 4223692 40.7 25.5 0.9 5.6 14.85 1.22 180 22.8 47.1 0.44 1880 0.26 113852 615817 4221005 41.5 27.4 1 2 13.75 1.12 170 20.3 42.8 0.47 1800 -0.11 12 Sample ID East North Rb ppm Li ppm Sn ppm Th ppm Y ppm Be ppm Ba ppm La ppm Ce ppm W ppm F ppm F_PC1 (score) 90554 615635 4220547 37.2 30.9 1 4.3 18.65 1.62 140 27 56.5 0.58 1800 1.08 90563 615675 4220525 40.5 26.1 0.8 3.1 11.3 1.08 150 17.8 39.5 0.58 1770 -0.68 90579 616187 4221702 43.2 37.9 1.9 5.3 24.5 2.09 120 30.8 75.8 0.69 1700 4.23 90557 615639 4220526 40 27.6 0.9 3.6 12.5 1.12 160 20.7 46.2 0.54 1650 -0.21 90595 616380 4221706 44.7 44.1 1.9 9.1 24 2.75 110 40.4 91.8 0.27 1640 5.14 90608 615815 4220724 18.7 10.1 1.8 7.5 37.7 1.74 170 19.9 52.7 0.78 1630 2.88 113875 615231 4218113 29.1 25.1 0.8 3.5 13.25 1.47 110 23.8 51 0.54 1630 -0.95 90581 616161 4221671 29.3 21.7 1.3 5.7 17.65 2.08 100 35.5 100.5 0.25 1520 1.29 90582 616143 4221659 32.1 25.4 1.4 4.1 17.9 1.58 110 27.4 55.5 0.46 1510 0.49 113855 615848 4220974 28.3 21.2 0.7 1.2 9.77 0.84 120 14.9 32.2 0.49 1490 -2.71 113743 615579 4218699 33.5 32.1 0.8 3.6 18.15 1.22 140 28.3 61 0.42 1480 0.48 90612 615745 4220663 15.4 8.5 1.1 5.9 46.3 2.69 50 17.6 38.8 0.49 1460 1.26 90609 615800 4220712 14.2 6.2 1.7 7.1 21.9 1.18 50 12.2 34.2 0.62 1450 -0.39 90580 616192 4221676 37.8 24.6 1.4 4.8 18.85 1.93 120 34.3 86.4 0.31 1300 1.68 113721 615911 4221583 30.5 26 1.3 7.2 11.3 0.66 100 17.2 41.3 0.58 1280 -0.70 90610 615783 4220703 22.4 9.5 1.4 8 14 1.21 60 13.8 38.6 0.53 1270 -0.90 113853 615830 4220992 37.8 24.4 0.8 1.1 11.4 0.93 150 17 37.4 0.46 1260 -1.54 90606 615831 4220748 17.8 9.6 1.3 5.1 25.5 1.31 140 15.7 45.1 0.57 1260 -0.14 113704 615543 4220392 36.8 29.4 1 4.2 13.35 1.15 160 21.3 49.8 0.68 1250 0.72 90553 615623 4220556 38 30.4 1 2.3 18.5 1.48 140 24.3 52.7 0.58 1240 0.51 90605 615833 4220774 11.2 7 1.7 6.2 24.8 2.87 50 13.2 29.7 0.45 1210 -0.56 90611 615759 4220688 25.4 10.9 1.1 5.2 14.7 1.68 90 14 32.6 0.48 1210 -1.34 90569 615952 4221737 34.7 31.3 1 5.2 39.4 2.47 120 85 165.5 0.39 1200 6.49 113750 615425 4218761 27.7 25.6 0.8 4.4 17.3 0.99 160 28.9 54.3 0.29 1200 -0.67 113804 616557 4221768 53 45.8 1.4 9.6 19.8 2.3 140 27.7 63.9 0.25 1200 3.81 113995 615056 4218204 29.4 17.5 0.9 4.6 15.25 1.28 120 22.8 46.7 0.29 1160 -1.52 90607 615823 4220737 23.8 12.3 1.3 4 20.3 1.05 100 15.2 39.4 0.68 1150 -0.53 113730 616006 4221290 34.4 32.4 1.1 6.5 21.7 1.16 140 23.9 54.2 0.77 1130 2.25 113749 615453 4218762 35.1 29.9 0.9 5.3 16.85 1.45 210 30.8 64.9 0.37 1130 1.24 113747 615488 4218740 39.6 28.8 1 5.3 16.2 1.46 160 29.7 55.6 0.3 1130 0.62 113808 615584 4218468 24.2 20.7 0.6 2.8 19.6 1.26 80 26.5 51.7 0.31 1130 -2.00 113801 616518 4221816 60.8 42.2 1.5 11.4 20.3 2.48 130 26.3 90.8 0.41 1120 5.95 90570 615984 4221742 35.6 36.2 1 3.8 23.7 2.09 130 35.5 74 0.42 1120 2.04 113862 615279 4218195 37.5 24.6 0.8 5.6 16.5 2.2 130 26.2 54.5 0.32 1120 0.41 90596 616427 4221724 53.1 37 1.6 10.7 22 2.34 160 41.1 104.5 0.29 1110 5.14 90573 616031 4221738 33.4 34.3 1.2 3.9 30.4 2.11 120 35.5 76.7 0.46 1100 2.55 90577 616136 4221716 36.8 30.5 1.1 4.2 25.6 1.94 150 36.8 86.8 0.45 1090 2.70 113873 615235 4218156 27 21.3 0.7 3.9 14.15 1.71 100 22.9 49.8 0.33 1090 -1.52 90644 615764 4221089 24.1 23.3 0.8 1.1 9.93 0.77 110 13.8 26.9 0.8 1070 -2.45 113857 615861 4220963 31.1 23.1 0.7 1.7 10.55 0.85 130 15.8 34.2 0.41 1070 -2.43 90599 616488 4221851 28.7 22.8 0.8 9.8 14 2.19 110 36.5 153.5 0.38 1060 2.49 90603 615817 4220830 24.8 12 1.1 4.1 16 1.34 80 16 35.7 0.47 1060 -1.81 13 Sample ID East North Rb ppm Li ppm Sn ppm Th ppm Y ppm Be ppm Ba ppm La ppm Ce ppm W ppm F ppm F_PC1 (score) 113997 615034 4218179 30.9 25.5 0.8 3.9 14.5 1.46 150 24.5 55.3 0.41 1060 -0.51 113876 615227 4218083 29.9 23.8 0.8 5.1 12.4 1.43 130 22.9 51.5 0.36 1050 -1.02 90572 616012 4221741 34.4 32.9 1.2 3.7 27.2 2.19 130 35.7 63.4 0.42 1040 2.01 90578 616167 4221708 29 24.9 1.6 3.9 25.8 2.45 100 27.4 58.5 0.34 1040 1.45 90583 616151 4221628 26.6 21.9 1.4 1.9 10.3 1.12 110 16.5 35.1 0.5 1040 -1.68 90564 615659 4220533 45.9 30 1 5.4 14.85 1.4 180 23.8 52.5 0.43 1040 0.94 113807 615600 4218473 23.7 18.2 0.6 3.9 15.45 1.08 90 24.5 51.3 0.34 1040 -2.29 90574 616061 4221734 38.7 34.1 1 4.1 28.8 2.25 140 43.3 88.7 0.38 1030 3.14 113731 616002 4221272 37.6 27.9 1 4.8 16.35 1.08 160 20.4 46.8 0.67 1030 0.67 113744 615558 4218705 31.3 30.4 0.8 4.3 14.1 1.18 130 25.6 54.3 0.38 1030 -0.57 113861 615297 4218182 36.5 22 0.8 3.8 16.5 2.18 110 25 54.4 0.39 1030 0.05 90556 615648 4220540 42.2 29.9 0.9 3.1 14.05 1.3 140 21.3 48.2 0.62 1020 0.15 113745 615531 4218717 32.3 30.5 0.9 5.7 13.7 1.37 140 27.4 57.9 0.41 1020 0.02 113998 615022 4218163 33.4 26.6 0.9 4.1 15.25 1.53 150 27.4 58.7 0.39 1020 0.08 114000 615019 4218136 34.9 23.7 0.9 6.6 15.25 1.4 160 27 58.1 0.34 1020 0.13 90616 615703 4220610 33.8 26.6 0.9 3.8 17.05 1.45 150 24.3 45.8 0.43 1010 0.07 90568 615691 4220587 30.7 22.4 0.8 2.2 11.6 0.94 140 17.7 39.6 0.49 1010 -1.91 90576 616111 4221718 36 27.9 1.1 3.7 26.3 1.88 130 40.2 93.1 0.5 1000 2.66 90594 616340 4221696 45.2 35.8 1.4 7 19.65 1.93 150 38.7 95 0.45 1000 3.74 113741 615921 4221231 35.6 26.8 1 5.6 18.9 0.97 140 24 52.4 0.8 1000 0.95 113817 615412 4218459 34.3 21.4 0.7 3.5 12.6 1.47 120 22.6 49.6 0.3 1000 -1.41 JORC 2012 – Table 1: Quinn Fluorspar Project Section 1 Sampling Techniques and Data (Criteria listed in the preceding section also apply to this section) z JORC Code explanation Commentary Sampling techniques • Nature and quality of sampling (eg cut channels, random chips, orspecific specialised industry standard measurement tools appropriate to the mineralsunderinvestigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling. • Include reference to measurestaken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. • Aspects of the determination of mineralisation that are Material to the Public Report. • In cases where ‘industry standard’ work has been done this would be relatively simple (eg ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or • Soil samples collected on Ridge and Spur soil lines by digging a small hole with a plastic spade to approximately B-Horizon • Sample sieved in the field to 6.35,, (1/4”) (and sieved again by the laboratory) 14 z JORC Code explanation Commentary mineralisation types (eg submarine nodules) may warrant disclosure of detailed information Drilling techniques • Drill type (eg core, reverse circulation, open- hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details(eg core diameter, triple or standard tube, depth of diamond tails, face- sampling bit or other type, whether core is oriented and if so, by what method, etc). • NA - no drilling reported in this release Drill sample recovery • Method of recording and assessing core and chip sample recoveriesand resultsassessed. • Measures taken to maximise sample recovery and ensure representative nature of the samples. • Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material. • NA - no drillingreported in this release Logging • Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. • Whetherlogging is qualitative orquantitative in nature. Core (or costean, channel, etc) photography. • The total length and percentage ofthe relevant intersections logged. • Sample descriptionson colourand soil type collected. Sub-sampling techniques and sample preparation • If core, whether cut or sawn and whether quarter, half or all core taken. • If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. • For all sample types, the nature, quality and appropriateness of the sample preparation technique. • Quality control procedures adopted for all sub- sampling stages to maximise representivity of samples. • Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second-half sampling. • Whether sample sizes are appropriate to the grain size of the material being sampled. • NA - no drilling reported in this release • Soil samplessieved at the laboratoryto 180 microns. Quality of assay data and laboratory tests • The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total. • For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrationsfactors applied and theirderivation, etc. • Nature of quality control procedures adopted (eg standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (ie lackof bias) and precision have been established. • Assays conducted by ALS Global Laboratories in Reno Nevada and Vancouver Canada. • Method F-IC881 to determine fluorine by KOH fusion and ion chromatography with detection limits of 20ppm to 20000ppm. Assays recor