Announcement PDF PO Box 661 Nedlands WA 6009 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r ASX Release Buxton Resources Ltd (ASX: BUX, BUXO) 09 March 2026 Centurion: Direct Evidence of Proximal Cu-Au System • Detrital sulphide fragments confirmed with 5.6% Copper, 245 ppm Silver, and up to 3.3 ppm Gold • The sulphide angularity and fragmentation suggest the source is a proximal basement high • New age dating identifies an O’Callaghans Supersuite cluster (~630 Ma) of highly oxidised zircons - the same magmatic event responsible for Paterson Orogen deposits including Telfer, Winu, & Havieron. • Au-Cu prospectivity further supported by indicator mineral chemistry • Effective and low-cost drilling solution to test basement has been identified Buxton Resources is pleased to announce the results from ongoing analysis of samples from Buxton’s 2025 drillhole CN002DD. Of particular significance is the confirmation of detrital Cu-Ag-Bi-Au bearing sulphides and highly oxidised zircons indicating the Centurion Project hosts a fertile magmatic-hydrothermal mineral system with links to the world-class Paterson Orogen copper-gold deposits. Buxton Managing Director Marty Moloney commented: “Centurion now moves from a project of possibility to a project of proof. By identifying the same ‘magmatic DNA’ shared by world-class deposits including Telfer, Winu, and Havieron, we have validated Centurion’s potential to host a province-defining discovery. With a clear drilling solution now in hand, we have the confidence to aggressively target the source of these sulphides.” Figure 1: Thin-section photograph highlighting angular, fragmented (i.e. detrital) polyphase sulphides hosted in sandy sediments at the base of CN002DD (~799.5m depth, reflected light). See Table 1 for sulphide mineral abundance data. Buxton cautions that visual estimates of mineral abundance should never be considered a proxy or substitute for laboratory analyses where concentrations or grades are the factor of principal economic interest. Visual estimates also potentially provide no information regarding impurities or deleterious physical properties relevant to valuations. This Announcement is supported by a video overview from Managing Director Marty Moloney available on Buxton’s InvestorHub PO Box 661 Nedlands WA 6009 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r New Petrological and Geochemical Results Two heavy mineral concentrates were prepared from Buxton’s 2025 drillhole CN002DD sample. These concentrates were submitted for integrated analysis using LA-ICPMS for “indicator mineral” geochemical characterisation. The minerals analysed include zircon, sulphides, garnet, apatite, iron-oxides and tourmaline. Age dating of the zircons was also undertaken. A core sample of pebble conglomerate from the base of CN002DD was also submitted for petrographic and micro-XRF analysis. In summary, the combination of detrital copper-silver-gold-bismuth bearing sulphides, high-oxidation magmatic signatures, metal-enriched indicator minerals, and Paterson-equivalent ages confirms that the Centurion basement possesses the right age, the right chemistry, and the right alteration to host a major copper-gold system. A detailed overview of this work is provided as Appendix 1. Refined Drilling Approach Following a comprehensive review of local drill operator capability, Buxton has identified a contractor with capability to drill mud rotary to depths exceeding 810 metres with a single wheeled mud/diamond drilling rig. This will provide a safe and rapid means of penetrating the entire cover sequence, including any similarly loose sands to those which caused CN002DD to be abandoned. This will provide a rapid and cost-effective means to test the basement. Next Steps Buxton will now undertake geochemical analysis of the full cored sequence. Additional material from the basal sequence will be submitted for specialised mineral concentration aimed at preserving and recovering additional sulphide minerals for further LA-ICPMS analysis. Several geophysical surveys are planned for the upcoming field season including passive seismic surveys (following positive results from testing conducted in November 2025) and a ground MT survey aimed at detecting basement conductors, along with a review of the magnetic and gravity datasets using cutting-edge processing techniques. PO Box 661 Nedlands WA 6009 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r We look forward to providing shareholders with further updates from ongoing activities in due course. ---o0o--- This announcement is authorised by the Board of Buxton Resources Ltd. For further information, please contact: Martin Moloney Sam Wright Managing Director Company Secretary marty@buxtonresources.com.au sam@buxtonresources.com.au PO Box 661 Nedlands WA 6009 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r Appendix 1 : Technical Detail & Indicator Mineral Geochemistry Background Buxton has previously reported analytical results from the 2025 diamond drill hole CN002DD, which intersected (and was abandoned in) the basal sequence assigned to the Elsa Sandstone immediately overlying the Centurion geophysical target. Significant silver-dominant mineralization within this basal sequence was reported, highlighted by a 3.9-metre interval from 805 metres depth that returned 4.06 ppm silver (Ag). This interval also exhibited anomalous levels of critical pathfinder elements, including copper (Cu), molybdenum (Mo), rhenium (Re), zinc (Zn), and tungsten (W), which are geochemically diagnostic of fertile magmatic-hydrothermal systems ASX 2 Oct 2025. The presence of these elevated metal concentrations within the sandy matrix at the base of the cover sequence was initially interpreted as a potential geochemical halo or a secondary enrichment zone. However, subsequent integrated petrological and geochemical analysis (detailed below) has confirmed that these values are at least partly related to primary, detrital sulphide fragments—including angular chalcopyrite—sourced from a proximal Proterozoic basement high. This confirms that the silver and associated metals are not distal anomalies but represent the physical erosion of a nearby mineralized system, indicating that the source of the copper-gold mineralization is in the immediate vicinity of the drillhole. New Analysis This Announcement covers two areas of work on the CN002DD drill core: 1) Micro-XRF mapping (Figure 2) and petrographic analysis (Figure 3) of coarse sandstone with a pebble conglomerate band at 799.5-799.6m depth (uncut core photo previously reported as Fig 3 from ASX 11 Aug 2025); and 2) Preparation of a Heavy Mineral Concentrate (HMC) from the basal sands in CN002DD from which two rounds of Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICPMS) geochemical analysis were undertaken i. Trace element analysis of selected “indicator” minerals (Table 2). ii. U-Pb isotopic age dating & trace element analysis of zircons (Table 3). Detrital Copper, Silver & Gold Bearing Sulphides PO Box 661 Nedlands WA 6009 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r Several highly significant findings relate to sulphides identified in petrology and recovered into the HMC: • Angular Chalcopyrite: The petrographically observed chalcopyrite is clearly angular and fragmented, implying a detrital origin (Figure 3) and minimal transport distance. In a high-energy sedimentary environment, such minerals are chemically and physically unstable; their preservation confirms that the primary source of the mineralisation is the adjacent Proterozoic basement high in the immediate vicinity of CN002DD. • Metal Rich Sulphide: HMC sample CON1001 (805m – 808.9m) contains primary detrital chalcopyrite + pyrite with a significant metal suite including Cu (5.6%), Ag (245 ppm), As (2,543 ppm), Bi (442 ppm) & Au (0.54 ppm) from sulphide spot 3-046, with up to 3.3 ppm Au in spot 3-047. The association of Cu-Ag-Bi-As-Au within these sulphide grains is a diagnostic "fingerprint" of high-temperature hydrothermal fluids, confirming that the elevated silver in the sands (3.9m at 4.06 ppm Ag with anomalous Cu, Mo, Re, Zn and W ASX 2 Oct 2025) is not a distal secondary effect, but is at least partially hosted within primary (hypogene) sulphide mineral fragments eroded from a local basement high. Based on the bulk interval grade of 4.06 ppm Ag (previously reported) and the specific sulphide mineral grade of 245 ppm Ag (reported herein), the average abundance of silver-bearing sulphide in the interval would be approximately 1.66% by weight. This calculated sulphide abundance is substantially higher than uXRF mapping of the petrological sample (~0.1% combined, see Figure 2 & Table 1) suggesting that the metal enrichment detected by partial and total leach assays stems primarily from post-burial chemical dispersion processes (where these metals would be hosted in soluble salts) in comparison to the mechanical dispersion component indicated by the detrital sulphides. The fact that both effects are now observed in this sample is consistent with proximity to the basement source of these metals. PO Box 661 Nedlands WA 6009 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r Figure 2: CN002DD detail of core section at ~799.55m depth (up hole to the right). Top panel: core photo for reference. Bottom panel: Micro-XRF mineral mapping of pyrite (green) and chalcopyrite (red) at 100um pixel resolution. See Table 1 for sulphide mineral abundance data. The Micro-XRF mapping indicates that a substantial amount of chalcopyrite is present in the sandy matrix as trains of particles generally <100um in size. However, only two ablatable grains were recovered to the HMC (which was a sample from ~5m further downhole). These sulphide particles have a low likelihood of recovery through the “mineral sand” HMC process used for LA-ICPMS analysis reported herein (mineral sand HMC is aimed at Ti-Zr oxide recovery / characterisation). Buxton will process remaining samples from the Elsa sandstone using a specialised concentration protocol aimed at recovering more of these sulphide grains. Buxton cautions that visual estimates of mineral abundance should never be considered a proxy or substitute for laboratory analyses where concentrations or grades are the factor of principal economic interest. Visual estimates also potentially provide no information regarding impurities or deleterious physical properties relevant to valuations. PO Box 661 Nedlands WA 6009 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r Figure 3: Thin section photomicrographs of petrology sample. Chalcopyrite (yellow) and pyrite (cream) included in detrital lithic clast representing reworking from primary crystalline host. Pale green well rounded detrital tourmaline accessory grain to lower right also likely derived from a primary crystalline basement lithology. Two additional instances of chalcopyrite were observed along the deepest portion of the interval (inset). Chalcopyrite demonstrates angular, fragmentary, and fractured morphologies with fragmentary fines ranging from ~20-120 µm. Chalcopyrite shows long contacts with adjacent quartz sand grains and is therefore interpreted as a locally derived, detrital phase. Pyrite is trace in the lithic sandstone and shows similar morphological features to chalcopyrite with maximum observed grain sizes of 60 µm. The inset shows a second, relatively coarse, isolated chalcopyrite grain with pervasive fragmentation and long contacts to adjacent quartz grains. Photomicrograph & petrologic analysis by Robert Madden, Microanalysis Australia. Table 1: Visual estimates (via Tornado Micro-XRF) of sulphide and oxide mineralogy from CN002DD Hole ID From (m) To (m) Interval (m) (True Width) Mineralisation Style Visual Estimation of Minerals % Pyrite Chalcopyrite CN002DD 799.5 799.6 0.1 Disseminated, Detrital 0.028% 0.066% Buxton cautions that visual estimates of mineral abundance should never be considered a proxy or substitute for laboratory analyses where concentrations or grades are the factor of principal economic interest. Visual estimates also potentially provide no information regarding impurities or deleterious physical properties relevant to valuations. PO Box 661 Nedlands WA 6009 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r Zircon Chemistry: The "Paterson Pulse" Age dating of zircons from the basal sandstone has identified two major pulses of magmatic activity. While the majority are linked to the Musgrave-aged basement (~1.2 Ga), a critical 10% cluster correlates with the O’Callaghans Supersuite (654 – 603 Ma). This timing is identical to the formation of the world-class Telfer and Havieron deposits on the western margin of the Canning Basin. Furthermore, these zircons formed under highly oxidised conditions, matching the specific chemical signature of fertile, ore-forming magmas. • O’Callaghans Age Cluster (~630 Ma): Approximately 15% of concordant zircons match the age of the O’Callaghans Supersuite, the same magmatic event responsible for the giant Telfer, Winu and Havieron deposits1 . • High Oxidation State: Application of the Loucks Oxybarometer2 to this 630 Ma population returned an average ΔFMQ of +2.46 (max +3.27, Figure 5). This is significant because values above +1.5 are strongly associated with fertile, copper-gold mineralising magmatic systems. High U/Th ratios (avg. 1.27) also support derivation from an oxidised, hydrothermal system. • Fertile IOCG Signature: The Centurion O’Callaghans data exhibits a mean Ce/Ce* of ~287 and a mean Eu/Eu* of 0.32 (peaking at 0.49). This places the Centurion data comfortably inside the "Mineralised Hiltaba" field of Wade et al.3 (Ce/Ce* > 100 and Eu/Eu* > 0.3) and well above their “barren” regional thresholds. • Musgrave Basement: The dominant zircon population (~34%) matches the Pitjantjatjara Supersuite (~1.2 Ga). These grains show elevated U/Th ratios (>1.2), which, given their association with Zn-rich tourmaline and high-Mn apatite (see below) provides further evidence that the basement has undergone significant hydrothermal metasomatism. The Pitjantjatjara Supersuite is highly prospective for IOCG-style mineralisation4 , particularly in the case of Centurion as it is clearly overprinted by the younger O’Callaghans oxidized magmatic event. This multi-stage evolution provides the prerequisites for forming large-scale mineral systems. 1 Dalstra, H. J., Rochat, B., Couper, C., & Glasser, L. (2025). Au–Cu and Cu–Au mineralisation in the Northern Paterson Province, Western Australia; new insights into an important intrusion-related gold district. Australian Journal of Earth Sciences, 72(5-6), 763–794. https://doi.org/10.1080/08120099.2025.2514704 2 Loucks, R. R., Fiorentini, M. L., & Henríquez, G. J. (2020). New Magmatic Oxybarometer Using Trace Elements in Zircon. Journal of Petrology, 61(3), egaa034 3 Wade, C. E., Reid, A. J., & Payne, J. L. (2022). Zircon Trace Element Geochemistry as an Indicator of Magma Fertility in Iron Oxide Copper-Gold Provinces. Economic Geology, 117(7), 1545–1574. 4 Smithies, R. H., Kirkland, C. L., Cliff, J. B., Howard, H. M., & Belousova, E. A. (2015). Syn-exhumation magmatism in the Musgrave Province in the context of the 1220–1150 Ma Giles Event. Precambrian Research, 261, 227-243. PO Box 661 Nedlands WA 6009 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r Figure 4: Zircon U-Pb age dates (n = 41) from samples CON1001NM and CMR0144NM (filtering for grains with discordance between -15% and +15%) Key Observations from the Age Distribution: • O'Callaghans Supersuite (654 – 603 Ma): A distinct cluster is present in both samples is the critical "Paterson-equivalent" population. Despite being a smaller percentage of the total, these zircons are the "ore-fertility" markers given their mean ΔFMQ of +2.04 plus also their exceptionally high Cerium anomalies (Table 3) that confirm the presence of the same aged magmatic system that provided the hydrothermal engine for deposits like Telfer and Havieron. • Pitjantjatjara Supersuite (~1220 – 1150 Ma): This represents the dominant source for CON1001NM (12 concordant grains in this window). This population anchors the sample to the Musgrave-aged basement high identified as having a high hydrothermal overprint (high U/Th). • Wider Distribution: The graph also shows a broader spread of ages, typical for detrital sediment derived from a complex Proterozoic basement, but the concentration in the two highlighted supersuites reinforces the interpretation of a locally derived, fertile source. Both samples capture the same dual-age magmatic story, supporting the conclusion that the entire area around the Centurion drillhole is part of a significant, multi-stage hydrothermal province. PO Box 661 Nedlands WA 6009 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r Figure 5: Plot comparing Loucks Oxybarometer results that highlights the significant disparity in oxidation states between the different zircon populations at Centurion (spread of all 33 analyses shown in grey). Analysis of Oxidation States (ΔFMQ): 1. O'Callaghans Supersuite (603-654 Ma): This population shows the highest median and mean oxidation state, with values peaking well above the +1.5 ΔFMQ fertility threshold. These zircons represent the highly oxidized magmatic-hydrothermal engine linked to the Paterson- style copper-gold mineralization event. With a median of +2.04 ΔFMQ, it sits squarely within the peak "Fertility Window" (+1.5 to +2.5) of major IOCG deposits such as those from Gawler Craton5 . 2. Pitjantjatjara Supersuite (1150-1220 Ma): This dominant basement population clusters around a neutral oxidation state. While it provided a stable host and metal source, the primary magmatism was not as inherently "fertile" as the later Neoproterozoic overprint. 3. All Centurion Data: The project-wide distribution indicates typical average redox state (~+0.4 ΔFMQ), highlighting that the O'Callaghans magmatic event represents a distinct, high- oxidation pulse compared to the regional background. Targeting Insight: The O'Callaghans-aged magmas at Centurion possessed the necessary oxygen fugacity to prevent early sulfide precipitation, thereby maximizing the potential for copper and gold transport into a hydrothermal system. This geochemical fingerprint strongly supports the prospective nature of the O'Callaghans-aged components for Cu-Au style mineralization. 5 Wade, C. E., Payne, J. L., Barovich, K., Gilbert, S., Wade, B. P., Crowley, J. L., Reid, A., & Jagodzinski, E. A. (2022). "Zircon Trace Element Geochemistry as an Indicator of Magma Fertility in Iron Oxide Copper-Gold Provinces." Economic Geology, 117(3), 703–718. PO Box 661 Nedlands WA 6009 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r Indicator Minerals Confirm Extensive Hydrothermal System Results from LA-ICPMS chemistry of other minerals include: • Manganese Apatite Signature: Sample CMR0144 (444m – 450m) hosts hydrothermal apatite with extreme manganese levels (up to 5,425 ppm Mn), a classic "near-miss" indicator for proximal IOCG-style systems6 . • Zinc-Tin Pathfinders: Detrital iron-rich tourmaline is also enriched in zinc (up to 1854 ppm), manganese (up to 5880 ppm) and tin (up to 840 ppm). High Zn and Mn in tourmaline are common "halos" around hydrothermal centres. Such iron-rich tourmalines are often associated with the intense sodic-calcic and iron-metasomatism that characterizes the cores of large IOCG systems.7 • Manganese-Calcium-Tin Garnet enrichment: The garnet analyses reach 19.8 wt% Mn (a spessartine component) and these garnets have highly scattered LREE/HREE ratios. There is also a distinct population of high-calcium grains (up to 20.9 wt% Ca). Several grains show elevated tin levels, with a peak of 15.2 ppm Sn. These Sn-rich garnets likely crystallized from, or were altered by, highly fractionated magmatic-hydrothermal fluids, matching the Sn-Zn signature seen in the detrital tourmalines. Metamorphic (non-prospective) garnets from standard pelitic or granitic rocks typically contain <2 ppm Sn. Considering the two samples, CON1001 (from the end of hole) represents a greater concentration of "target" material (primary copper-gold ore fragments), while CMR0144 captures the "proximal alteration" footprint (high-Mn apatite and high-Ca garnets). In essence, the lower sediments appear sourcing from closer to the centre of a alteration system consistent with a magmatic-hydrothermal mineralisation event. These chemical "fingerprints" from indicator minerals cannot by themselves be considered definitive evidence of prospectivity for any given mineral system. However, in conjunction with the zircon, sulphide and petrographic evidence Buxton has collected from CN002DD, the chemistry of these other minerals does provide further support for the presence of a proximal mineralised system. 6 Mao, M., Zentilli, M., & Dickie, J. (2016). The geochemical and luminescence signatures of apatite from the magnetite- apatite and iron oxide-copper-gold deposits of the Chilean Iron Belt. Economic Geology, 111(4), 1003-1014. 7 Slack, J. F. (1996). Tourmaline associations with hydrothermal ore deposits. Reviews in Mineralogy and Geochemistry, 33(1), 559-643.. 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r Table 2: CN002DD LA-ICPMS trace element results (discussed analytes) from indicator minerals other than zircon (sample ID suffixes NM = non magnetic, M1 = weakest magnetic fraction, M2 = moderate magnetic fraction, M3 = most highly magnetic fraction) Label Sample Mineral Comment Ca ppm Mn ppm Fe ppm Cu ppm Zn ppm As ppm Ag ppm Sn ppm Au ppm Pb ppm Bi ppm spot1-001 CMR0144M1 Garnet 10500 11120 226900 -2 56 -1.0 0 6.0 -0.02 -0.1 -0.05 spot1-002 CMR0144M1 Garnet 209000 5360 151850 -2 9.5 -1 -0.2 12.4 -0.02 -0.1 -0.05 spot1-003 CMR0144M1 Garnet 11000 11690 228300 -2 56 -1 -0.2 6.4 -0.02 -0.1 -0.05 spot1-004 CMR0144M1 Garnet 14000 16580 216350 -2 78 -1 -0.2 6.4 -0.02 -0.1 -0.05 spot1-005 CMR0144M1 Garnet 8500 16885 216900 -2 148 -1 -0.2 6 -0.02 -0.1 -0.05 spot1-006 CMR0144M1 Garnet 11500 3950 215000 -2 82 -1 -0.2 5.2 -0.02 -0.1 -0.05 spot1-007 CMR0144M1 Garnet 16500 12065 224750 -2 68.5 -1 -0.2 6.2 -0.02 -0.1 -0.05 spot1-008 CMR0144M1 Garnet 13000 9170 214400 -2 57.5 -1 -0.2 5.8 -0.02 -0.1 -0.05 spot1-009 CMR0144M1 Garnet 11000 11830 209800 -2 153 -1 -0.2 5.6 -0.02 -0.1 -0.05 spot1-010 CMR0144M1 Garnet 13000 16585 229450 -2 98.5 -1 -0.2 5.4 -0.02 -0.1 -0.05 spot1-011 CMR0144M1 Garnet 16500 9355 224400 -2 80.5 -1 -0.2 5.8 -0.02 0.1 -0.05 spot1-012 CMR0144M1 Garnet 11000 32620 219000 -2 35.5 -1 -0.2 6.6 -0.02 -0.1 -0.05 spot1-013 CMR0144M1 Garnet 10500 14430 233000 -2 76.5 -1 -0.2 6.4 -0.02 -0.1 -0.05 spot1-014 CMR0144M1 Garnet 6000 16400 225200 -2 33 -1 -0.2 6.6 -0.02 0.1 -0.05 spot1-015 CMR0144M3 Garnet 38000 14880 198350 -2 60 -1 -0.2 6.4 -0.02 -0.1 -0.05 spot1-016 CMR0144M3 Garnet 29500 13960 225300 -2 50.5 -1 -0.2 6.8 -0.02 -0.1 -0.05 spot1-017 CMR0144M3 Garnet 36000 15440 200750 -2 46.5 -1 -0.2 7 -0.02 -0.1 -0.05 spot1-018 CMR0144M3 Garnet 47500 62110 175600 -2 73 -1 -0.2 7.2 -0.02 -0.1 -0.05 spot1-019 CMR0144M3 Garnet 40500 11785 205300 -2 56.5 -1 -0.2 7.4 -0.02 -0.1 -0.05 spot1-020 CMR0144M3 Garnet 35500 14215 205600 -2 34.5 -1 -0.2 7.6 -0.02 -0.1 -0.05 spot1-021 CMR0144M3 Garnet 29000 22045 204600 -2 42 -1 -0.2 7.4 -0.02 0.1 -0.05 spot1-022 CMR0144M3 Garnet 29500 13240 202400 -2 49 -1 -0.2 6.4 -0.02 -0.1 -0.05 spot1-023 CMR0144M3 Garnet 34000 15895 197350 -2 122.5 -1 -0.2 6.6 -0.02 -0.1 -0.05 spot1-024 CMR0144M3 Garnet 27000 11010 200550 -2 56.5 -1 -0.2 7 -0.02 -0.1 -0.05 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r Label Sample Mineral Comment Ca ppm Mn ppm Fe ppm Cu ppm Zn ppm As ppm Ag ppm Sn ppm Au ppm Pb ppm Bi ppm spot1-025 CMR0144M3 Garnet 41000 12585 201850 -2 48 -1 -0.2 6.4 -0.02 0.1 -0.05 spot2-001 CON1001M1 Garnet Ablation penetrated into the glass slide 40500 68575 128150 6 30.0 -1 -0.2 21.6 -0.02 2.3 -0.05 spot2-002 CON1001M1 Garnet Ablation penetrated into the glass slide 17000 268805 15600 4 47 4 -0.2 3.2 0.02 0.7 -0.05 spot2-003 CON1001M1 Garnet 6000 154040 132150 -2 256 -1 -0.2 1.6 -0.02 0.3 -0.05 spot2-004 CON1001M1 Garnet Ablation penetrated into the glass slide 5500 194350 125050 4 136 2 -0.2 3.2 -0.02 1.3 0.35 spot2-005 CON1001M1 Garnet 7500 10795 244650 -2 69 -1 -0.2 1.4 -0.02 -0.1 -0.05 spot2-006 CON1001M1 Garnet 61500 112365 136300 -2 20 -1 -0.2 1.2 -0.02 0.5 -0.05 spot2-007 CON1001M1 Garnet Ablation penetrated into the glass slide 65500 1010 1300 8 23 -1 -0.2 27.2 -0.02 4.7 -0.05 spot2-008 CON1001M1 Garnet 50000 105845 154200 -2 49 -1 -0.2 1.2 -0.02 -0.1 -0.05 spot2-009 CON1001M1 Garnet Ablation penetrated into the glass slide 15000 274170 48050 -2 7 2 -0.2 1.6 -0.02 -0.1 -0.05 spot2-010 CON1001M1 Garnet Ablation penetrated into the glass slide 18500 117385 166900 4 50.5 -1 0.6 4.8 -0.02 0.7 -0.05 spot2-011 CON1001M2 Garnet 10500 2555 211800 -2 218 -1 -0.2 1.2 -0.02 1.2 -0.05 spot2-012 CON1001M2 Garnet 10000 5520 214200 -2 365 -1 -0.2 1 -0.02 0.2 -0.05 spot2-013 CON1001M2 Garnet Ablation penetrated into the glass slide 8500 7920 219800 2 155.5 -1 0.2 0.6 -0.02 2.5 -0.05 spot2-014 CON1001M2 Garnet 9000 2200 208850 2 265.5 -1 -0.2 1 -0.02 3.9 -0.05 spot2-015 CON1001M2 Garnet 64500 171220 73950 -2 27.5 -1 -0.2 2 -0.02 0.8 0.05 spot2-016 CON1001M2 Garnet 43000 112950 148000 -2 84.5 3 -0.2 2 -0.02 0.8 -0.05 spot2-017 CON1001M2 Garnet 9000 5710 215950 -2 297.5 -1 -0.2 1.2 -0.02 0.2 -0.05 spot2-018 CON1001M2 Garnet Too small for the spot size, Ablation penetrated into the glass slide 12500 3745 189750 16 105.5 2 -0.2 8.8 -0.02 39.1 0.35 spot2-019 CON1001M2 Garnet Ablation penetrated into the glass slide 10500 6065 210750 12 105.5 -1 0.4 6.2 -0.02 4.6 0.1 spot2-020 CON1001M2 Garnet 10000 2320 196450 -2 421.5 -1 -0.2 1.2 -0.02 -0.1 -0.05 spot2-021 CON1001M2 Garnet 4500 164565 151900 -2 413.5 -1 0.2 15.2 -0.02 -0.1 -0.05 spot2-022 CON1001M2 Garnet 14000 115705 154450 -2 48.5 12 -0.2 1.4 -0.02 -0.1 0.05 spot2-023 CON1001M2 Garnet 31000 198225 59450 -2 126.5 -1 -0.2 0.8 -0.02 -0.1 -0.05 spot2-024 CON1001M2 Fe-Oxides -500 120 710350 14 51.5 -1 -0.2 1.2 -0.02 4.9 -0.05 15 Robinson Av Belmont WA 6104 T: 08-9380 6063 E: info@buxtonresources.com.au W: www.buxtonresources.com.au View online: https://buxtonresources.com.au/link/y1gk6r Label Sample Mineral Comment Ca ppm Mn ppm Fe ppm Cu ppm Zn ppm As ppm Ag ppm Sn ppm Au ppm Pb ppm Bi ppm spot2-025 CON1001M2 Fe-Oxides 1500 85 600950 134 62.5 106 1 2.2 -0.02 8.3 0.05 spot2-026 CON1001M2 Fe-Oxides Ablation penetrated into the glass slide 1500 85 592550 158 230.5 135 0.8 1 -0.02 9.4 -0.05 spot2-027 CON1001M2 Fe-Oxides -500 750 713250 -2 52.5 -1 -0.2 0.8 -0.02 0.7 -0.05 spot2-028 CON1001M2 Fe-Oxides -500 295 703550 -2 27 6 -0.2 17.2 -0.02 123.9 3.65 spot2-029 CON1001M2 Fe-Oxides -500 1255 708550 2 153.5 14 -0.2 6.8 -0.02 137.2 7.95 spot2-030 CON1001M2 Fe-Oxides Ablation penetrated into the glass slide 21000 925 419500 38 142 33 0.6 17.2 -0.02 103.1 2.3 spot2-031 CON1001M2 Fe-Oxides -500 575 711200 2 64 13 -0.2 7.2 -0.02 43.7 3.75 spot2-032 CON1001M2 Fe-Oxides Ablation penetrated into the glass slide 8000 5810 542150 588 1300.5 6 0.4 9 -0.02 499.9 2.95 spot2-033 CON1001M2 Fe-Oxides -500 225 713200 2 74 2 -0.2 0.8 -0.02 12.3 0.15 spot2-034 CON1001M2 Fe-Oxides -500 2565 710050 4 51.5 13 -0.2 4.2 -0.02 33.4 3.8 spot2-035 CON1001M2 Fe-Oxides -500 3420 709850 -2 10 18 -0.2 6.8 -0.02 152.7 4.7 spot2-036 CON1001M2 Fe-Oxides -500 870 711050 4 53 13 -0.2 14.2 -0.02 106.8 12.25 spot2-037 CON1001M2 Fe-Oxides Ablation penetrated into the glass slide 14500 400 523650 40 84 32 -0.2 14.4 -0.02 36.9 0.8 spot2-038 CON1001M2 Fe-Oxides -500 260 673850 -2 22 38 -0.2 10.8 -0.02 56.7 21.9 spot2-039 CON1001M2 Fe-Oxides -500 1045 709950 -2 5587.5 -1 -0.2 1.4 0.02 93.8 -0.05 spot2-040 CON1001M2 Tourmaline 2000 885 113900 -2 626.5 -1 -0.2 16.8 0.02 18.8 0.15 spot2-041 CON1001M2 Tourmaline 3000 360 68650 -2 256.5 -1 -0.2 3.8 -0.02 4 -0.05 spot2-042 CON1001M2 Tourmaline 5000 485 75200 -2 251 -1 -0.2 26.2 -0.02 4.1 -0.05 spot2-043 CON1001M2 Tourmaline 3000 775 80800 -2 698.5 -1 -0.2 11.2 0.02 4.8 -0.05 spot2-044 CON1001M2 Tourmaline 2000 1535 117300 -2 137 1 -0.2 29.4 -0.02 2.9 0.1 spot2-045 CON1001M2 Tourmaline 1000 1710 96300 -2 411.5 -1 -0.2 7.4 -0.02 0.7 -0.05 spot2-046 CON1001M2 Tourmaline 1000 2375 111150 -2 281.5 2 -0.2 121.4 -0.02 1.8 -0.05 spot2-047 CON1001M2 Tourmaline 6000 305 58750 -2 215.5 -1 -0.2 5.6 -0.02 3.3 -0.05 spot2-048 CON1001M2