Guardian Metal Rsrc. - Tempiute Mine Project – Significant Assay Results
RNS Number : 8628O
Guardian Metal Resources PLC
30 June 2025
30 June 2025
Guardian Metal Resources plc
('Guardian Metal' or the 'Company')
Tempiute Mine Project - Significant Assay Results
Very High Grade Tungsten and Gallium Mineralisation Confirmed Across Multiple High-Impact Project Areas
Guardian Metal Resources plc (LON:GMET, OTCQX:GMTLF), a strategic mineral exploration development company focused on tungsten in Nevada, USA, is pleased to announce assay results from the Tempiute tungsten project ("Tempiute" or the "Project") and newly staked exploration targets. Tempiute, formerly known as the Emerson Tungsten Mine, is located in south-central Nevada less than 250 miles (402 km) southeast of the Company's Pilot Mountain tungsten project.
As part of its systematic evaluation of Tempiute-historically one of the top tungsten-producing mines in the United States-Guardian Metal has identified multiple new zones of exposed tungsten mineralisation. Through direct claim staking, the Company has significantly expanded its land position by staking 31 additional Bureau of Land Management ("BLM") Mining Claims. Geochemical sampling of these newly identified areas has confirmed the presence of significant tungsten mineralisation. As a result, the Company has further strengthened its 100%-owned and optioned property portfolio across this exciting district.
Guardian Metal engaged Dr. Lawrence Carter to conduct a geological field review of the Tempiute Project and surrounding targets identified during the Company's recently completed regional desktop exploration programme. Dr. Carter's initial field observations, along with the Company's subsequent staking of additional claims to secure newly verified targets, were announced on 30 April 2025.1
Oliver Friesen, CEO of Guardian Metal, commented:
"These exciting results from Tempiute highlight how much untapped potential remains in one of America's most historically significant tungsten districts. As we continue advancing both Tempiute and Pilot Mountain at pace, Guardian Metal remains focused on a clear mission: to bring mined tungsten supply back to U.S. soil, reduce reliance on foreign sources, and help build a secure, resilient domestic supply chain for the future."
HIGHLIGHTS
§ High grade tungsten mineralisation confirmed along >1,300 m strike length of outcropping skarn at Tempiute where historic underground mining was carried out up to 350m below surface. Rock chip samples returned assay values up to 0.94% tungsten trioxide (WO3) (Table 1).
§ Notably, historical reports highlighted the gallium (Ga) potential across Tempiute but this metal was not routinely assessed. The Company's 2025 sampling has confirmed significant gallium results across the historically mined horizon with samples up to 90 ppm Ga.
§ High grade tungsten and gallium skarn mineralisation confirmed at newly claimed exploration targets named the 'East Zone' located along the east margins of the Tempiute north quartz monzonite stock including results up to 1.2% WO3 with 90 ppm Ga and 0.87% WO3 with 100 ppm Ga (Table 1). The 'East Zone' represents a new high-impact underexplored area for future exploration that is 100% owned.
§ New grab samples from "truck-ready" historic ore stockpiles contain up to 0.40% WO3 and 60 ppm Ga, and samples from a sulphide rich stockpile contained up to 7,960 ppm Zn. These supplement previous stockpile samples of up to 1.50% WO3 and 70 ppm Ga (Table 2).
§ Auger sampling of the historical Tempiute tailings material has identified strongly elevated results for gallium, tungsten and zinc down the entire 9.75 m deep auger hole (Table 3). Further auger test holes have already been commissioned and are underway.
§ Porphyry-style Mo mineralisation confirmed with zones of stockwork quartz-molybdenite-pyrite veins in quartz-sericite-pyrite (QSP) altered quartz monzonite veins containing up to 4,300 ppm Mo. Both north and south quartz monzonite intrusions are geochemically 'fertile' from a porphyry system perspective and further details will be covered in a future announcement.
§ High grade tungsten skarn mineralisation confirmed at the newly staked Worthington system with highlight results up to 2.66% WO3 along with 1.39% Zn and 2,110 ppm Mo (Table 4).
HIGH GRADE TUNGSTEN AND GALLIUM SKARN MINERALISATION AT TEMPIUTE
At the Tempiute mine area, garnet-pyroxene skarn was traced in outcrop for over a 1,300 m distance, along the contact between the south Cretaceous-aged quartz monazite intrusion and the host limestones. Rock chip samples were collected along the entire 1,300 m outcrop. Geochemical analysis confirmed consistent results >0.19% WO3 along the strike length, with sample highlights of up to of 0.94% WO3. Significantly, gallium (Ga) is also consistently >60 ppm along the strike length, with an individual sample returning a high of 90 ppm Ga (Table 1).
Dr. Carter's fieldwork identified multiple new zones of outcropping garnet skarn mineralisation along the southern, eastern, and northern margins of the north quartz monzonite stock. These newly discovered zones were subsequently secured through additional BLM claim staking by the Company. Rock-chip samples collected from these outcrops and newly acquired claims returned very high-grade tungsten and encouraging gallium values, including 1.20% WO₃ with 90 ppm Ga and 0.87% WO₃ with 100 ppm Ga. While some of these skarns show signs of limited historical mining, others appear entirely unworked. No evidence of past drilling was observed, suggesting these zones remain largely unexplored. As such, these new claims present a significant opportunity for Guardian Metal to enhance the value of the broader Project area.
Table 1: Summary of selected rock chip samples of outcropping skarn from across the Tempiute project.
| Sample ID | Latitude | Longitude | Lithology | WO3 (%) | Zn (ppm) | Mo (ppm) | Ga (ppm) |
| LC-TP-03* | 37.62968 | -115.62927 | Skarn, gossanous | 0.94 | 539 | 65 | 10 |
| LC-TP-05 | 37.65063 | -115.63186 | Skarn, coarse Mo | 0.02 | 403 | 50 | 60 |
| LC-TP-06 | 37.64087 | -115.63178 | Garnet skarn | 0.22 | 12200 | 98 | 90 |
| LC-TP-15 | 37.63397 | -115.63085 | Skarn, gossanous | 0.24 | 171 | 12 | 40 |
| LC-TP-17 | 37.63340 | -115.63028 | Garnet skarn | 0.11 | 202 | 11 | 70 |
| LC-TP-18 | 37.63452 | -115.63161 | Garnet skarn | 0.78 | 1315 | 703 | 60 |
| LC-TP-19 | 37.63487 | -115.63135 | Garnet skarn | 0.02 | 220 | 3 | 30 |
| LC-TP-20 | 37.63621 | -115.63325 | Skarn, coarse Mo | 0.03 | 1230 | 4190 | 20 |
| LC-TP-23 | 37.64268 | -115.62888 | Garnet skarn | 0.03 | 577 | 45 | 30 |
| LC-TP-24 | 37.64269 | -115.62890 | Garnet skarn | 0.70 | 22300 | 88 | 80 |
| LC-TP-26 | 37.64131 | -115.63099 | Banded skarn | 0.09 | 1530 | 10 | 50 |
| LC-TP-29 | 37.64012 | -115.63236 | Garnet skarn | 0.25 | 1075 | 9 | 70 |
| LC-TP-30 | 37.63220 | -115.62864 | Garnet skarn | 0.02 | 310 | 9 | 70 |
| LC-TP-31* | 37.63195 | -115.62870 | Garnet skarn | 0.04 | 181 | 7 | 50 |
| LC-TP-32* | 37.63141 | -115.62754 | Garnet skarn | 0.13 | 162 | 10 | 60 |
| LC-TP-33* | 37.63118 | -115.62632 | Gossan | 0.37 | 6260 | 88 | 10 |
| LC-TP-35* | 37.62960 | -115.62740 | Gossan | 0.27 | 3130 | 153 | 10 |
| LC-TP-41* | 37.65316 | -115.62138 | Garnet skarn | 0.02 | 822 | 4 | 70 |
| LC-TP-42* | 37.65155 | -115.62095 | Garnet skarn | 0.01 | 438 | 2 | 50 |
| LC-TP-43* | 37.65092 | -115.62080 | Garnet skarn | 1.20 | 4230 | 38 | 90 |
| LC-TP-45* | 37.64517 | -115.62265 | Garnet skarn | 0.87 | 4720 | 60 | 100 |
| LC-TP-46* | 37.64530 | -115.62312 | Garnet skarn | 0.05 | 1760 | 15 | 50 |
| LC-TP-50* | 37.65661 | -115.62527 | Garnet skarn | 0.03 | 669 | 15 | 40 |
| LC-TP-52 | 37.64216 | -115.62949 | Garnet skarn | 0.13 | 15050 | 53 | 40 |
| LC-TP-53 | 37.64218 | -115.62946 | Gossanous veins | 0.59 | 403 | 157 | 30 |
| Analysis by ALS' ME-ICP61. Samples over >1500 ppm W (>0.19 % WO3) re-run by ALS' XRF15c. W concentrations determined by ICP-AES converted to % WO3 by stoichiometric calculation. | |||||||
| Sample ID | Latitude | Longitude | Sample Description | WO3 (%) | Zn (ppm) | Cu (ppm) | Ga (ppm) |
| LC-TP-09 | 37.63723 | -115.62363 | Gossan stockpiled | 0.04 | 7960 | 214 | 10 |
| LC-TP-10 | 37.63777 | -115.62342 | Gossan stockpiled | 0.08 | 3020 | 90 | 20 |
| LC-TP-14 | 37.63449 | -115.63111 | Garnet skarn stockpiled | 0.15 | 282 | 1 | 30 |
| LC-TP-39 | 37.63934 | -115.63264 | Garnet skarn stockpiled | 0.33 | 39700 | 30 | 40 |
| LC-TP-40 | 37.63917 | -115.63282 | Garnet skarn stockpiled | 0.16 | 444 | 18 | 60 |
| LC-TP-54 | 37.65091 | -115.63121 | Coarse Garnet skarn stockpiled | 0.01 | 279 | 3 | 40 |
| LC-TP-55 | 37.65078 | -115.63142 | Banded skarn stockpiled | 0.40 | 1025 | 65 | 10 |
| OF-01* | 37.65069 | -115.63148 | Gossanous skarn, stockpiled | 0.37 | 1320 | 628 | 20 |
| OF-02* | 37.65065 | -115.63142 | Gossanous skarn, stockpiled | 0.55 | 523 | 479 | 20 |
| OF-03* | 37.64212 | -115.62945 | Semi-massive sulphide, stockpiled | 0.25 | 213 | 3580 | 20 |
| OF-04* | 37.64214 | -115.62943 | Garnet skarn, stockpiled | 0.04 | 139 | 43 | 80 |
| OF-05* | 37.63454 | -115.63109 | Skarn, coarse Mo, stockpiled | 0.11 | 648 | 24 | 30 |
| OF-06* | 37.63454 | -115.63109 | Garnet skarn, stockpiled | 0.48 | 2960 | 22 | 20 |
| OF-07* | 37.63644 | -115.63382 | Garnet skarn, stockpiled | 1.50 | 3720 | 32 | 60 |
| OF-09* | 37.63643 | -115.63381 | Semi-massive sulphide, stockpiled | 0.31 | 238 | 805 | 10 |
| OF-10* | 37.63643 | -115.63381 | Semi-massive sulphide, stockpiled | 0.03 | 259 | 1975 | 10 |
| OF-11* | 37.63952 | -115.63238 | Gossanous skarn, stockpiled | 0.36 | 768 | 1905 | 20 |
| OF-13* | 37.63958 | -115.63255 | Garnet skarn, stockpiled | 0.31 | 220 | 17 | 60 |
| OF-14* | 37.63957 | -115.63255 | Semi-massive sulphide, stockpiled | 0.01 | 366 | 1740 | 20 |
| OF-15* | 37.63920 | -115.63256 | Garnet skarn, stockpiled | 0.94 | 5510 | 24 | 70 |
| Analysis by ALS' ME-ICP61. Samples over >1500 ppm W (>0.19 % WO3) re-run by ALS' XRF15c. W concentrations determined by ICP-AES converted to % WO3 by stoichiometric calculation. *Previously collected samples, partly reported by the Company 18 December 20242 | |||||||
| Sample ID | Hole | Latitude | Longitude | WO3 (ppm) | Zn (ppm) | Ga (ppm) |
| TP-T-03 | DH-02 | 37.65941 | -115.64525 | 745 | 4840 | 30.3 |
| TP-T-05 | DH-02 | 37.65941 | -115.64525 | 510 | 4560 | 34.4 |
| TP-T-07 | DH-02 | 37.65941 | -115.64525 | 355 | 3090 | 41.5 |
| TP-T-09 | DH-02 | 37.65941 | -115.64525 | 292 | 2560 | 43.2 |
| TP-T-11 | DH-02 | 37.65941 | -115.64525 | 239 | 2390 | 42.4 |
| W and Ga analysis by ALS' ME-MS81. W concentrations determined by ICP-MS converted to % WO3 by stoichiometric calculation. Zn by ALS' ME-MS61L. | ||||||
| Sample ID | Latitude | Longitude | WO3 (%) | Zn (ppm) | Ag (g/t) | Cu (ppm) | Mo (ppm) |
| LC-WRT-01 | 37.95870 | -115.61130 | 2.66 | 13850 | <0.5 | 25 | 2110 |
| LC-WRT-07 | 37.95487 | -115.61055 | <0.1 | 1060 | 9.1 | 11 | 1 |
| Guardian Metal Resources plc Oliver Friesen (CEO) | Tel:+44 (0) 20 7583 8304 |
| Cairn Financial Advisers LLP Nominated Adviser Sandy Jamieson/Jo Turner/Louise O'Driscoll | Tel: +44 20 7213 0880 |
| Shard Capital Partners LLP Lead Broker Damon Heath/Erik Woolgar | Tel: +44 (0) 20 7186 9000 |
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