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Western Metallica Validates Copper Porphyry Potential by Completing Scout Drilling Program at its Caña Brava Cu-Mo Project In Peru

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Western Metallica Resources Corp.
Western Metallica Resources Corp.

TORONTO, Feb. 12, 2025 (GLOBE NEWSWIRE) -- Western Metallica Resources Corp. (TSXV: WMS) (“Western Metallica” or the “Company”) is pleased to report results from its inaugural scout drilling program at the Luz Maria copper-molybdenum target, located within the Company’s 100%-owned Caña Brava Project, Northern Peru. Full results from the three initial drill holes have been received, confirming homogeneous copper and molybdenum grades throughout. The increase in sulfide content, and the change from disseminated pyrrhotite dominated mineralization in drill holes LM24DD001 and LM24DD002, to a stockwork of sulfide (pyrrhotite-pyrite-molybdenite-chalcopyrite) veinlets in drill hole LM24DD003, suggests an eastward vector towards a hotter centre of the porphyry system. Such evidence confirms the prospectivity for a major porphyry style copper-molybdenum deposit, as similar signatures can be associated with large and economic copper systems along the Andean Belt.

Greg Duras, President and CEO of Western Metallica Resources, stated: “We believe that the initial 3-hole 1,056 metres of drilling completed as part of our maiden scout drilling program has only scratched the surface of the significant and unlocked potential for porphyry-related copper and molybdenum mineralization at Luz Maria. The exploration work conducted, and the data compiled to date by our technical team has already defined a WNW-ESE trending, 10-kilometre, unexplored structural corridor of porphyry-related targets, of which Luz Maria was the first to be drill tested. This initial program has tested only a portion of Luz Maria’s 2.7-kilometre-long alteration footprint, and we believe these results position us at the discovery stage of an Eocene-age porphyry belt in northern Peru.

Drilling Highlights:

  • The three diamond drill holes completed at the Luz Maria prospect all intersected broad intervals of strongly altered intrusive rocks, with well-developed potassic, phyllic and sodic alteration assemblages, typical of Andean porphyry systems (refer to table 1).

  • A total of 1,056.25 metres were drilled between October 2024 and early January 2025, strategically moving from West – from the site of the strongest regolith Cu and Mo anomaly coinciding with the outcrops of intrusive rocks - to East, where the unsupervised cluster classification 3D model, based on the geophysical data available, identified a high chargeability, high mag susceptibility and high metal factor (high chargeability / low resistivity) target under the sedimentary wall rock.

  • This first step scout drilling program only tested to a maximum depth of approximately 300 vertical metres and 300 metres on strike along the 2,700-metre-long major axis of the alteration footprint identified to date, representing approximately 5% of the Luz Maria anomaly.

  • Drill hole LM24DD003 was intended to continue well beyond the initially planned 350 metres to investigate the incipient strong alteration and increasing vein density at greater depth. Unfortunately, the hole did not reach target depth due to operational drilling difficulties.

  • The drill program has successfully proved that both the intrusive rocks, diorite in drill holes LM24DD001 and LM24DD002, quartz-monzonite in drill hole LM24DD003 and the sedimentary wall rock, all host homogeneous copper-molybdenum mineralization (refer to figures 3, 4, and 5) consistently along the length of the drill holes (400 ppm Cu and 100 ppm Mo in LM24DD001, 450ppm Cu and 100 ppm Mo in LM24DD002, and 350ppm Cu and 80 ppm Mo in LM24DD003), albeit in subeconomic quantities.

  • The rocks are strongly altered with biotite and pyrrhotite replacement of the ferromagnesian minerals, with a clear overprint by quartz-sericite alteration increasing progressively from West (LM24DD001) to East (LM24DD003).

  • Mineralization occurs as both chalcopyrite and molybdenite disseminations, and in stockworks of Early Biotite and B veins. The best result obtained so far is 1.8 metres at 0.2% Cu, from 146.7-148.50 metres, within a zone featuring high-density pyrrhotite-chalcopyrite infill and dissemination (refer press release dated January 14, 2025).

  • The increasing pyrrhotite at depth (refer to figures 1 and 2), and the stronger magnetic and chargeability signatures at depth, will support geological interpretation work aimed at targeting the hotter zones, closer to the porphyry source than the widespread low-grade mineralization and alteration found at Luz Maria (refer to figure 6).