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Western Metallica Drills Large Multiphase Porphyry System at Its Caña Brava Cu-Mo Project In Peru

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Western Metallica Resources Corp.
Western Metallica Resources Corp.

TORONTO, Jan. 14, 2025 (GLOBE NEWSWIRE) -- Western Metallica Resources Corp. (TSXV: WMS) (“Western Metallica” or the “Company”) is pleased to report initial results from its ongoing drill program at the Luz Maria copper-molybdenum target, located within the Company’s 100%-owned Caña Brava Project, Northern Peru. The initial two completed drill holes hit at least two diorite intrusions and a polymictic hydrothermal breccia, displaying consistent strong potassic alteration, multiple vein systems and sulfide mineralization typical of Andean porphyry systems. Results from these two drill holes confirm homogeneous copper and molybdenum grades throughout the drill hole. A third drill hole intercepted 285 metres of quartz-monzonite and shows increasing alteration and mineralization intensity at depth. While most of the assays from this drilling program are pending, Company geologists believe that the intensity and extent of the alteration and mineralization system at Luz Maria indicates that the Company is operating within a major Cu-Mo porphyry system.

Drilling Highlights:

  • Three diamond drill holes have been completed to date at the Luz Maria prospect, all directed from the center of the surface geochemical anomaly to the center of the main chargeability anomaly. All drill holes intersected broad intervals of strongly altered intrusive rocks, with strongly developed potassic, phyllic and sodic alteration assemblages, typical of Andean porphyry systems.

  • The ongoing drill program is aimed at testing the copper-molybdenum mineralization found over an area of 500 metres by 300 metres, which represents less than 5% of the Luz Maria alteration footprint area defined so far, and is focused on a sector featuring strongly altered diorite and quartz-monzonite outcrops coincident with strong magnetic and chargeability anomalies identified by drone magnetic and Induced Polarization surveys completed during 2024.

  • Drill hole LM24DD001, completed by contractor Energold to a depth of 396.1 metres, intersected 275 metres of an altered and mineralized diorite host rock with continuous and homogeneous grades averaging 400 ppm Cu and 100 ppm Mo.

  • Strong, pervasive secondary biotite is observed throughout drill hole LM24DD001, often overprinted by a phyllic alteration assemblage of quartz and sericite. Mineralization occurs as chalcopyrite and molybdenite both as disseminations and in a stockwork of Early Biotite (EB, refer to Figure 1) and B veins.

  • Drill hole LM24DD002 was completed to a depth of 329.7 meters, with increasing alteration intensity and veining. Results have been received for approximately 50% of the samples obtained from this hole. 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 veining (refer to Figure 2).