Strategically located in the Miocene porphyry belt, near an operational Gold mine that has produced over 500,000 ounces of gold, Peru 0008 spans 800 hectares of exceptional exploration potential.
The property features widespread and intense quartz-sericite-tourmaline-pyrophyllite (dickite) alteration, indicative of a robust mineralizing system. Localized A-type and Maricunga-style quartz veining further highlight the deposit’s porphyry-epithermal transition zone.
Hydrothermal breccias, heavily silicified and enriched with tourmaline-sericite, deliver impressive grades of up to 3.1 g/t Au, 940 g/t Ag, 1.0% Cu, 2.3% Pb, and 2.7% Zn, showcasing the property’s high-grade potential.
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