Pijilí Project

Located in southern Ecuador within the Camilo Ponce Enriquez Mining District, characterized as a Cu-Au (Mo) alkaline porphyry system from the Oligocene (31.19 +/- 0.13 Ma Re/Os), recently discovered near the Miocene Chaucha deposit in southern Ecuador. Initially, the main anomalies cover an area of 1.5 x 1 km, with a distribution of stockwork zones, quartz-pyrite-chalcopyrite veins, magnetites, chlorites, green sericite, and features of porphyry systems and post-episodic hydrothermal alteration assemblage, chloritic, as well as high-grade zones characterized by USTs with disseminated chalcopyrite and veins of up to 1% copper equivalent.