The Cinto Copper Project consists of seven tenements totalling 3,200ha in the highly prospective southern Peruvian Copper belt, located some 15km to the southeast of the world class Toquepala Au/Ag/Cu/Mo Porphyry Mine.
The northern permits are underlain by igneous rocks of the Cretaceous Toquepala Group and the late Cretaceous-early Tertiary batholith related to the Toquepala porphyry mine some 15km to the northwest.
The regional Incapuquio fault crosses the permits and the underlying igneous rocks are covered by recent sediments, generally south of the fault and increasing in thickness to the southwest.
Several zones of hydrothermal alteration in the concessions are noted in published geological maps.
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