silver

San Andrés

Overview The San Andrés project is located in the Puna de Jujuy, about 190 km from the capital city. Is located approximately 15 km from La Providencia Mine (next operation of Hanaq) and is accessed through a secondary road.San Andrés is a low to intermediate sulfidation deposit mainly containing Ag-Cu-Pb. The form of mineralization is…

Cerro Tinte

Overview Cerro Tinte is a low sulphidation epithermal deposit of Silver, Lead and Zinc composed from calcareous and pyroclastic rocks. It has banded structures reaching 3 meters of width with barite quartz and replacement zones by sulphides. Surface Geochemical results reached values of 357 gr/ton of Silver Gallery (Click to view full image) Location Map

Cerro Delta

Overview Cerro Delta is an Epithermal Deposit of High Au and Ag Sulphurization composed of granitic to porphyric rock instructed by dacitic dome, andesitic lavas and mafic dikes. It presents zones of Advanced Argilica alterations with central zones composed by structures with Qz-Vuggy with silica superimposition. Surface geochemical results reached values of up to 5.75 gr/Tn….

Providencia

Overview La Providencia is an epithermal deposit of silver, lead, copper and zinc lodged in conglomerate sediments of quaternary (Conglomerate La Providencia, Peralta and Sureda, 1992. Pleistocene), which overlie tectonic contact with red sediments of Pastos Grandes group (Sijes Formation) of the Upper Tertiary. The latter rely on unconformity on the Ordovician pelites and wackes…

Cerro Delta – Epithermal Deposit of High Au and Ag Sulphurization

Cerro Delta is an Epithermal Deposit of High Au and Ag Sulphurization composed of granitic to porphyric rock instructed by dacitic dome, andesitic lavas and mafic dikes. It presents zones of Advanced Argilica alterations with central zones composed by structures with Qz-Vuggy with silica superimposition. Surface geochemical results reached values of up to 5.75 gr/Tn. Geophysical…

Providencia – Final Approbal

La Providencia is an epithermal deposit of silver, lead, copper and zinc lodged in conglomerate sediments of quaternary (Conglomerate La Providencia, Peralta and Sureda, 1992. Pleistocene), which overlie tectonic contact with red sediments of Pastos Grandes group (Sijes Formation) of the Upper Tertiary. The latter rely on unconformity on the Ordovician pelites and wackes of…