Overview San Andres project is located in the Puna of Jujuy, approximately 190 km of the capital city and 15 km of La Providencia Mine (operation coming soon by Hanaq) and can be accessed through a secondary road. San Andres is a low to intermediate sulfidation deposit that contains mostly Ag-Cu-Pb. Mineralization occurs scatteredly and…
Overview Cerro Tinte is a silver, lead and zinc low-sulfidation epithermal deposit composed by calcareous and pyroclastic rocks. It presents banded structures that can get to 3 meters wide with quartz-barite and zones replaced by sulfides. The results of Surface Geochemistry amount to values of 357 gr/tn of silver. Gallery (Click to view full image)…
Overview Cerro Delta, located on the Maricunga Belt, is a high-sulfidation epithermal Au–Ag deposit composed by graniodorite to porphyritic rocks intruded by dacitic domes, andesite lavas and mafic reservoirs. It comprises Advanced Argilic alteration zones with central zones composed by vuggy quartz textures with silica superpositions. The superficial geochemical results show values of up to…
Overview La Providencia is an epythermal deposit of silver, copper, lead and zinc found in quaternary deposits (Deposits of La Providencia, Peralta and Sureda, 1992. Pleistocene), which all are superimposed by the tectonic shift of red bed-type sediments of the sediments group known as Pastos Grandes (Sijes Formation) of the Tertiary Period. Such sediments are…
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…
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…