Carbonatos en vetas en el distrito epitermal de baja sulfuracion de El Peñon, II Region, Chile: ambiente de formacion e implicancias para la exploracion.
Abstract:Carbonate minerals are common gangue minerals in the low sulfidation epithermal Au-Ag District of El Peñón, II Región, Chile. They can be subdivided into two principal groups on the basis of the paragenetic relationships. Paragenetically early carbonates occur together with quartz and sulfide minerals in banded veins and are closely associated with precious metal mineralization. These carbonates are compositionally complex, consisting of calcite, finely intermixed with ankerite, kutnohorite, rhodochrosite and … Show more
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