ABSTRACT

Systematic structural analysis of lineaments, penetrative structures and vein disposition of W (Cu, Mo, Bi, Au) breccia bodies and vein type deposits in Cerro Áspero Mining District, Sierras Pampeanas de Córdoba, Argentina are presented. The analysis shows a strong structural control over the hydrothermal mineralization defined by N to NNE, NNW and WNW regional scale shear zones.