Geochemical distribution and supergene behavior of indium at the Pingüino epithermal polymetallic vein system, Patagonia, Argentina

Abstract

The Pingüino deposit, located in the lowsulfidation epithermal metallogenic province of the Deseado Massif, Patagonia, Argentina, represents a distinct deposit type for this region. It evolved through two differentmineralization events: an early In-bearing polymetallic event that introduced In, Zn, Pb, Ag, Cd, Au, As, Cu, Sn,W and Bi, represented by a complex sulfide assemblage, and late Ag-Au quartz-rich veining that crosscut and overprinted the early polymetallic mineralization. Three In-bearing mineralization stages were identified within the polymetallic event. Iron-rich sphalerite of the second stage is the major In carrier in the deposit. The spatial distribution of Inwithin the veins shows itsmaximummean values in theMarta Centro and Ivonne Norte veins, in a pattern similar to the Zn distribution, showing a close spatial relation with the unexposed Kasia intrusive complex. At the vein scale, and in the hypogene zone, the In distribution is associated with variations in the temperature ofmineralizing fluids. The vertical distribution of In within the veins exhibits consistent values both below and above the oxidation level, resembling the behavior of Pb and Sn, and therefore suggesting that In behaves as an immobile element during vein weathering.