Titlebook: Ore Genesis; The State of the Art G. C. Amstutz,G. Frenzel,A. Goresy Conference proceedings 1982 Springer-Verlag Berlin Heidelberg 1982 Art

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A Strata-Bound Ni-Co Arsenide/Sulphide Mineralization in the Paleozoic of the Yauli Dome, Central Peosition of lavas, tuffs and their hydrothermal exhalative derivatives among the seafloor sediments..This is in stark contrast to other Ni-Co mineralization known from the Eastern Paleozoic Belt in Peru, attributed to either the plutonic ultrabasic or the hydrothermal granite environments.

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A Strata-Bound Ni-Co Arsenide/Sulphide Mineralization in the Paleozoic of the Yauli Dome, Central Peakly metamorphosed series of interbedded slates/phyllites, fossiliferous marbles and basic volcanics and volcaniclastics. The intimate inter-layering of these formations on both the macro- and micro-scales is taken to indicate a synsedi-mentary origin for the mineralization, related to submarine dep