Analysis reveals trends in noble-metal distribution in Rudno-Altaian deposits, suggesting distinct geochemical associations.
Concentrations of Au, Ag, and all PGM’s are estimated in a variety of ore types of sulfide minerals of the Rudno-A1taian pyrite-polymetallic deposits. It has been stated that gold-silver and PGM mineralizations pertain to chalcophile and siderophile geochemical assemblages, respectively. In level of platinum potential and trends of PGM distribution, two types of deposits are recognized: near-Irtysh and Leninogorsk.
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Lapukhov et al. (1993) studied this question.
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