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.
Lapukhov et al. (Thu,) studied this question.