A new interpretation for the origin of the Norilsk type PGE-Cu-Ni sulfide depositsстатья
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Аннотация:Origin of sulfide PGE-CU-Ni deposits of in Norilsk and Talnakh associated with Triassic basalt traps of Siberia are considered. It is shown that ore elements of these deposits (probably, except Fe) are derived from mantle rather than crust. They entered the basalts owing to the remobilization (recycling) of ore elements from Early Proterozoic sediments and rocks in the Siberian Platform basement. Criteria of prospecting for analogous deposits are presente