Platinum potential of mafic–ultramafic massifs in the western part of the Dambuka ore district (Upper Amur Region, Russia)

Resumo

New data on the Pt potential of mafic–ultramafic massifs of the Khani–Maya, Uldegit, and Dzhalta complexes in the western part of the Dambuka ore district are discussed. The Khani–Maya Complex is represented by metamorphosed gabbro, gabbronorites, gabbro anorthosites, subordinate pyroxenites, hornblendites, and peridotites. The Uldegit Complex is composed of pyroxenites, hornblendites, gabbro, gabbronorites, norites, troctolites, peridotites, dunites, actinolite–tremolites, serpentinites, anthophyllites, and tremolite–plagioclase rocks. The Dzhalta Complex is formed of peridotites, gabbro, eclogitized gabbro, hornblendites, cortlandites, and pyroxenites. All these complexes differ from each other by the concentrations of Ni, Cu, Co, Au, and platinoids depending on the composition of the constituting rocks and the presence of sulfide minerals.