Гидротермально-осадочные образования в золотоносных черносланцевых комплексах

Abstract

Underwater hydrothermal-sedimentary bodies within auriferous black schist complexes by the (Fe + Mn)/Ti module are determined. They are presented by numerous small interbeds and rare layers and lenses of the quartz and sulfide-quartz compositions enriched with Mn, Fe, Ni, Co, Cu, Au, and other elements.