Genesis of the Berezitovoe Gold-Polymetallic Deposit: Evidence from the Isotope Composition of Lead, Oxygen, and Sulfur

摘要

The results of the study of stable oxygen, sulfur, and lead isotopes in rocks and ores of the Berezitovoe gold-polymetallic deposit in the Upper Amur allowing us to clarify the debatable problems of its genesis are discussed in this paper. The importance of this problem is determined by the fact that the considered deposit is represented by an ore object of a fluid-explosive nature related to poorly studied and special types, which are relatively abundant in adjacent ore areas of East Transbaikalia.