Abstract

Data on the sulfur isotopic composition of sulfides from gold-silver deposits of volcanoplutonic belts were systematized. The deposits differ in the variation range, character of distribution, and modal values of δ34S. It was shown that the sulfur isotopic composition is an integral parameter related to a combination of geologic factors. Based on the analysis of the compiled database, it was concluded that the sulfur isotopic composition of deposits evolves in time in an oscillatory manner, similar to the periodic variations in the isotopic composition of sulfide and sulfate sulfur in the Earth’s sedimentary shell.

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