Abstract
Striking preponderance of the light isotopes and a very wide range of variation (δS34 from +13.5 to -21.8) are typical of the isotopic composition of sulfidic sulfur in copper ore deposits of the area, even as they are in the case of analogous ore deposits elsewhere. Fluctuations in the isotopic composition of sulfur in profiles of cupriferous rocks and parts thereof are explainable by specificities in physicochemical environments of the sediment-water-organic substance system. -- Authors.
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