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Sulfur Isotopic Composition of Sulfides in Skarn and Vein Mineralization of the Dal’negorsk Ore Region (Primorye)

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Abstract

The S isotopic composition in the ore-forming minerals galena and sphalerite was studied in different Ag–Pb–Zn deposits of the region. It was pointed out that the δ34S modal values range from–1.2 to +6.7‰ in the minerals with a positive value for the skarn mineralization. In the flyschoid formation, the vein-type mineralization is characterized by negative and positive values. The narrow range of δ34S values indicates the marginal-continental type of the mineralization and the multiple origins of its sources.

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Authors and Affiliations

  1. Institute of Geology and Nature Management, Far East Branch, Russian Academy of Sciences, Blagoveshchensk, Amur oblast, Russia

    L. I. Rogulina, V. G. Moiseenko, E. G. Odarichenko & E. N. Voropayeva

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  1. L. I. Rogulina
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  2. V. G. Moiseenko
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  3. E. G. Odarichenko
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  4. E. N. Voropayeva
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Correspondence to L. I. Rogulina.

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Original Russian Text © L.I. Rogulina, V.G. Moiseenko, E.G. Odarichenko, E.N. Voropayeva, 2018, published in Doklady Akademii Nauk, 2018, Vol. 479, No. 1, pp. 77–79.

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Rogulina, L.I., Moiseenko, V.G., Odarichenko, E.G. et al. Sulfur Isotopic Composition of Sulfides in Skarn and Vein Mineralization of the Dal’negorsk Ore Region (Primorye). Dokl. Earth Sc. 479, 352–354 (2018). https://doi.org/10.1134/S1028334X1803008X

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  • DOI: https://doi.org/10.1134/S1028334X1803008X

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