Email this article Sulfur Isotopic Composition of Sulfides in Skarn and Vein Mineralization of the Dal’negorsk Ore Region (Primorye)
- Authors: Rogulina L.I.1, Moiseenko V.G.1, Odarichenko E.G.1, Voropayeva E.N.1
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Affiliations:
- Institute of Geology and Nature Management, Far East Branch
- Issue: Vol 479, No 1 (2018)
- Pages: 352-354
- Section: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/192493
- DOI: https://doi.org/10.1134/S1028334X1803008X
- ID: 192493
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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.
About the authors
L. I. Rogulina
Institute of Geology and Nature Management, Far East Branch
Author for correspondence.
Email: rogulina@mail.ru
Russian Federation, Blagoveshchensk, Amur oblast
V. G. Moiseenko
Institute of Geology and Nature Management, Far East Branch
Email: rogulina@mail.ru
Russian Federation, Blagoveshchensk, Amur oblast
E. G. Odarichenko
Institute of Geology and Nature Management, Far East Branch
Email: rogulina@mail.ru
Russian Federation, Blagoveshchensk, Amur oblast
E. N. Voropayeva
Institute of Geology and Nature Management, Far East Branch
Email: rogulina@mail.ru
Russian Federation, Blagoveshchensk, Amur oblast
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