Sulfide Mineralization Hosted by Spurrite-Mervinite Marbles (Kochumdek River, East Siberia)


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Abstract

Marbles of the Kochumdek complex contain pyrrhotite, rasvumite, alabandine, würtzite, galena, and acanthite. The diversity of sulfides is caused by efficient crystal chemical fractionation of trace elements under metamorphism of spurrite–merwinite facies. The isotopic–geochemical features of sulfides reveal their formation at the expense of trace elements and sulfur budget of the sedimentary parent rocks.

About the authors

E. V. Sokol

Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences

Author for correspondence.
Email: sokol@igm.nsc.ru
Russian Federation, Novosibirsk, 630090

A. S. Deviatiiarova

Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences

Email: sokol@igm.nsc.ru
Russian Federation, Novosibirsk, 630090

S. N. Kokh

Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences

Email: sokol@igm.nsc.ru
Russian Federation, Novosibirsk, 630090

V. V. Reverdatto

Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences

Email: sokol@igm.nsc.ru
Russian Federation, Novosibirsk, 630090

D. A. Artemyev

Institute of Mineralogy, Southern Ural Federal Research Center of Mineralogy and Geoecology, Ural Branch,
Russian Academy of Sciences; National Research Southern Ural State University

Email: sokol@igm.nsc.ru
Russian Federation, Miass, Chelyabinsk oblast, 456317; Chelyabinsk, 454080

V. Yu. Kolobov

Publishing House of the Siberian Branch, Russian Academy of Sciences

Email: sokol@igm.nsc.ru
Russian Federation, Novosibirsk, 630090


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