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


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Resumo

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.

Sobre autores

E. Sokol

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

Autor responsável pela correspondência
Email: sokol@igm.nsc.ru
Rússia, Novosibirsk, 630090

A. Deviatiiarova

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

Email: sokol@igm.nsc.ru
Rússia, Novosibirsk, 630090

S. Kokh

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

Email: sokol@igm.nsc.ru
Rússia, Novosibirsk, 630090

V. Reverdatto

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

Email: sokol@igm.nsc.ru
Rússia, Novosibirsk, 630090

D. 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
Rússia, Miass, Chelyabinsk oblast, 456317; Chelyabinsk, 454080

V. Kolobov

Publishing House of the Siberian Branch, Russian Academy of Sciences

Email: sokol@igm.nsc.ru
Rússia, Novosibirsk, 630090


Declaração de direitos autorais © Pleiades Publishing, Ltd., 2019

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