Coarse-crystalline pyrite of the Central Timan

Author:

Shaybekov R.I.1,Sokerin M.Yu.2,Kotelnikov V.G.3,Lysyuk A.Yu.2,Ignatyev G.V.2,Tropnikov E.M.2

Affiliation:

1. Institute of Geology Komi SC UB RAS, ul. Pervomayskaya 54, Syktyvkar, 167000 Russia;shaybekov@geo.komisc.ru

2. Institute of Geology Komi SC UB RAS, ul. Pervomayskaya 54, Syktyvkar, 167000 Russia

3. Syktyvkar sector of FGBU «VSEGEI», Oktyabrskiy pr. 127, Syktyvkar, 167000 Russia

Abstract

The results of mineralogical, geochemical, X-ray, isotopic and spectroscopic studies of coarse-crystalline pyrite (Kyvvozh Formation, Dimtem’el Creek, Central Timan) are presented. Pyrite is characterized by cubic habit and zonal Co distribution. It contains galena, thorite, zircon, monazite, rutile, chlorite, muscovite, quartz, albite, apatite and calcite inclusions. The unit cell parameter of pyrite vary from 5.4137 ± 0.0002 to 5.4187 ± 0.0010 A and correspond to an ideal pyrite. The sulfur isotopic composition of coarse-crystalline pyrite of 15.8‰ indicates its formation as a result of sulfate reduction during epigenesis.

Publisher

South Urals Federal Research Center for Mineralogy and Geoecology of the Urals Branch of the RAS

Reference35 articles.

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3. Ault W.U., Kulp J.L. (1959) Isotopic geochemistry of sulphur. Geochimica Et Cosmochimica Acta, 16(4), 201–235.

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5. Barker S.L.L., Hickey K.A., Cline J.S., Dipple G.M., Kilburn M.R., Vaughan J.R., Longo A.A.(2009) Uncloaking invisible gold: use of nanoSIMS to evaluate gold, trace elements, and sulphur isotopes in pyrite from Carlin-type gold deposits. Economic Geology, 104(7), 897–904.

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