Experience in applying a local analysis an sulfur isotopes in the ore sulfides of the largest deposits of Bodaibinsky Synclinoria (Eastern Siberia)

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Abstract

The experience of LA—ICP determining of the isotopic composition of sulfur pyrite and arsenopyrite of gold deposits of the Baikal-patomsky plateau is considered. The technique is characterized. It is shown that all the studied samples have values δ34S and δ33S strictly corresponding to the law of mass-dependent fractionation of sulfur isotopes. A regular alleviation of the isotopic composition of sulfur of pyrite as its crystals grow for Sukhoi Log and the isotopic homogeneity of pyrite and pyrrhotite of the Golets Vysokhashiy deposit are established. It is concluded that the possible role of metamorphism of the Mamsko-Oronsky belt in the formation of isotopic homogeneity of ore sulfides.

About the authors

N. A. Goryachev

Institute of Geology and Natural Management of Far Eastern Branch of Russian Academy of Sciences; Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences

Author for correspondence.
Email: goryachev@neisri.ru

Corresponding Member of the RAS

Russian Federation, 1, Relochniy lane, Blagoveshchensk, 675000; PBox 9, 1a, Favorsky street, Irkutsk, 664033

A. V. Ignatiev

Far East Geological Institute, Far East Branch, Russian Academy of Sciences

Email: goryachev@neisri.ru
Russian Federation, 159, 100-letya avenue, Vladivostok, 690022

T. A. Velivetskaya

Far East Geological Institute, Far East Branch, Russian Academy of Sciences

Email: goryachev@neisri.ru
Russian Federation, 159, 100-letya avenue, Vladivostok, 690022

A. E. Budyak

Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences

Email: goryachev@neisri.ru
Russian Federation, PBox 9, 1a, Favorsky street, Irkutsk, 664033

Yu. I. Tarasova

Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences

Email: goryachev@neisri.ru
Russian Federation, PBox 9, 1a, Favorsky street, Irkutsk, 664033

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