The first data on mass-independent fractionation of sulfur isotopes in sulfides from rocks of the eastern part of the Fennoscandian Shield


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Abstract

The first data on the multi-isotope composition of sulfur (32S, 33S, 34S) in samples from the Fennoscandian Shield were obtained by the laser local method. An anomalous concentration of the stable isotope 33S was registered in some samples. Δ33S ranges from–0.45 to +0.24‰, which indicates the mass-independent fractionation of S isotopes and provides evidence for the processes of primarily sedimentary accumulation of sulfides in the Archean oxygen-free atmosphere.

About the authors

A. V. Ignat’ev

Far East Geological Institute, Far East Branch

Author for correspondence.
Email: ignatiev@fegi.ru
Russian Federation, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022

A. I. Khanchuk

Far East Geological Institute, Far East Branch; Far East Federal University

Email: ignatiev@fegi.ru
Russian Federation, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022; Vladivostok

S. V. Vysotskii

Far East Geological Institute, Far East Branch; Far East Federal University

Email: ignatiev@fegi.ru
Russian Federation, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022; Vladivostok

T. A. Velivetskaya

Far East Geological Institute, Far East Branch

Email: ignatiev@fegi.ru
Russian Federation, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022

V. I. Levitskii

Vinogradov Institute of Geochemistry, Siberian Branch

Email: ignatiev@fegi.ru
Russian Federation, ul. Favorskogo 1a, Irkutsk, 664033

E. N. Terekhov

Geological Institute

Email: ignatiev@fegi.ru
Russian Federation, Pyzhevsky per. 7, Moscow, 119017


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