Specific features of carbon and oxygen stable isotopes (δ13C and δ18O) geochemistry in the isolated carbonate platform section on the east of the Urals (the Famennian and Tournaisian Stages)

G. A. Mizens
V. N. Kuleshov
S. A. Sapurin
T. I. Stepanova
O. L. Petrov

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Publication date

January 2016

Publisher

A.N. Zavaritsky Institute of Geology and Geochemistry

Journal

LITHOSPHERE (Russia)

Abstract

New data about the stable carbon and oxygen isotopic composition for the Frasnian/Famennian and Devonian/Carboniferous boundary intervals, as well as for middle and upper parts of the Tournasian Stage (the Lower Carboniferous), are represented in this article. Isotopic composition, specific features and depositional conditions which were revealed in the isolated carbonate platform basin are considered

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Specific features of carbon and oxygen stable isotopes (δ13C and δ18O) geochemistry in the isolated carbonate platform section on the east of the Urals (the Famennian and Tournaisian Stages)

Abstract

Extracted data

Specific features of carbon and oxygen stable isotopes (δ13C and δ18O) geochemistry in the isolated carbonate platform section on the east of the Urals (the Famennian and Tournaisian Stages)

Abstract

Extracted data

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