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
Affiliations
G. A. Mizens
Institute of Geology and Geochemistry, Urals Branch of RAS
V. N. Kuleshov
Geological Institute of RAS
S. A. Sapurin
Institute of Geology and Geochemistry, Urals Branch of RAS
T. I. Stepanova
Institute of Geology and Geochemistry, Urals Branch of RAS
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.
