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)

Литосфера

O. L. Petrov¹  V. N. Kuleshov¹  T. I. Stepanova²  S. A. Sapurin²  G. A. Mizens² 

[1] Geological Institute of RAS;Institute of Geology and Geochemistry, Urals Branch of RAS;

关键词: изотопы углерода и кислорода;    фаменский ярус;    турнейский ярус;    граница франа и фамена;    граница девона и карбона;    глобальные геологические события;    карбонатная платформа;    stable carbon and oxygen isotopes;    the famennian stage;    the tournaisian stage;    the frasnian/famennian boundary;    the devonian/carboniferous boundary;    global geological events;    carbonate platform;   

DOI  :  

来源: DOAJ

【 摘 要 】

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.

【 授权许可】

Unknown