西伯利亚地台寒武系含油气矿床有机质碳同位素组成及碳酸盐碳氧组成特征

Q4 Earth and Planetary Sciences
S. I. Golyshev, P. N. Sobolev, N. L. Padalko, S. I. Dykhan, P. F. Yavorov, M. I. Prazdnichnykh, E. V. Chernikov
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引用次数: 0

摘要

本文介绍了西伯利亚地台中下寒武统Shumnaya组、Inikan组和Kuonamka组碳酸盐岩组分(CRC)的碳(δ13С)和氧(δ18О)同位素组成和分散有机质(SOM)的碳(δ13C)数据。揭示了结直肠癌碳氧同位素组成与寒武系domanicoid矿床相类型的关系。考虑了下、中寒武统沉积物中DOM碳同位素组成与沉积条件的相互关系。在西伯利亚地台东南部,发现了下寒武统碳酸盐岩矿床,其碳异常同位素组成为CRC (δ13Сср = 6,6‰)和DOM (δ13С = - 36,5‰)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
FEATURES OF THE CARBON ISOTOPE COMPOSITION OF ORGANIC MATTER AND CARBON AND OXYGEN CARBONATE CONSTITUENT OF OIL AND GAS PRODUCING DEPOSITS OF THE CAMBRIAN OF THE SIBERIAN PLATFORM
The paper presents data on the carbon (δ13С) and oxygen (δ18О) isotopic composition of the carbonate rock constituent (CRC) and carbon (δ13C) of dispersed organic matter (SOM) of rocks of the Shumnaya, Inikan and Kuonamka Formations of the Lower-Middle Cambrian of the Siberian Platform. Dependence of the carbon and oxygen isotopic composition of CRC on the facies subtype of domanicoid deposits of the Cambrian was revealed. The interrelation of the carbon isotope composition of DOM with depositional conditions of sediments of the Lower and Middle Cambrian was considered. In the south-east of the Siberian Platform, Lower Cambrian carbonate deposits with carbon anomalous isotopic composition of CRC (δ13Сср = 6,6 ‰) and carbon of DOM (δ13С = –36,5 ‰) were found.
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来源期刊
Geology and Mineral Resources of Siberia
Geology and Mineral Resources of Siberia Earth and Planetary Sciences-Geology
CiteScore
0.30
自引率
0.00%
发文量
23
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