Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch

被引：1

作者：

Orlova, A. Yu ^{[1
]}

Khisamov, R. S. ^{[2
]}

Bazarevskaya, V. G. ^{[3
]}

Poludetkina, E. N. ^{[1
]}

Fadeeva, N. P. ^{[1
]}

Shardanova, T. A. ^{[1
]}

机构：

[1] Lomonosov Moscow State Univ, Petr Geol Dept, 1 Leninskie Gory, Moscow 119234, Russia

[2] Tatneft PJSC, Inst TatNIPIneft, Almetyevsk, Russia

[3] Tatneft PJSC, Inst TatNIPIneft, Sci Field Geol Hard Recover Reserves, Almetyevsk, Russia

来源：

GEORESURSY | 2021年 / 23卷 / 02期

关键词：

South Tatar arch; domanic formation; rocks of mixed composition (rhythmites); limestones; organic matter; potential; type of organic matter; catagenetic transformation; hydrocarbons;

D O I：

10.18599/grs.2021.2.8

中图分类号：

TE [石油、天然气工业];

学科分类号：

0820 ;

摘要：

The article deals with the lithology and geochemistry of organic matter of Upper Devonian-Lower Carboniferous deposits (Carbonate Devonian) of the eastern part of the South Tatar arch. Rocks of this age have a high generative potential due to increased concentrations of organic matter (OM) and its phytogenic and zoophytogenic composition. They refer to non-traditional sources of hydrocarbons. The generative potential depends on the facial environment and the transformation of OM. The highest potential have carbonate-siliceous and siliceous-carbonate rhythmites domannic horizon.

引用

页码：87 / 98

页数：12

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