1. Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch
- Author
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Natalia P. Fadeeva, Venera Bazarevskaya, T. A. Shardanova, Aleksandra Yu. Orlova, E. N. Poludetkina, and Rais Khisamov
- Subjects
Tatar ,potential ,catagenetic transformation ,020209 energy ,Geochemistry ,02 engineering and technology ,010502 geochemistry & geophysics ,01 natural sciences ,Devonian ,chemistry.chemical_compound ,0202 electrical engineering, electronic engineering, information engineering ,Organic matter ,hydrocarbons ,Arch ,limestones ,organic matter ,0105 earth and related environmental sciences ,chemistry.chemical_classification ,QE1-996.5 ,Geology ,south tatar arch ,language.human_language ,Geophysics ,domanic formation ,chemistry ,language ,Carbonate ,rocks of mixed composition (rhythmites) ,type of organic matter - Abstract
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.
- Published
- 2021
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