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

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 p...

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Bibliographic Details
Published in:Georesursy Vol. 23; no. 2; pp. 87 - 98
Main Authors: Orlova, Aleksandra Yu, Khisamov, Rais S., Bazarevskaya, Venera G., Poludetkina, Elena N., Fadeeva, Natalia P., Shardanova, Tatiana A.
Format: Journal Article
Language:English
Published: Georesursy Ltd 01-04-2024
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Summary: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.
ISSN:1608-5043
1608-5078
DOI:10.18599/grs.2021.2.8