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

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
Main Authors: A. Yu. Orlova, R. S. Khisamov, V. G. Bazarevskaya, E. N. Poludetkina, N. P. Fadeeva, T. A. Shardanova
Format: Article
Language:English
Published: Georesursy Ltd. 2024-04-01
Series:Georesursy
Subjects:
south tatar arch
domanic formation
rocks of mixed composition (rhythmites)
limestones
organic matter
potential
type of organic matter
catagenetic transformation
hydrocarbons
Online Access:https://www.geors.ru/jour/article/view/198
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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

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