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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Published in: | Georesursy Vol. 23; no. 2; pp. 87 - 98 |
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Main Authors: | , , , , , |
Format: | Journal Article |
Language: | English |
Published: |
Georesursy Ltd
01-04-2024
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Subjects: | |
Online Access: | Get full text |
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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. |
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ISSN: | 1608-5043 1608-5078 |
DOI: | 10.18599/grs.2021.2.8 |