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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| Format: | Article |
| Language: | English |
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Georesursy Ltd.
2024-04-01
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| Series: | Georesursy |
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| Online Access: | https://www.geors.ru/jour/article/view/198 |
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| author | A. Yu. Orlova R. S. Khisamov V. G. Bazarevskaya E. N. Poludetkina N. P. Fadeeva T. A. Shardanova |
| author_facet | A. Yu. Orlova R. S. Khisamov V. G. Bazarevskaya E. N. Poludetkina N. P. Fadeeva T. A. Shardanova |
| author_sort | A. Yu. Orlova |
| collection | DOAJ |
| description | 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. |
| format | Article |
| id | doaj-art-8c99d538c0e4423b8c33cee3e531bf8c |
| institution | Matheson Library |
| issn | 1608-5043 1608-5078 |
| language | English |
| publishDate | 2024-04-01 |
| publisher | Georesursy Ltd. |
| record_format | Article |
| series | Georesursy |
| spelling | doaj-art-8c99d538c0e4423b8c33cee3e531bf8c2025-07-21T10:35:35ZengGeoresursy Ltd.Georesursy1608-50431608-50782024-04-01232879810.18599/grs.2021.2.8197Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar archA. Yu. Orlova0R. S. Khisamov1V. G. Bazarevskaya2E. N. Poludetkina3N. P. Fadeeva4T. A. Shardanova5Lomonosov Moscow State UniversityTatneft PJSCTatneft PJSCLomonosov Moscow State UniversityLomonosov Moscow State UniversityLomonosov Moscow State UniversityThe 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.https://www.geors.ru/jour/article/view/198south tatar archdomanic formationrocks of mixed composition (rhythmites)limestonesorganic matterpotentialtype of organic mattercatagenetic transformationhydrocarbons |
| spellingShingle | A. Yu. Orlova R. S. Khisamov V. G. Bazarevskaya E. N. Poludetkina N. P. Fadeeva T. A. Shardanova Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch Georesursy south tatar arch domanic formation rocks of mixed composition (rhythmites) limestones organic matter potential type of organic matter catagenetic transformation hydrocarbons |
| title | Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch |
| title_full | Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch |
| title_fullStr | Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch |
| title_full_unstemmed | Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch |
| title_short | Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch |
| title_sort | geochemistry of organic matter in carbonate devonian sediments of the south tatar arch |
| topic | south tatar arch domanic formation rocks of mixed composition (rhythmites) limestones organic matter potential type of organic matter catagenetic transformation hydrocarbons |
| url | https://www.geors.ru/jour/article/view/198 |
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