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...
Ausführliche Beschreibung
Autor*in: |
Aleksandra Yu. Orlova [verfasserIn] Rais S. Khisamov [verfasserIn] Venera G. Bazarevskaya [verfasserIn] Elena N. Poludetkina [verfasserIn] Natalia P. Fadeeva [verfasserIn] Tatiana A. Shardanova [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch ; Russisch |
Erschienen: |
2021 |
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Übergeordnetes Werk: |
In: Georesursy - Georesursy Ltd., 2017, 23(2021), 2, Seite 87-98 |
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Übergeordnetes Werk: |
volume:23 ; year:2021 ; number:2 ; pages:87-98 |
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DOI / URN: |
10.18599/grs.2021.2.8 |
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Katalog-ID: |
DOAJ064156788 |
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10.18599/grs.2021.2.8 doi (DE-627)DOAJ064156788 (DE-599)DOAJ8c99d538c0e4423b8c33cee3e531bf8c DE-627 ger DE-627 rakwb eng rus QE1-996.5 Aleksandra Yu. Orlova verfasserin aut Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 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. south tatar arch domanic formation rocks of mixed composition (rhythmites) limestones organic matter potential type of organic matter catagenetic transformation hydrocarbons Geology Rais S. Khisamov verfasserin aut Venera G. Bazarevskaya verfasserin aut Elena N. Poludetkina verfasserin aut Natalia P. Fadeeva verfasserin aut Tatiana A. Shardanova verfasserin aut In Georesursy Georesursy Ltd., 2017 23(2021), 2, Seite 87-98 (DE-627)1014868580 16085078 nnns volume:23 year:2021 number:2 pages:87-98 https://doi.org/10.18599/grs.2021.2.8 kostenfrei https://doaj.org/article/8c99d538c0e4423b8c33cee3e531bf8c kostenfrei https://geors.ru/archive/article/1090/ kostenfrei https://doaj.org/toc/1608-5078 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 23 2021 2 87-98 |
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10.18599/grs.2021.2.8 doi (DE-627)DOAJ064156788 (DE-599)DOAJ8c99d538c0e4423b8c33cee3e531bf8c DE-627 ger DE-627 rakwb eng rus QE1-996.5 Aleksandra Yu. Orlova verfasserin aut Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 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. south tatar arch domanic formation rocks of mixed composition (rhythmites) limestones organic matter potential type of organic matter catagenetic transformation hydrocarbons Geology Rais S. Khisamov verfasserin aut Venera G. Bazarevskaya verfasserin aut Elena N. Poludetkina verfasserin aut Natalia P. Fadeeva verfasserin aut Tatiana A. Shardanova verfasserin aut In Georesursy Georesursy Ltd., 2017 23(2021), 2, Seite 87-98 (DE-627)1014868580 16085078 nnns volume:23 year:2021 number:2 pages:87-98 https://doi.org/10.18599/grs.2021.2.8 kostenfrei https://doaj.org/article/8c99d538c0e4423b8c33cee3e531bf8c kostenfrei https://geors.ru/archive/article/1090/ kostenfrei https://doaj.org/toc/1608-5078 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 23 2021 2 87-98 |
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10.18599/grs.2021.2.8 doi (DE-627)DOAJ064156788 (DE-599)DOAJ8c99d538c0e4423b8c33cee3e531bf8c DE-627 ger DE-627 rakwb eng rus QE1-996.5 Aleksandra Yu. Orlova verfasserin aut Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 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. south tatar arch domanic formation rocks of mixed composition (rhythmites) limestones organic matter potential type of organic matter catagenetic transformation hydrocarbons Geology Rais S. Khisamov verfasserin aut Venera G. Bazarevskaya verfasserin aut Elena N. Poludetkina verfasserin aut Natalia P. Fadeeva verfasserin aut Tatiana A. Shardanova verfasserin aut In Georesursy Georesursy Ltd., 2017 23(2021), 2, Seite 87-98 (DE-627)1014868580 16085078 nnns volume:23 year:2021 number:2 pages:87-98 https://doi.org/10.18599/grs.2021.2.8 kostenfrei https://doaj.org/article/8c99d538c0e4423b8c33cee3e531bf8c kostenfrei https://geors.ru/archive/article/1090/ kostenfrei https://doaj.org/toc/1608-5078 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 23 2021 2 87-98 |
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Aleksandra Yu. Orlova misc QE1-996.5 misc south tatar arch misc domanic formation misc rocks of mixed composition (rhythmites) misc limestones misc organic matter misc potential misc type of organic matter misc catagenetic transformation misc hydrocarbons misc Geology Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch |
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QE1-996.5 Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch south tatar arch domanic formation rocks of mixed composition (rhythmites) limestones organic matter potential type of organic matter catagenetic transformation hydrocarbons |
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Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch |
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Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch |
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Aleksandra Yu. Orlova Rais S. Khisamov Venera G. Bazarevskaya Elena N. Poludetkina Natalia P. Fadeeva Tatiana A. Shardanova |
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Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch |
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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. |
abstractGer |
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. |
abstract_unstemmed |
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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Geochemistry of organic matter in carbonate Devonian sediments of the South Tatar arch |
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