Lithological and biostratigraphic characteristics of the Upper Silurian and Lower Devonian deposits of the southwestern part of the field named after Roman Trebs
A conodont sequence from the Przhidolian stage of the Upper Silurian and almost the entire Lokhkovian stage of the Lower Devonian has been established in the sections of the Upper Silurian-Lower Devonian on the southwestern part of the field named after Roman Trebs (Timano-Pechora oil and gas provin...
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ftdoajarticles:oai:doaj.org/article:328803fc0c1a4257b41b25b1a9df2345 2023-05-15T17:55:00+02:00 Lithological and biostratigraphic characteristics of the Upper Silurian and Lower Devonian deposits of the southwestern part of the field named after Roman Trebs Т.М. Mavrinskaya E.N. Savelyeva K.D. Shumatbaev 2018-06-01T00:00:00Z https://doi.org/10.18599/grs.2018.2.81-87 https://doaj.org/article/328803fc0c1a4257b41b25b1a9df2345 EN RU eng rus Georesursy Ltd. https://geors.ru/archive/article/913/ https://doaj.org/toc/1608-5043 https://doaj.org/toc/1608-5078 doi:10.18599/grs.2018.2.81-87 1608-5043 1608-5078 https://doaj.org/article/328803fc0c1a4257b41b25b1a9df2345 Georesursy, Vol 20, Iss 2, Pp 81-87 (2018) Silurian Devonian conodonts logging lithology cyclicity Geology QE1-996.5 article 2018 ftdoajarticles https://doi.org/10.18599/grs.2018.2.81-87 2022-12-30T21:46:12Z A conodont sequence from the Przhidolian stage of the Upper Silurian and almost the entire Lokhkovian stage of the Lower Devonian has been established in the sections of the Upper Silurian-Lower Devonian on the southwestern part of the field named after Roman Trebs (Timano-Pechora oil and gas province). According to the conodonts, two biostratigraphic subdivisions are distinguished in the rank of layers with fauna in the Upper Silurian and three of them in the Lokhkovian stage of the Lower Devonian. The layers can be compared with the standard conodont zonal scale. The Silurian-Devonian boundary has a complex rationale for biostratigraphic data (conodonts), cyclostratigraphy, and logging data (electrical and radioactive methods). The Lower Devonian deposits are overlain by terrigenous packs of the Timanian horizon of the Frasnian stage. The break in the sedimentation covers the interval from the Praghian stage of the Lower Devonian to the Dzhierskian horizon of the Frasnian stage of the Upper Devonian inclusively. The regularity of the placement of reservoir rocks in the section of wells is analyzed and their relation to the cyclicity of sedimentation is noted. Article in Journal/Newspaper Pechora Directory of Open Access Journals: DOAJ Articles Georesursy 20 2 81 87 |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
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language |
English Russian |
topic |
Silurian Devonian conodonts logging lithology cyclicity Geology QE1-996.5 |
spellingShingle |
Silurian Devonian conodonts logging lithology cyclicity Geology QE1-996.5 Т.М. Mavrinskaya E.N. Savelyeva K.D. Shumatbaev Lithological and biostratigraphic characteristics of the Upper Silurian and Lower Devonian deposits of the southwestern part of the field named after Roman Trebs |
topic_facet |
Silurian Devonian conodonts logging lithology cyclicity Geology QE1-996.5 |
description |
A conodont sequence from the Przhidolian stage of the Upper Silurian and almost the entire Lokhkovian stage of the Lower Devonian has been established in the sections of the Upper Silurian-Lower Devonian on the southwestern part of the field named after Roman Trebs (Timano-Pechora oil and gas province). According to the conodonts, two biostratigraphic subdivisions are distinguished in the rank of layers with fauna in the Upper Silurian and three of them in the Lokhkovian stage of the Lower Devonian. The layers can be compared with the standard conodont zonal scale. The Silurian-Devonian boundary has a complex rationale for biostratigraphic data (conodonts), cyclostratigraphy, and logging data (electrical and radioactive methods). The Lower Devonian deposits are overlain by terrigenous packs of the Timanian horizon of the Frasnian stage. The break in the sedimentation covers the interval from the Praghian stage of the Lower Devonian to the Dzhierskian horizon of the Frasnian stage of the Upper Devonian inclusively. The regularity of the placement of reservoir rocks in the section of wells is analyzed and their relation to the cyclicity of sedimentation is noted. |
format |
Article in Journal/Newspaper |
author |
Т.М. Mavrinskaya E.N. Savelyeva K.D. Shumatbaev |
author_facet |
Т.М. Mavrinskaya E.N. Savelyeva K.D. Shumatbaev |
author_sort |
Т.М. Mavrinskaya |
title |
Lithological and biostratigraphic characteristics of the Upper Silurian and Lower Devonian deposits of the southwestern part of the field named after Roman Trebs |
title_short |
Lithological and biostratigraphic characteristics of the Upper Silurian and Lower Devonian deposits of the southwestern part of the field named after Roman Trebs |
title_full |
Lithological and biostratigraphic characteristics of the Upper Silurian and Lower Devonian deposits of the southwestern part of the field named after Roman Trebs |
title_fullStr |
Lithological and biostratigraphic characteristics of the Upper Silurian and Lower Devonian deposits of the southwestern part of the field named after Roman Trebs |
title_full_unstemmed |
Lithological and biostratigraphic characteristics of the Upper Silurian and Lower Devonian deposits of the southwestern part of the field named after Roman Trebs |
title_sort |
lithological and biostratigraphic characteristics of the upper silurian and lower devonian deposits of the southwestern part of the field named after roman trebs |
publisher |
Georesursy Ltd. |
publishDate |
2018 |
url |
https://doi.org/10.18599/grs.2018.2.81-87 https://doaj.org/article/328803fc0c1a4257b41b25b1a9df2345 |
genre |
Pechora |
genre_facet |
Pechora |
op_source |
Georesursy, Vol 20, Iss 2, Pp 81-87 (2018) |
op_relation |
https://geors.ru/archive/article/913/ https://doaj.org/toc/1608-5043 https://doaj.org/toc/1608-5078 doi:10.18599/grs.2018.2.81-87 1608-5043 1608-5078 https://doaj.org/article/328803fc0c1a4257b41b25b1a9df2345 |
op_doi |
https://doi.org/10.18599/grs.2018.2.81-87 |
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87 |
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