Conditions of formation and forecast of natural reservoirs in clinoform complex of the Lower Cretaceous of the Barents-Kara shelf

Unique Leningradsky and Rusanovsky gascondensate fields in the Barrem-Cenomanian layer are discovered in the Kara Sea. Non-industrial accumulations of oil and gas have been discovered in the Lower Cretaceous sediments of the western part of the Barents Sea shelf. However, the structure and oil and g...

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Published in:Georesursy
Main Authors: A.V. Mordasova, A.B. Stoupakova, A.A. Suslova, D.K. Ershova, S.A. Sidorenko
Format: Article in Journal/Newspaper
Language:English
Russian
Published: Georesursy Ltd. 2019
Subjects:
Online Access:https://doi.org/10.18599/grs.2019.2.63-79
https://doaj.org/article/053749f62df143d59626e5bb2cdd8504
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spelling ftdoajarticles:oai:doaj.org/article:053749f62df143d59626e5bb2cdd8504 2023-05-15T15:38:54+02:00 Conditions of formation and forecast of natural reservoirs in clinoform complex of the Lower Cretaceous of the Barents-Kara shelf A.V. Mordasova A.B. Stoupakova A.A. Suslova D.K. Ershova S.A. Sidorenko 2019-05-01T00:00:00Z https://doi.org/10.18599/grs.2019.2.63-79 https://doaj.org/article/053749f62df143d59626e5bb2cdd8504 EN RU eng rus Georesursy Ltd. https://geors.ru/archive/article/972/ https://doaj.org/toc/1608-5043 https://doaj.org/toc/1608-5078 doi:10.18599/grs.2019.2.63-79 1608-5043 1608-5078 https://doaj.org/article/053749f62df143d59626e5bb2cdd8504 Georesursy, Vol 21, Iss 2, Pp 63-79 (2019) Barents-Kara shelf Cretaceous sediments seismic stratigraphic analysis clinoform cyclite disagreement surface flooding paleogeography natural reservoir Geology QE1-996.5 article 2019 ftdoajarticles https://doi.org/10.18599/grs.2019.2.63-79 2022-12-31T08:47:35Z Unique Leningradsky and Rusanovsky gascondensate fields in the Barrem-Cenomanian layer are discovered in the Kara Sea. Non-industrial accumulations of oil and gas have been discovered in the Lower Cretaceous sediments of the western part of the Barents Sea shelf. However, the structure and oil and gas potential of the Lower Cretaceous sediments of the Barents-Kara shelf remain unexplored. Based on the seismic-stratigraphic and cyclostratigraphic analysis, a regional geological model of the Lower Cretaceous deposits of the Barents-Kara shelf was created, the distribution area and the main stages of the accumulation of clinoforms were identified. As a result of a detailed analysis of the morphology of clinoform bodies, paleogeographic conditions were restored in the Early Cretaceous and a forecast of the distribution of sandy reservoirs was given Article in Journal/Newspaper Barents Sea Kara Sea Directory of Open Access Journals: DOAJ Articles Barents Sea Kara Sea Georesursy 21 2 63 79
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
Russian
topic Barents-Kara shelf
Cretaceous sediments
seismic stratigraphic analysis
clinoform
cyclite
disagreement
surface flooding
paleogeography
natural reservoir
Geology
QE1-996.5
spellingShingle Barents-Kara shelf
Cretaceous sediments
seismic stratigraphic analysis
clinoform
cyclite
disagreement
surface flooding
paleogeography
natural reservoir
Geology
QE1-996.5
A.V. Mordasova
A.B. Stoupakova
A.A. Suslova
D.K. Ershova
S.A. Sidorenko
Conditions of formation and forecast of natural reservoirs in clinoform complex of the Lower Cretaceous of the Barents-Kara shelf
topic_facet Barents-Kara shelf
Cretaceous sediments
seismic stratigraphic analysis
clinoform
cyclite
disagreement
surface flooding
paleogeography
natural reservoir
Geology
QE1-996.5
description Unique Leningradsky and Rusanovsky gascondensate fields in the Barrem-Cenomanian layer are discovered in the Kara Sea. Non-industrial accumulations of oil and gas have been discovered in the Lower Cretaceous sediments of the western part of the Barents Sea shelf. However, the structure and oil and gas potential of the Lower Cretaceous sediments of the Barents-Kara shelf remain unexplored. Based on the seismic-stratigraphic and cyclostratigraphic analysis, a regional geological model of the Lower Cretaceous deposits of the Barents-Kara shelf was created, the distribution area and the main stages of the accumulation of clinoforms were identified. As a result of a detailed analysis of the morphology of clinoform bodies, paleogeographic conditions were restored in the Early Cretaceous and a forecast of the distribution of sandy reservoirs was given
format Article in Journal/Newspaper
author A.V. Mordasova
A.B. Stoupakova
A.A. Suslova
D.K. Ershova
S.A. Sidorenko
author_facet A.V. Mordasova
A.B. Stoupakova
A.A. Suslova
D.K. Ershova
S.A. Sidorenko
author_sort A.V. Mordasova
title Conditions of formation and forecast of natural reservoirs in clinoform complex of the Lower Cretaceous of the Barents-Kara shelf
title_short Conditions of formation and forecast of natural reservoirs in clinoform complex of the Lower Cretaceous of the Barents-Kara shelf
title_full Conditions of formation and forecast of natural reservoirs in clinoform complex of the Lower Cretaceous of the Barents-Kara shelf
title_fullStr Conditions of formation and forecast of natural reservoirs in clinoform complex of the Lower Cretaceous of the Barents-Kara shelf
title_full_unstemmed Conditions of formation and forecast of natural reservoirs in clinoform complex of the Lower Cretaceous of the Barents-Kara shelf
title_sort conditions of formation and forecast of natural reservoirs in clinoform complex of the lower cretaceous of the barents-kara shelf
publisher Georesursy Ltd.
publishDate 2019
url https://doi.org/10.18599/grs.2019.2.63-79
https://doaj.org/article/053749f62df143d59626e5bb2cdd8504
geographic Barents Sea
Kara Sea
geographic_facet Barents Sea
Kara Sea
genre Barents Sea
Kara Sea
genre_facet Barents Sea
Kara Sea
op_source Georesursy, Vol 21, Iss 2, Pp 63-79 (2019)
op_relation https://geors.ru/archive/article/972/
https://doaj.org/toc/1608-5043
https://doaj.org/toc/1608-5078
doi:10.18599/grs.2019.2.63-79
1608-5043
1608-5078
https://doaj.org/article/053749f62df143d59626e5bb2cdd8504
op_doi https://doi.org/10.18599/grs.2019.2.63-79
container_title Georesursy
container_volume 21
container_issue 2
container_start_page 63
op_container_end_page 79
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