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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Main Authors: A.V. Mordasova, A.B. Stoupakova, A.A. Suslova, D.K. Ershova, S.A. Sidorenko
Format: Article
Language:English
Published: Georesursy Ltd. 2019-05-01
Series:Georesursy
Subjects:
Online Access:https://geors.ru/archive/article/972/
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spelling doaj-053749f62df143d59626e5bb2cdd85042020-11-25T01:11:10ZengGeoresursy Ltd.Georesursy1608-50431608-50782019-05-01212637910.18599/grs.2019.2.63-79Conditions of formation and forecast of natural reservoirs in clinoform complex of the Lower Cretaceous of the Barents-Kara shelf A.V. Mordasova0A.B. Stoupakova1A.A. Suslova2D.K. Ershova3S.A. Sidorenko4Lomonosov Moscow State UniversityLomonosov Moscow State UniversityLomonosov Moscow State UniversityLomonosov Moscow State UniversityOil and Gas Resources of the Continental Shelf, Oil and Gas Research Institute of the Russian Academy of SciencesUnique 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 givenhttps://geors.ru/archive/article/972/Barents-Kara shelfCretaceous sedimentsseismic stratigraphic analysisclinoformcyclitedisagreementsurface floodingpaleogeographynatural reservoir
collection DOAJ
language English
format Article
sources DOAJ
author A.V. Mordasova
A.B. Stoupakova
A.A. Suslova
D.K. Ershova
S.A. Sidorenko
spellingShingle 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
Georesursy
Barents-Kara shelf
Cretaceous sediments
seismic stratigraphic analysis
clinoform
cyclite
disagreement
surface flooding
paleogeography
natural reservoir
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.
series Georesursy
issn 1608-5043
1608-5078
publishDate 2019-05-01
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
topic Barents-Kara shelf
Cretaceous sediments
seismic stratigraphic analysis
clinoform
cyclite
disagreement
surface flooding
paleogeography
natural reservoir
url https://geors.ru/archive/article/972/
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