Features of Composition and Cement Type of the Lower Triassic Reservoirs in the North of the Timan-Pechora Oil and Gas Province

The work is devoted to the study of cement type and composition of the Lower Triassic deposits of the Timan-Pechora province, their influence on reservoir properties of rocks. The work was based on laboratory studies of core, generalization of published data. Morphological and genetic analysis of cl...

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Published in:Georesursy
Main Author: N.N. Timonina
Format: Article in Journal/Newspaper
Language:English
Russian
Published: Georesursy Ltd. 2017
Subjects:
Online Access:https://doi.org/10.18599/grs.19.1.7
https://doaj.org/article/23649c536ba443fa8d3c54a4ab6e67d8
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spelling ftdoajarticles:oai:doaj.org/article:23649c536ba443fa8d3c54a4ab6e67d8 2023-05-15T17:54:58+02:00 Features of Composition and Cement Type of the Lower Triassic Reservoirs in the North of the Timan-Pechora Oil and Gas Province N.N. Timonina 2017-03-01T00:00:00Z https://doi.org/10.18599/grs.19.1.7 https://doaj.org/article/23649c536ba443fa8d3c54a4ab6e67d8 EN RU eng rus Georesursy Ltd. https://geors.ru/archive/article/825/ https://doaj.org/toc/1608-5043 https://doaj.org/toc/1608-5078 doi:10.18599/grs.19.1.7 1608-5043 1608-5078 https://doaj.org/article/23649c536ba443fa8d3c54a4ab6e67d8 Georesursy, Vol 19, Iss 1, Pp 38-44 (2017) Oil and gas province type of reservoirs void clay minerals regeneration Geology QE1-996.5 article 2017 ftdoajarticles https://doi.org/10.18599/grs.19.1.7 2022-12-30T21:39:35Z The work is devoted to the study of cement type and composition of the Lower Triassic deposits of the Timan-Pechora province, their influence on reservoir properties of rocks. The work was based on laboratory studies of core, generalization of published data. Morphological and genetic analysis of clay minerals was carried out using X-ray and electron-microscopic methods. As a result of the conducted studies it was established that the type, composition and distribution of the cement is influenced by the composition of demolition sources, sedimentation conditions, and post-sedimentation transformations. Kaolinite, chlorite, smectite and hydromica associations are distinguished according to the predominance of clay mineral in the sandstone cement. Kaolinite cement of sandstones is most typical for continental fluvial facies, especially channel beds. Smectite association is most characteristic of the floodplain, oxbow and lake facies of the zone. The revealed regularities will contribute to the improvement of accurate reconstruction of sedimentation conditions, construction of more adequate geological models of the reservoir, taking into account its reservoir heterogeneity both at the level of the reservoir and its constituent interlayers. Article in Journal/Newspaper Pechora Directory of Open Access Journals: DOAJ Articles Georesursy 19 1 38 44
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
Russian
topic Oil and gas province
type of reservoirs
void
clay minerals
regeneration
Geology
QE1-996.5
spellingShingle Oil and gas province
type of reservoirs
void
clay minerals
regeneration
Geology
QE1-996.5
N.N. Timonina
Features of Composition and Cement Type of the Lower Triassic Reservoirs in the North of the Timan-Pechora Oil and Gas Province
topic_facet Oil and gas province
type of reservoirs
void
clay minerals
regeneration
Geology
QE1-996.5
description The work is devoted to the study of cement type and composition of the Lower Triassic deposits of the Timan-Pechora province, their influence on reservoir properties of rocks. The work was based on laboratory studies of core, generalization of published data. Morphological and genetic analysis of clay minerals was carried out using X-ray and electron-microscopic methods. As a result of the conducted studies it was established that the type, composition and distribution of the cement is influenced by the composition of demolition sources, sedimentation conditions, and post-sedimentation transformations. Kaolinite, chlorite, smectite and hydromica associations are distinguished according to the predominance of clay mineral in the sandstone cement. Kaolinite cement of sandstones is most typical for continental fluvial facies, especially channel beds. Smectite association is most characteristic of the floodplain, oxbow and lake facies of the zone. The revealed regularities will contribute to the improvement of accurate reconstruction of sedimentation conditions, construction of more adequate geological models of the reservoir, taking into account its reservoir heterogeneity both at the level of the reservoir and its constituent interlayers.
format Article in Journal/Newspaper
author N.N. Timonina
author_facet N.N. Timonina
author_sort N.N. Timonina
title Features of Composition and Cement Type of the Lower Triassic Reservoirs in the North of the Timan-Pechora Oil and Gas Province
title_short Features of Composition and Cement Type of the Lower Triassic Reservoirs in the North of the Timan-Pechora Oil and Gas Province
title_full Features of Composition and Cement Type of the Lower Triassic Reservoirs in the North of the Timan-Pechora Oil and Gas Province
title_fullStr Features of Composition and Cement Type of the Lower Triassic Reservoirs in the North of the Timan-Pechora Oil and Gas Province
title_full_unstemmed Features of Composition and Cement Type of the Lower Triassic Reservoirs in the North of the Timan-Pechora Oil and Gas Province
title_sort features of composition and cement type of the lower triassic reservoirs in the north of the timan-pechora oil and gas province
publisher Georesursy Ltd.
publishDate 2017
url https://doi.org/10.18599/grs.19.1.7
https://doaj.org/article/23649c536ba443fa8d3c54a4ab6e67d8
genre Pechora
genre_facet Pechora
op_source Georesursy, Vol 19, Iss 1, Pp 38-44 (2017)
op_relation https://geors.ru/archive/article/825/
https://doaj.org/toc/1608-5043
https://doaj.org/toc/1608-5078
doi:10.18599/grs.19.1.7
1608-5043
1608-5078
https://doaj.org/article/23649c536ba443fa8d3c54a4ab6e67d8
op_doi https://doi.org/10.18599/grs.19.1.7
container_title Georesursy
container_volume 19
container_issue 1
container_start_page 38
op_container_end_page 44
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