Lithogenetic Features of Rocks Containing Productive Oil Deposits in the Lower Carboniferous Terrigenous Strata

Conducted comprehensive studies on lithogenetic characteristics of clastic sedimentary petroleum reservoirs and enclosing rocks, which allowed assessing the stability of rock when drilling exploration and production wells (mineral composition, structural-textural features, lithogenetic change, etc.)...

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Main Authors: K. P. Kazimov, N. E. Moloshtanova
Format: Article
Language:English
Published: Perm Sate National Research University 2019-12-01
Series:Vestnik Permskogo Universiteta: Seriâ Geologiâ
Subjects:
Online Access:http://geology-vestnik.psu.ru/index.php/geology/article/view/324
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spelling doaj-389d0f38674244c29709707e0b1b092e2020-11-25T01:07:48ZengPerm Sate National Research UniversityVestnik Permskogo Universiteta: Seriâ Geologiâ1994-36012313-47982019-12-0118435636110.17072/psu.geol.18.4.356269Lithogenetic Features of Rocks Containing Productive Oil Deposits in the Lower Carboniferous Terrigenous StrataK. P. Kazimov0N. E. Moloshtanova1Пермский государственный национальный исследовательский университет 614990, Пермь, ул. Букирева, 15Пермский государственный национальный исследовательский университет 614990, Пермь, ул. Букирева, 15Conducted comprehensive studies on lithogenetic characteristics of clastic sedimentary petroleum reservoirs and enclosing rocks, which allowed assessing the stability of rock when drilling exploration and production wells (mineral composition, structural-textural features, lithogenetic change, etc.). The findings about membership of the studied rocks to the products of early and late mezocatagenesis are presented.http://geology-vestnik.psu.ru/index.php/geology/article/view/324литогенетические особенности горных породминеральный составструктура и текстура горных породмезокатагенез
collection DOAJ
language English
format Article
sources DOAJ
author K. P. Kazimov
N. E. Moloshtanova
spellingShingle K. P. Kazimov
N. E. Moloshtanova
Lithogenetic Features of Rocks Containing Productive Oil Deposits in the Lower Carboniferous Terrigenous Strata
Vestnik Permskogo Universiteta: Seriâ Geologiâ
литогенетические особенности горных пород
минеральный состав
структура и текстура горных пород
мезокатагенез
author_facet K. P. Kazimov
N. E. Moloshtanova
author_sort K. P. Kazimov
title Lithogenetic Features of Rocks Containing Productive Oil Deposits in the Lower Carboniferous Terrigenous Strata
title_short Lithogenetic Features of Rocks Containing Productive Oil Deposits in the Lower Carboniferous Terrigenous Strata
title_full Lithogenetic Features of Rocks Containing Productive Oil Deposits in the Lower Carboniferous Terrigenous Strata
title_fullStr Lithogenetic Features of Rocks Containing Productive Oil Deposits in the Lower Carboniferous Terrigenous Strata
title_full_unstemmed Lithogenetic Features of Rocks Containing Productive Oil Deposits in the Lower Carboniferous Terrigenous Strata
title_sort lithogenetic features of rocks containing productive oil deposits in the lower carboniferous terrigenous strata
publisher Perm Sate National Research University
series Vestnik Permskogo Universiteta: Seriâ Geologiâ
issn 1994-3601
2313-4798
publishDate 2019-12-01
description Conducted comprehensive studies on lithogenetic characteristics of clastic sedimentary petroleum reservoirs and enclosing rocks, which allowed assessing the stability of rock when drilling exploration and production wells (mineral composition, structural-textural features, lithogenetic change, etc.). The findings about membership of the studied rocks to the products of early and late mezocatagenesis are presented.
topic литогенетические особенности горных пород
минеральный состав
структура и текстура горных пород
мезокатагенез
url http://geology-vestnik.psu.ru/index.php/geology/article/view/324
work_keys_str_mv AT kpkazimov lithogeneticfeaturesofrockscontainingproductiveoildepositsinthelowercarboniferousterrigenousstrata
AT nemoloshtanova lithogeneticfeaturesofrockscontainingproductiveoildepositsinthelowercarboniferousterrigenousstrata
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