КФУ. Карточка публикации. Carbonate formation of the Lower Carboniferous in central part of Volga-Ural basin

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CARBONATE FORMATION OF THE LOWER CARBONIFEROUS IN CENTRAL PART OF VOLGA-URAL BASIN

Форма представления

Статьи в зарубежных журналах и сборниках

Год публикации

2014

Язык

английский

Авторы, сотрудники КФУ

Ескин Алексей Александрович, автор

Кольчугин Антон Николаевич, автор

Королев Эдуард Анатольевич, автор

Морозов Владимир Петрович, автор

Библиографическое описание на языке оригинала

Carbonate formation of the Lower Carboniferous in central part of Volga-Ural basin

Аннотация

Carbonate rocks of the Lower Carboniferous (Tournaisian stage) of the central Volga–Ural basin (the eastern portion of the East European platform) are of practical scientific interest to geologists, particularlybecause they contain large reserves of oil. Although such layers have been studied, various questions pertaining to development of sedimentation schemes for the rocks have not been answered. We have attempted to resolve these by studying a wealth of drill core materials. The study involved structural and genetic analysis of rocks and facies reconstructions. The rocks are mainly represented by different types of shallowwater limestone. The thickness of coeval layers and their lithological structures changes from well to well within an oilfield, primarily due to the different environments of sedimentation during the Tournaisian stage. Therefore, to identify the characteristics of carbonate sedimentation, we have studied the sequences of different types of limestone and analysed ..

Ключевые слова

Limestone, oil prospects, sedimentation, seabed topography, wave base level

Название журнала

Current Science

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https://repository.kpfu.ru/?p_id=119798

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Ескин Алексей Александрович	ru_RU
dc.contributor.author	Кольчугин Антон Николаевич	ru_RU
dc.contributor.author	Королев Эдуард Анатольевич	ru_RU
dc.contributor.author	Морозов Владимир Петрович	ru_RU
dc.date.accessioned	2014-01-01T00:00:00Z	ru_RU
dc.date.available	2014-01-01T00:00:00Z	ru_RU
dc.date.issued	2014	ru_RU
dc.identifier.citation	Carbonate formation of the Lower Carboniferous in central part of Volga-Ural basin	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/?p_id=119798	ru_RU
dc.description.abstract	Current Science	ru_RU
dc.description.abstract	Carbonate rocks of the Lower Carboniferous (Tournaisian stage) of the central Volga–Ural basin (the eastern portion of the East European platform) are of practical scientific interest to geologists, particularlybecause they contain large reserves of oil. Although such layers have been studied, various questions pertaining to development of sedimentation schemes for the rocks have not been answered. We have attempted to resolve these by studying a wealth of drill core materials. The study involved structural and genetic analysis of rocks and facies reconstructions. The rocks are mainly represented by different types of shallowwater limestone. The thickness of coeval layers and their lithological structures changes from well to well within an oilfield, primarily due to the different environments of sedimentation during the Tournaisian stage. Therefore, to identify the characteristics of carbonate sedimentation, we have studied the sequences of different types of limestone and analysed ..	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Limestone	ru_RU
dc.subject	oil prospects	ru_RU
dc.subject	sedimentation	ru_RU
dc.subject	seabed topography	ru_RU
dc.subject	wave base level	ru_RU
dc.title	Carbonate formation of the Lower Carboniferous in central part of Volga-Ural basin	ru_RU
dc.type	Статьи в зарубежных журналах и сборниках	ru_RU