KFU. Card publication. Carbonate formation of the Lower Carboniferous in central part of Volga-Ural basin

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FEDERAL UNIVERSITY

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

Form of presentation

Articles in international journals and collections

Year of publication

2014

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Authors, employees of KFU

Eskin Aleksey Aleksandrovich, author

Kolchugin Anton Nikolaevich, author

Korolev Eduard Anatolevich, author

Morozov Vladimir Petrovich, author

Bibliographic description in the original language

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

Annotation

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 ..

Keywords

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

The name of the journal

Current Science

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=119798&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Eskin Aleksey Aleksandrovich	ru_RU
dc.contributor.author	Kolchugin Anton Nikolaevich	ru_RU
dc.contributor.author	Korolev Eduard Anatolevich	ru_RU
dc.contributor.author	Morozov Vladimir Petrovich	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/eng/?p_id=119798&p_lang=2	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	Articles in international journals and collections	ru_RU