CLINOFORMS IN THE UPPER PART OF THE SEDIMENTARY COVER OF THE CENTRAL CASPIAN

dc.contributor.author	Lebedev L.I.
dc.contributor.author	Skorobogat'ko A.N.
dc.date.accessioned	2020-10-06T05:07:27Z
dc.date.available	2020-10-06T05:07:27Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31088169
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 2, 98-100
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17720
dc.description.abstract	Processes of hydrocarbon accumulation in oil and gas basins are controlled by various geologic bodies, including the so-called clinoforms, which certainly affect these processes. It is very important to determine the origin of clinoforms in sedimentary strata. Clinoforms usually are confined to zones of uncompensated downwarping. An example of such zones is the central Caspian, where geoacoustic profiling carried out to study the structure of the upper part of the sedimentary cover revealed various wedge-shaped sedimentary bodies. They are expressed most clearly in the structure of the Quaternary deposits in the southern part of the basin, where they were mapped in detail.
dc.subject	Quaternary	en
dc.title	CLINOFORMS IN THE UPPER PART OF THE SEDIMENTARY COVER OF THE CENTRAL CASPIAN
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary	en
dc.subject.age	Кайнозой::Четвертичная	ru

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