CLINOFORMS IN THE UPPER PART OF THE SEDIMENTARY COVER OF THE CENTRAL CASPIAN
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
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 |
Files in this item
Files | Size | Format | View |
---|---|---|---|
There are no files associated with this item. |
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru