THE SOUTH CASPIAN BASIN: A REVIEW OF ITS EVOLUTION FROM SUBSIDENCE MODELLING

dc.contributor.author	Brunet M.-F.
dc.contributor.author	Korotaev M.V.
dc.contributor.author	Ershov A.V.
dc.contributor.author	Nikishin A.M.
dc.date.accessioned	2022-02-15T07:16:12Z
dc.date.available	2022-02-15T07:16:12Z
dc.date.issued	2003
dc.identifier	https://elibrary.ru/item.asp?id=13425231
dc.identifier.citation	Sedimentary Geology, 2003, 156, 1-4, 119-148
dc.identifier.issn	0037-0738
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/35396
dc.description.abstract	The basement surface of the South Caspian depression lies at a depth of 20–25 km, making it one of the deepest basins in the world. It occupies the southern, deep-water, part of the Caspian Sea and two adjacent lowlands: the West Turkmenia in the east and the Lower Kura in the west. The basin can be subdivided into several sub-basins with two main depocentres, one in the northern part of the basin, just on the southern flank of the Apsheron Sill, and one, called the Pre-Alborz trough, located in the south-eastern part of the marine basin.
dc.title	THE SOUTH CASPIAN BASIN: A REVIEW OF ITS EVOLUTION FROM SUBSIDENCE MODELLING
dc.type	Статья

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