A MECHANISM OF THE FORMATION OF DEEP SEDIMENTARY BASINS ON CONTINENTS: THE BARENTS BASIN

dc.contributor.author	Artyushkov E.V.
dc.date.accessioned	2022-07-25T04:36:24Z
dc.date.available	2022-07-25T04:36:24Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13461616
dc.identifier.citation	Doklady Earth Sciences, 2004, 397, 5, 595-599
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38381
dc.description.abstract	Inside continents and on their edges, deep sedimentary basins such as Caspian, Southern Caspian, Barents, Black-Sea, and other ones exist. Thickness of sediment layers in them are 15 to 20 km and more. According one version of mechanism of forming the basin, tension of lithosphere is reason for arising the basin. According other version of mechanism of forming the basin, rock compaction in lower crust due to phase transition is reason for arising the basin. Formation of Barents basin has been considered. Rocks in the basin have been investigated. Results of the investigations that the main reason of the basin formation is rock compaction.
dc.title	A MECHANISM OF THE FORMATION OF DEEP SEDIMENTARY BASINS ON CONTINENTS: THE BARENTS BASIN
dc.type	Статья

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