GEOLOGICAL EVOLUTION AND GENESIS OF THE CENTRAL PAMIRS

dc.contributor.author	Lutkov V.S.
dc.contributor.author	Dronov V.I.
dc.contributor.author	Minaev V.E.
dc.contributor.author	Babaev A.M.
dc.date.accessioned	2022-01-18T03:31:07Z
dc.date.available	2022-01-18T03:31:07Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=27769820
dc.identifier.citation	Doklady Earth Sciences, 2003, 391, 6, 794-796
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34394
dc.description.abstract	The central Pamirs (CP) as an element of the Alpine Afghanistan-Central Pamir-Tashkurgan Fold System (Fig. 1) is characterized by diverse and multistage sedimentation, magmatism, and metamorphism spanning a wide (Proterozoic-Cenozoic) time interval. Perfect exposures, deep vertical incisions, comprehensive geological investigations (especially in Tajikistan, and abundant information on crystalline basement and abyssal xenoliths allow us to use the CP as a test site for the study of evolution and genesis of intra-continental structures in the Alpine-Himalayan Mobile Belt.
dc.title	GEOLOGICAL EVOLUTION AND GENESIS OF THE CENTRAL PAMIRS
dc.type	Статья

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