COLLISIONAL METAMORPHISM AS A RESULT OF THRUSTING IN THE TRANSANGARA REGION OF THE YENISEI RIDGE

dc.contributor.author	Likhanov I.I.
dc.contributor.author	Popov N.V.
dc.contributor.author	Reverdatto V.V.
dc.contributor.author	Vershinin A.E.
dc.contributor.author	Kozlov P.S.
dc.date.accessioned	2024-11-02T11:07:43Z
dc.date.available	2024-11-02T11:07:43Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13520942
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 8, 1313-1317
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46332
dc.description.abstract	The Yenisei Ridge is one of the most interesting regions in the southwestern folded framework of the Siberian Craton with respect to geodynamics. The regional structure of the Transangara sector of the Yenisei Ridge is traditionally displayed as a NW-trending system of tectonic sheets divided by faults characterized by the collision of blocks and thrusting. Therefore, this region was subject to pressure-variable regional metamorphism expressed in the juxtaposition of low-and moderate-pressure metamorphic facies.
dc.subject	Yenisei ridge
dc.title	COLLISIONAL METAMORPHISM AS A RESULT OF THRUSTING IN THE TRANSANGARA REGION OF THE YENISEI RIDGE
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06080332

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