MATHEMATICAL MODELING OF OVERTHRUSTING FAULT AS A CAUSE OF ANDALUSITE-KYANITE METAMORPHIC ZONING IN THE YENISEI RIDGE

dc.contributor.author	Korobeinikov S.N.
dc.contributor.author	Polyansky O.P.
dc.contributor.author	Likhanov I.I.
dc.contributor.author	Sverdlova V.G.
dc.contributor.author	Reverdatto V.V.
dc.date.accessioned	2024-10-23T07:15:46Z
dc.date.available	2024-10-23T07:15:46Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13509031
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 652-656
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46112
dc.description.abstract	Regional structural features of the Yenisei Ridge are traditionally displayed as a NW-trending linear system of tectonic sheets that are thrust over one another and separated by faults where collision of blocks occurs. As a result, low- and moderate-pressure series of regional metamorphism turn out to be juxtaposed. Moderate-pressure metamorphism related to collision is locally superimposed on low-pressure metamorphic rocks. Therefore, andalusite is progressively replaced with kyanite, and new mineral assemblages of moderate pressure and deformational microstructures are formed.
dc.subject	Yenisei ridge
dc.title	MATHEMATICAL MODELING OF OVERTHRUSTING FAULT AS A CAUSE OF ANDALUSITE-KYANITE METAMORPHIC ZONING IN THE YENISEI RIDGE
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06040325

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