EVIDENCE FOR SVECONORWEGIAN (GRENVILLIAN) MAGMATIC ACTIVITY IN THE NORTHWESTERN BALTIC SHIELD

dc.contributor.author	Arzamastsev A.A.
dc.contributor.author	Arzamastseva L.V.
dc.contributor.author	Fedotov Zh.A.
dc.contributor.author	Montero P.
dc.contributor.author	Bea F.
dc.contributor.author	Travin A.V.
dc.date.accessioned	2024-10-23T07:15:47Z
dc.date.available	2024-10-23T07:15:47Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13509043
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1034-1037
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46115
dc.description.abstract	The crustal structure in the Baltic Shield is determined by a system of geological blocks, which formed at different evolutionary stages of this largest stable Precambrian domain. Cratonization of the Archean Karelian, Kola, and Belomorian domains terminated after the Svecofennian orogeny 1.88–1.75 Ga ago. Up to now, the principal structural elements of the shield formed by that time have remained practically unchanged over its entire area.
dc.subject	Baltic Shield
dc.title	EVIDENCE FOR SVECONORWEGIAN (GRENVILLIAN) MAGMATIC ACTIVITY IN THE NORTHWESTERN BALTIC SHIELD
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070075
dc.subject.age	Докембрий::Архей

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