PETROLOGY OF POSTOROGENIC GRANITOIDS OF THE NORTHERN BALTIC SHIELD

dc.contributor.author	Vetrin V.R.
dc.contributor.author	Berezhnaya N.G.
dc.contributor.author	Rodionov N.V.
dc.date.accessioned	2024-10-27T02:28:48Z
dc.date.available	2024-10-27T02:28:48Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13518439
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 9, 1476-1479
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46268
dc.description.abstract	In the northern Baltic Shield, diorites, monzodiorites, and quartz diorites are constituents of postorogenic granite massifs, the localization of which was controlled by NE- and NW-trending fault zones. The NE-trending transform faults controlled the emplacement of the Litsa–Aragub and Yuovvoaiv complexes (1.77–1.76 and 1.79–1.77 Ga old, respectively); the Vainospäa Massif; and, probably, the “Nattanen-type” massifs (Nattanen, Tepasto, Pomovaara, Riestovaara) (1.8 to 1.77 Ga old [3]) located at the southern framing of the Lapland granulite belt.
dc.subject	Baltic shield
dc.subject	granitoids
dc.title	PETROLOGY OF POSTOROGENIC GRANITOIDS OF THE NORTHERN BALTIC SHIELD
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06090327

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