EARLY PROTEROZOIC MAGMATIC BELT OF THE MOSCOW REGION

dc.contributor.author	Bogdanova S.V.
dc.contributor.author	Bibikova E.V.
dc.contributor.author	Postnikov A.V.
dc.contributor.author	Taran L.N.
dc.date.accessioned	2022-08-03T05:20:56Z
dc.date.available	2022-08-03T05:20:56Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13464348
dc.identifier.citation	Doklady Earth Sciences, 2004, 395, 3, 315-318
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38440
dc.description.abstract	The Moscow region is situated in the most complicated tectonic junction of the East European Craton (EEC), characterized by the intrusion of tectonic units of various orders and ages, such as the wedge of the Neoarchean Volga-Ural segment from the east, Neoarchean and Paleoproterozoic structures of the Fennoscandian segment from the north, and Meso- and Neoarchean tectonic units of the Sarmatian segment from the south. All of these EEC crustal segments have sharply distinct Archean and Paleoproterozoic histories and are divided in their present-day structure by early-middle Proterozoic transcratonic (Central Russian-Volyn-Orsha and Pachelma) rift segments that inherited the Paleoproterozoic Ryazan-Saratov (Pachelma) collisional belt (∼2 Ga) and Central Russian collisional belt (1.80-1.75 Ga).
dc.subject	Proterozoic
dc.title	EARLY PROTEROZOIC MAGMATIC BELT OF THE MOSCOW REGION
dc.type	Статья
dc.subject.age	Precambrian::Proterozoic
dc.subject.age	Докембрий::Протерозой	ru

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