THE LATE PROTEROZOIC POSITION OF THE UKRAINIAN SHIELD FROM PALEOMAGNETIC DATA

dc.contributor.author	Mikhailova N.P.
dc.contributor.author	Kravchenko S.N.
dc.date.accessioned	2020-04-08T04:42:09Z
dc.date.available	2020-04-08T04:42:09Z
dc.date.issued	1987
dc.identifier	https://elibrary.ru/item.asp?id=30901702
dc.identifier.citation	JOURNAL OF GEODYNAMICS, 1987, 7, 1-2, 69-77
dc.identifier.issn	0264-3707
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16365
dc.description.abstract	On the basis of the paleomagnetic study of 300 dykes of various composition and with ages ranging from 2300 to 600 Ma, it is established that the peri-equatorial position of the Ukrainian Shield for this time span was rather stable, with latitudes displaced by no more than 30°. At the very beginning of the Riphean, the Ukrainian Shield was turning counter-clockwise at a rate of 0,05°/1 Ma.The drift of the Ukrainian Shield in the Proterozoic is not conformable with that of the Baltic Shield. The former is more mobile structure than the latter. This implies a new viewpoint of the consolidation of the basement of the East-European Platform.
dc.subject	Proterozoic	en
dc.title	THE LATE PROTEROZOIC POSITION OF THE UKRAINIAN SHIELD FROM PALEOMAGNETIC DATA
dc.type	Статья
dc.subject.age	Precambrian::Proterozoic	en
dc.subject.age	Докембрий::Протерозой	ru

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