PALEOMAGNETISM OF PERMIAN THROUGH EARLY TRIASSIC SEQUENCES IN CENTRAL SPITSBERGEN: IMPLICATIONS FOR PALEOGEOGRAPHY

dc.contributor.author	Nawrocki J.
dc.date.accessioned	2021-01-09T03:54:52Z
dc.date.available	2021-01-09T03:54:52Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=129924
dc.identifier.citation	Earth and Planetary Science Letters, 1999, , 1, 59-70
dc.identifier.issn	0012-821X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22405
dc.description.abstract	Upper Carboniferous through Lower Triassic sediments from Spitsbergen have yielded paleomagnetic results, with those for the Late Gzhelian-Early Permian being the more reliable. The corresponding pole (38°N, 171°E) is fully concordant with the Early Permian segment of the apparent polar wander path for Baltica. It does not support hypotheses about post-Carboniferous mobilism of Spitsbergen with respect to Stable Europe. Neither Mesozoic nor later rifting processes changed the position of Spitsbergen considerably in relation to the Stable Europe.
dc.subject	SPITSBERGEN
dc.subject	PALEOMAGNETISM
dc.subject	PERMIAN
dc.subject	APPARENT POLAR WANDERING
dc.subject	PALEOGEOGRAPHY
dc.title	PALEOMAGNETISM OF PERMIAN THROUGH EARLY TRIASSIC SEQUENCES IN CENTRAL SPITSBERGEN: IMPLICATIONS FOR PALEOGEOGRAPHY
dc.type	Статья
dc.subject.age	Палеозой::Пермская	ru
dc.subject.age	Paleozoic::Permian	en

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