WAS BALTICA RIGHT-WAY-UP OR UPSIDE-DOWN IN THE NEOPROTEROZOIC?

Cawood P.A.; Pisarevsky S.A.

dc.contributor.author	Cawood P.A.
dc.contributor.author	Pisarevsky S.A.
dc.date.accessioned	2024-12-07T09:08:13Z
dc.date.available	2024-12-07T09:08:13Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=14718940
dc.identifier.citation	Journal of the Geological Society, 2006, 163, 5, 753-759
dc.identifier.issn	0016-7649
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46897
dc.description.abstract	Baltica is a progeny of Rodinia, born from the breakup of the supercontinent in the Neoproterozoic. Within Rodinia, Baltica is generally placed adjacent to NE Laurentia but in a variety of configurations, which vary by up to 3000 km along the strike of the Laurentian margin and include both right-way-up and upside-down orientations (current coordinates). Geological and palaeomagnetic data show that the only viable reconstruction juxtaposes the western Scandinavian margin of Baltica, in its right-way-up orientation, against the Rockall-Scotland-SE Greenland segment of Laurentia.
dc.subject	Neoproterozoic
dc.title	WAS BALTICA RIGHT-WAY-UP OR UPSIDE-DOWN IN THE NEOPROTEROZOIC?
dc.type	Статья
dc.identifier.doi	10.1144/0016-76492005-126
dc.subject.age	Precambrian::Proterozoic::Neoproterozoic
dc.subject.age	Докембрий::Протерозой::Неопротерозойская