CONTINENTAL BREAK-UP AND COLLISION IN THE NEOPROTEROZOIC AND PALAEOZOIC - A TALE OF BALTICA AND LAURENTIA
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dc.contributor.author | Torsvik T.H. | |
dc.contributor.author | Smethurst M.A. | |
dc.contributor.author | Sturt B.A. | |
dc.contributor.author | Meert J.G. | |
dc.contributor.author | Van der Voo R. | |
dc.contributor.author | Walderhaug H.J. | |
dc.contributor.author | McKerrow W.S. | |
dc.contributor.author | Brasier M.D. | |
dc.date.accessioned | 2020-12-05T10:57:25Z | |
dc.date.available | 2020-12-05T10:57:25Z | |
dc.date.issued | 1996 | |
dc.identifier | https://elibrary.ru/item.asp?id=31709193 | |
dc.identifier.citation | Earth-Science Reviews, 1996, , 3, 229-258 | |
dc.identifier.issn | 0012-8252 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/20469 | |
dc.description.abstract | During the Neoproterozoic and Palaeozoic the two continents of Baltica and Laurentia witnessed the break-up of one supercontinent, Rodinia, and the formation of another, but less long-lived, Pangea. Baltica and Laurentia played central roles in a tectonic menage a trois that included major orogenic events, a redistribution of palaeogeography and a brief involvement of both with Gondwana. Many of these plate re-organisations took place over a short time interval and invite a re-evaluation of earlier geodynamic models which limited the speeds at which large continental plates could move to an arbitrarily low value. | |
dc.subject | Neoproterozoic | en |
dc.title | CONTINENTAL BREAK-UP AND COLLISION IN THE NEOPROTEROZOIC AND PALAEOZOIC - A TALE OF BALTICA AND LAURENTIA | |
dc.type | Статья | |
dc.subject.age | Precambrian::Proterozoic::Neoproterozoic | en |
dc.subject.age | Докембрий::Протерозой::Неопротерозойская | ru |
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