PALAEOMAGNETIC CONFIGURATION OF CONTINENTS DURING THE PROTEROZOIC

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dc.contributor.author Pesonen L.J.
dc.contributor.author Elming S.A.
dc.contributor.author Mertanen S.
dc.contributor.author Pisarevsky S.
dc.contributor.author D'Agrella-Filho M.S.
dc.contributor.author Meert J.G.
dc.contributor.author Schmidt P.W.
dc.contributor.author Abrahamsen N.
dc.contributor.author Bylund G.
dc.date.accessioned 2022-02-21T00:48:16Z
dc.date.available 2022-02-21T00:48:16Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=14369467
dc.identifier.citation Tectonophysics, 2003, 375, 1-4, 289-324
dc.identifier.issn 0040-1951
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/35586
dc.description.abstract Palaeomagnetic data are used to study the configurations of continents during the Proterozoic. Applying stringent reliability criteria, the positions of the continents at 12 times in the 2.45- to 1.00-Ga period have been constructed. The continents lie predominantly in low to intermediate latitudes. The sedimentological indicators of palaeoclimate are generally consistent with the palaeomagnetic latitudes, with the exception of the Early Proterozoic, when low latitude glaciations took place on several continents.
dc.subject Palaeomagnetism
dc.subject Proterozoic
dc.subject Supercontinent
dc.subject Mantle plume
dc.subject Kenorland
dc.subject Hudsonland
dc.subject Columbia
dc.subject Rodinia
dc.subject Palaeolatitude
dc.subject Palaeogeography
dc.subject Accretion
dc.subject Mafic dykes
dc.title PALAEOMAGNETIC CONFIGURATION OF CONTINENTS DURING THE PROTEROZOIC
dc.type Статья
dc.subject.age Precambrian::Proterozoic
dc.subject.age Докембрий::Протерозой ru


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