PALAEOMAGNETIC CONFIGURATION OF CONTINENTS DURING THE PROTEROZOIC

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dc.contributor.authorPesonen L.J.
dc.contributor.authorElming S.A.
dc.contributor.authorMertanen S.
dc.contributor.authorPisarevsky S.
dc.contributor.authorD'Agrella-Filho M.S.
dc.contributor.authorMeert J.G.
dc.contributor.authorSchmidt P.W.
dc.contributor.authorAbrahamsen N.
dc.contributor.authorBylund G.
dc.date.accessioned2022-02-21T00:48:16Z
dc.date.available2022-02-21T00:48:16Z
dc.date.issued2003
dc.description.abstractPalaeomagnetic 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.identifierhttps://elibrary.ru/item.asp?id=14369467
dc.identifier.citationTectonophysics, 2003, 375, 1-4, 289-324
dc.identifier.issn0040-1951
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/35586
dc.subjectPalaeomagnetism
dc.subjectProterozoic
dc.subjectSupercontinent
dc.subjectMantle plume
dc.subjectKenorland
dc.subjectHudsonland
dc.subjectColumbia
dc.subjectRodinia
dc.subjectPalaeolatitude
dc.subjectPalaeogeography
dc.subjectAccretion
dc.subjectMafic dykes
dc.subject.agePrecambrian::Proterozoic
dc.subject.ageДокембрий::Протерозойru
dc.titlePALAEOMAGNETIC CONFIGURATION OF CONTINENTS DURING THE PROTEROZOIC
dc.typeСтатья

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