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dc.contributor.authorElming, S.
dc.contributor.authorPisarevsky, Sergei
dc.contributor.authorLayer, P.
dc.contributor.authorBylund, G.
dc.date.accessioned2017-01-30T15:05:25Z
dc.date.available2017-01-30T15:05:25Z
dc.date.created2015-02-01T20:00:58Z
dc.date.issued2014
dc.identifier.citationElming, S. and Pisarevsky, S. and Layer, P. and Bylund, G. 2014. A palaeomagnetic and 40Ar/39Ar study of mafic dykes in southern Sweden: A new Early Neoproterozoic key-pole for the Baltic Shield and implications for Sveconorwegian and Grenville loops. Precambrian Research. 244: pp. 192-206.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/43175
dc.identifier.doi10.1016/j.precamres.2013.12.007
dc.description.abstract

We present the results of palaeomagnetic and40Ar/39Ar studies of the Proterozoic mafic dykes in the Norrköping and Falun areas of the southern Sweden. The primary remanence of two 939 ± 3 Ma dykes is supported by the rigorous baked contact test. The remanence direction of two other dykes, one of which was previously U–Pb dated at 946 ± 1 Ma is close to the reverse direction of 939 Ma dykes. Using these results together with previously published 935 ± 5 Ma palaeomagnetic data from the Göteborg-Slussen mafic dykes and some dykes from the Falun area we calculated the mean 946–935 Ma palaeopole for Baltica (0.9° S, 240.7° E, A95= 6.7), which can be qualified as the key pole. Using this pole together with other date we conclude that the Grenville and Sveconorwegian loops of Laurentian and Baltican Apparent Polar Wander Paths are temporary displaced by 100–150 m.y. We propose new palaeogeographic reconstructions of Baltica and Laurentia at ca. 940 Ma and ca. 850 Ma. We also present two new Mesoproterozoic non-key poles from 1410 Ma and 1595 Ma dykes.

dc.publisherElsevier BV
dc.subjectKey pole
dc.subjectPalaeomagnetism
dc.subjectBaltica
dc.subjectPalaeogeography
dc.subjectMesoproterozoic
dc.subjectNeoproterozoic
dc.titleA palaeomagnetic and 40Ar/39Ar study of mafic dykes in southern Sweden: A new Early Neoproterozoic key-pole for the Baltic Shield and implications for Sveconorwegian and Grenville loops
dc.typeJournal Article
dcterms.source.volume244
dcterms.source.startPage192
dcterms.source.endPage206
dcterms.source.issn0301-9268
dcterms.source.titlePrecambrian Research
curtin.departmentDepartment of Applied Geology
curtin.accessStatusFulltext not available


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