Paleomagnetism of 1780-1770 Ma mafic and composite intrusions of Smaland (Sweden): implications for the mesoproterozoic supercontinent

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ID: 294786
2010
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Abstract
We present a paleomagnetic study of 1785 to 1770 Ma composite and mafic intrusions in Småland, Sweden. A positive inverse baked contact test suggests the primary nature of their magnetization. The palaeomagnetic pole (45.7°N, 182.7°E, A~95~=8.0°) may be regarded as a key pole for Fennoscandia. Available paleomagnetic data suggest that Laurentia and Fennoscandia/Baltica drifted together since 1780 Ma until at least 1265 Ma. These two continents could form a core of a hypothetical Mesoproterozoic supercontinent.
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Authors Sergei Pisarevsky, Göran Bylund
Journal american journal of science
Year 2010
DOI
10.2475/09.2010.15
URL
https://ajs.scholasticahq.com/article/61844.pdf
Keywords Keywords not found

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