The East European craton at the end of the Paleoproterozoic: A new paleomagnetic pole of 1.79–1.75 Ga

Reliable paleomagnetic poles were calculated for 1.80–1.78 and 1.76–1.75 Ga as a result of the detailed paleomagnetic studies of the Late Paleoproterozoic igneous complexes and the North Ladoga region and Onega structure of the East European craton. According to the new paleomagnetic data, the final...

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Veröffentlicht in:	Moscow University geology bulletin 2016, Vol.71 (1), p.8-17
Hauptverfasser:	Lubnina, N. V., Pasenko, A. M., Novikova, M. A., Bubnov, A. Yu
Format:	Artikel
Sprache:	eng
Schlagworte:	Cratons Earth and Environmental Science Earth Sciences Geological time Geology Igneous rocks Magnetic fields Paleomagnetism
Online-Zugang:	Volltext
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