Paleomagnetism of granites from the Angara-Kan basement inlier, Siberian craton
A.N. Didenko a,b , I.K. Kozakov c , A.V. Dvorova b
a Kosygin Institute of Tectonics and Geophysics, Far Eastern Branch of the RAS, 65 ul. Kim Yu Chena, Khabarovsk, 680000, Russia
b Geological Institute, Russian Academy of Sciences, 7 Pyzhevsky per., Moscow, 119017, Russia
c Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, 21 nab. Makarova, St. Petersburg, 199034, Russia
Keywords: Paleoproterozoic; paleomagnetic pole; Siberian craton
Pages: 57-62
Abstract
We report a new paleomagnetic determination of Paleoproterozoic rocks from the Siberian craton which showed a positive baked contact test and a stable age of the high-temperature NRM component. The mean paleomagnetic pole of Siberia for ~1730 Ma located at 42.9
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