Paleomagnetism of granites from the Angara-Kan basement inlier,Siberian craton |
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| Authors: | AN Didenko IK Kozakov AV Dvorova |
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| Institution: | 1. Kosygin Institute of Tectonics and Geophysics, Far Eastern Branch of the RAS, 65 ul. Kim Yu Chena, Khabarovsk, 680000, Russia;2. Geological Institute, Russian Academy of Sciences, 7 Pyzhevsky per., Moscow, 119017, Russia;3. Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, 21 nab. Makarova, St. Petersburg, 199034, Russia |
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| 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° S, 109.6° E (α95 = 5.3°) is compatible with the pole positions obtained recently for the middle and late Early Proterozoic. |
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