Paleomagnetism of granites from the Angara-Kan basement inlier, Siberian craton

摘要

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 similar to 1730 Ma located at 42.9 degrees S, 109.6 degrees E (alpha(95) = 5.3 degrees) is compatible with the pole positions obtained recently for the middle and late Early Proterozoic.