Abstract
Formation of eastern frontier of the Siberian craton is bound to the riftogenny processes, which split the continent at the end of the Middle Paleozoic. The paleomagnetic data obtained on middle Paleozoic kimberlites and bazites from a zone of dynamic influence of the Vilyui paleorift indicate a turn of the Aldan terreyn rather Angaro-Anabar clockwise in the post-late Devonian time. The corner of a turn of terreyn gradually increases in east direction and reaches 22° for east flank of the Charo-Sinsk dyke belt.
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