ИСТИНА

Modern paleomagnetic data allow for developing reliable APWP for the Siberian platform. Comparison of the Siberian and European APWPs show that since the Mesozoic time both platforms were part of the North Eurasian tectonic plate (North part of Pangea supercontinent). The plate was located in close to the modern coordinates and drifted with clockwise rotation. Since the early Jurassic time, the eastern part of the Siberian platform reached the North Pole. During the Jurassic period, the rotation was maintained and by the end of the period the plate occupied a sublatitudinal position.