Яндекс.Метрика

Д.В. Метелкин, В.А. Верниковский,И.В.Белоносов

: Доклады РАН

The available geologic indicators of accretion-collisional events associated with the collision of the Predivinsk terrane and Siberian craton in combination with the obtained paleomagnetic data imply that the island arc obduction to the continent periphery occurred shortly after the considered volcanic complex formation. The Predivinsk island arc terrane 640 mln years ago was located in the direct vicinity from its periphery. Correspondingly, the calculated paleomagnetic pole in the first approximation can be used for constructing Neo-Proterozoic interval of apparent pole motion trajectory for Siberia.
индекс в базе ИАЦ: 023968