Palinspastic reconstruction of the relative position of the important Devonian sections in the north-east of the Pechora basin at the time of their formation was performed by structural methods. It is shown that the displacement of Preduralskii marginal basin’s sections relative to their position in the Devonian increases from west to east, but does not exceed 60 km. The displacement sections of the Polar Urals and Pai-Khoi is estimated to be 80-100 km.