Figure 17. Interpretation of the tectonic environment in the Pripyat Paleorift in terms of the forward-rotation
movement of the Internal Graben block, constructed by T. A. Starchik and R. E. Aisberg.
(1) Marginal faults of the Pripyat-Donetsk aulacogen; (2) western boundary of the Pripyat Paleorift; (3) the
angle and direction of the inferred rotations of the North Pripyat and South Pripyat marginal faults relative
to those of the Dnieper-Donetsk aulacogen; (4) the vector of the main extension stress of the paleorift;
sketch of the dynamic effect of the Bragin stamp; (5) vector of active force and the trajectories of the
compression (6) and extension (7).