Western structural closing of the Pripyat–Dneprov–Donetsk aulacogen

In segmented paleorift systems such as the Pripyat–Dnieper–Donetsk aulacogen, which penetrate deep into continent from side of paleoocean margin and most often close here, each segment represents an autonomous structure lithosphere. The presented article shows that tectonic position Pripyat western closing indicated aulacogen was due to a change in intensity syn-rift plate-tectonic processes extended rift system east west. band Paleoproterozoic Fenno-Sarmatian collision, Central Belarusian suture zone Russian transpression belt isolated by S. V. Bogdanova 2018 blocking transverse barrier relative development Hercynian synrift direction.