A tectonogeodynamic model for the junction zone between the Fennoscandian and Sarmatian segments of the East European Platform

Seismic gravity modeling along the Eurobridge-96–Eurobridge-97 DSS geotransects has shown that the Central Belarus suture zone formed in the Paleoproterozoic as a results of the subduction and collision processes at the convergent junction of the Fennoscandian and Sarmatian segments of the East European Platform. The influence of pre-Riphean processes on the subsequent tectonic events occurring on the territory of Belarus during the Phanerozoic has been established.