Evolution of the crust in Belarus recorded in paleodynamics of the gravityfield

Different stages of evolution of geological structures are recorded in time dynamics of their gravity field. The regularities of the crust evolution o n the territory of Belarus were investigated through claculation and geolog ical interpretetation of the gravity field dynamics in a succession of dens ity models that reflect the main stages of the tectonic history of the regi on: Early Archean-Late Archean-Early Proterozoic-Riphean-Vendian-Late Paleo zoic (Devonian-Carboniferous).