STRUCTURE AND DEVELOPMENT OF THE MAIN LAYERS OF LITHOSPHERE OF THE PRIPYAT TROUGH AND ADJACENT STRUCTURES
A set of Maps describing the deep structure and tectonic vertical stratification of the earth's crust has been designed for the territory of the Pripyat Trough and neighboring areas: maps of the thicknesses of the main layers of the consolidated crust - “granite”, “diorite”, “basalt” and the topography of the surfaces of these layers, as well as the surface Moho. As a result of the tectonophysical interpretation of the proposed set of Maps and the DSS materials, the authors have developed a concept for the formation of the Pripyat Paleorift, which includes the four leading factors - the activation of the Sarmatian-Turanian lineament, the convergence of the Fennoscandian and Sarmatian tectonic plates, the elevation of the hot asthenospheric lens and the isostatic process.