Reflection of Cenozoic geodynamics of Byelorussian Polessye relief in potamological indicators

Abstract

Geodynamic features of Byelorussian topography have been studied using the indicational analysis of elements of buried Neogene valleys and present-day drainage network revealed by the remote survey. It has been inferred that the Late Oligocene - Anthropogene tectonic and geodynamic processes, as reflected in the morphology of river valleys, were controlled by the structural setup of both the platform cover and the basement of the Pripyat Depression.