Paleoseismic dislocations of the northeastern part of the Baltic Schield and their geological-tectonic position

Abstract

Local paleoseismic dislocations have been found in the Kola region as a result of specialized geologic and geomorphologic investigations. They are interpreted as a direct evidence of tectonic disturbances by strong ancient earthquakes, affecting both topographical relief and the bedrock. Paleoseismic dislocations are concentrated in specific localities - paleoseismic areas. The areas coincide with the position o particular Precambrian and neotectonic structures, which are characterized by differential movements.