Structural position and some features of the geological structure and the development of the Black Sea Depression

The structural position of the Black Sea deep-sea depression is generally determined by its location in area intersection diagonal transcontinental tectonolineament belts. different thickness deposits same age depressions emphasizes bloc structure earth's crust water area. Space photographs clearly show contours are enveloping long arcs mountain ranges and valleys Caucasus, Ajaro-Trialetia, Eastern Western Pontides. Such large oval arcuate, partially sequentially superimposed structures (the Miesian plate, Pannonian Bohemian massifs) characteristic entire southeastern border East European platform reflect activity processes destruction southern foreland zone development classic geosyncline. available data allow us to assume nature depression, formed as a result mainly vertical tectonic movements field mantle plume activations.