GEOLOGIC - TECTONICAL STRUCTURE AND SEISMISITY OF THE AZERBAIJANIAN PART OF THE GREAT CAUCASUS AND ADJOIN TERRITORIES

Regional geologic-geophysical investigations allowed interpretation Stuctures and Comosition of the Alpine cover and more deep norizons of the eart's Crust up to ۵۰-۶۰ km and corfirmed of the Onenomenon of its tectonic laminated with the Southern vergence geostructural Zones of the "Common (... )" Stretch and deep fractures limiting them. which refleci the phenorrenon of the motion of every South zone under the north one. Studying of focus zones location regularity reflects the correlation of the earthquakes focuses with subnorizontal and subvertical boundaries in the earth's crust, what show their structural - name correlation.