DATA OF DEEP GEOPHYSICAL SURVEYS ALONG CHEGEM PROFILE (CENTRAL BLOCK, THE GREATER CAUCASUS)

Abstract

Geophysical observations along the chegemsky profile (pass Titled - Budennovsk) are a continuation of the deep studies of the structure of the greater Caucasus the complex geophysical characteristics of the section of the earth crust in the cross the entire structure of the orogen. On the basis of actual materials of the method of exchange waves of earthquakes, the method of telluric current and gravity-filming separate elements of the structure of the greater Caucasus as part of the Alpine collisional belt, obviously occurred when the canopy on thrusting from the North of the earth’s crust of the Scythian plate in the consolidated crust of the Transcaucasian microplate.