Magnetotelluric and Seismic Natural Fields Complex for Geodynamic Research

Magnetotelluric and seismic (P-SV converted waves data) field works were fulfilled in Western and Central Caucasus. These exploration works showed, that the sedimentary cover of Indolo-Cuban depression is about 12 km. In the limits of Scifian plate was framed lover floor folded basis (r = 100-300 Ohm.m). Zones of conductivity under the Elbrus mountain are correlated with the absence converted waves. The boundaries between geoelectric inhomogeneities are corresponded with deep faults.