Comparative analysis of GPS, seismic and electromagnetic data on the central Tien Shan Territory

On the base of the GPS-measured velocity field referring to the recent crust movements over sizable terrestrial areas (Central Tien Shan), the strain rate tensor is evaluated as the tensor components are governed by space gradients of the velocity field. The areas of the extreme values of the strain rate tensor components are shown to coincide with the highest seismic activity areas. Also shown is the fact that, in the direction of the crust surface layer compression, the deep layer electric conductivity reaches its maximum. A simplest explanation of this phenomenon is proposed.