Geoelectric model of tectonosphere along the international geotraverse II (Carpathian region) on the basis of two-dimensional modeling of induction vectors
© I.M. Logvinov, V.N. Tarasov
On the basis of 2D interpretation of GDS data in 12 points located within a 10 km wide stripe along the geotraverse II from the Transcarpathian depression up to the Volyn-Podolsk plate, it was possible to compile a fairly reliable geoelectric model of this region. A set of anomalous objects have been distinguished within the Earth's crust of Carpathians with minimal electric resistance up to 0,5 Ohm × m. An anomalous object has been offered within the upper mantle with minimal electric resistances (less than 15 Ohm x m) spatially confined to the Krosno zone of Carpathians.