Seismic tomographic model along the geotraverse VI profile

Inner structure and kinematics of the Sushchany-Perga fault zone of the Ukrainian Shield according to the tectonophysical study

“…SP and Horyn fault zones dipping to the SE and can be traced to the Moho surface at a depth of 55 km in the obtained section [Ilchenko, 1985;Sollogub, 1986Sollogub, , 1988. It was reinterpreted the seismic materials and constructed a seismic tomographic model along the VI line of geotraverse that made it possible to clarify the earth crust structure in the vicinity of SP fault zone [Lysynchuk et al, 2019[Lysynchuk et al, , 2020. At the profile distances between the PC 900-840 in terms of the velocity structure (within the velocity values of 5.0 to 6.0 km/s) we can observe a trough down to the depth of 15 km which corresponds to the trough of the OMIB with the Paleoproterozoic crust.…”

“…In the Podolian Domain between 750-620 pickets, velocity uplift is marked at the depth of 25 km from the velocity isoline of 7.0 km/s in lower crust up to the surface at PC 650 with a velocity of 5.25 km/s. The upper crust of the Volyn block lies at depths of 7-21 km, the middle crust -at depths of 20-35 km, and the surface of Moho lies at a depth of 45-50 km [Lysynchuk et al, 2020].…”