Reconstruction of seismic DSS crosssection of the VI geotravers and detaling of velocity characteristics of the earth crust in the gravity Bandura structure

摘要

The paper proposes reinterpretation of digitized seismic hodographs of geotraverse VI (on the distance 440-520), and further calculation of the velocity model using tomographic inversion in order to clarify the deep structure of the Pobuzkyi mining-ore district (PMOD) of the Ukrainian shield (USh), which is characterized by various mineral complexes of crystalline Precambrian rocks.