Magnetic inhomogeneity of the Earth’s crust of the Dnieper-Donetsk Basin along the profiles GEORIFT 2013 and Dykanka-Druzhkivka

For the first time, there was performed a comprehensive analysis of the geomagnetic field and magnetic heterogeneity of the Earth’s crust with structural features and longitudinal wave velocities, detected according to deep seismic sounding (DSS) data along the GEORIFT 2013 and Dykanka-Druzhkivka (XII) profiles within the Dnieper-Donets Basin. The relationship of the magnetic heterogeneity of the crystalline Earth’s crust with seismic boundaries along refracted and reflected waves, as well as with deep faults in the meridional and submeridional directions, was shown. The hydrocarbon deposits are localization, the intersections of faults and transregional tectonic seams with longitudinal and sublatitudinal faults, which are often accompanied by local magnetic anomalies.