MAGNETIC INHOMOGENITY OF THE EARTH CRUST OF THE DNIEPER-DONETSK BASIN ALONG THE PROFILE GEORIFT 2013

For the first time, a combined analysis of the geomagnetic field and magnetic heterogeneity of the Earth's crust with structural features, which were revealed according to the data of the DSS along the longitudinal profile of GEORIFT 2013[1], was performed. It is shown that the deep sources of the Chernihiv and Lokhvytsk regional magnetic anomalies correspond to increased velocities of longitudinal seismic waves and the rise of seismic boundaries behind refracted and reflected waves. The magnetic sources of the upper part of the crystalline Earth's crust and the bottom of the sedimentary cover are characterized by an increased saturation of the boundaries of refracted and reflected waves, as well as a loss of their correlation and a change in the angles of inclination.