Magnetic models of the Earth's crust along the profiles of dss 25, dss 28 and dss 29 (in connection with the investigation of the transition zone from the East European platform to the Black sea megadepression)
It is shown, that the highly magnetic crust is confined to the riftogenic deflections and fordeeps within the transition zone from the East - European Platform to the Black Sea megadepression, and the weakly magnetic and non-magnetic crust - to the Mesozoic and Paleozoic sutures.