Abstract: | Based on geological and geophysical data, characteristics of neotectonic activity of the eastern border of the Pannonian Depression are presented.As a result of differential tectonic movements during the Neogene-Quaternary, separate morphostructural units are subjected to subsidence and uplifting, along active faults.The local seismic activity is related, mainly, to the movements along the borders of grabens, as well as at the contact between different crustal blocks. |