The seismicity of Romania is clustered in several epicentral zones: Vrancea, Făgăraș-Câmpulung, Banat, Crișana, Maramureș, and Southern Dobrogea.

The Vrancea area is responsible for over 90% of all earthquakes in Romania, releasing over 95% of the seismic energy.

[4] Two belts of moderate and shallower seismicity are emphasized in the other regions of the country: one along the Southern Carpathians and the eastern edge of the Pannonian Basin, the other along the Eastern Carpathians that extends towards SE on the Peceneaga–Camena line.

All seismic events are shown in detail in the ROMPLUS catalog of the National Institute for Earth Physics.

After 1997, the catalog was permanently filled and updated with data on seismic events produced in Romania and around national borders.