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THE EVOLUTION OF THE STRESS FIELD IN EASTERN MACEDONIA AND THRACE
Bulletin of the Geological Society of Greece
Eastern Macedonia and Thrace are characterized by moderate seismicity compared to the adjacent North Aegean area, as it is derived from both historical information and instrumental records. The known strong (M>6.5) historical earthquakes that occurred during the past three centuries, however, have caused appreciable casualties and for this reason the seismic hazard assessment in the study area is of considerable social importance. These events (Didimoteiho earthquake (M=7.4) in 1752, Komotinidoi:10.12681/bgsg.16580 fatcat:uizqy5ntp5barhbggnto4yiqiy