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A seismic source is defined, in the present work, as the part of the seismogenic layer of the earth’s crust with a circular horizontal dimension (E, R), where E is the epicenter of the largest earthquake (mainshock) ever occurred in this seismic source and radius equal to the half fault length of this largest earthquake (R=L/2). In addition to foreshocks and aftershocks other smaller mainshocks occur in other smaller faults of this source or in parts of the main fault. All available historical and instrumental data concerning strong (M≥6.0) shallow (h≤60 km) and intermediate depth (60km<h≤100km) shocks which occurred in the Aegean area between 464 B.C. and 2008 are used in the present work in an attempt to identify the seismic sources in this area, as well as to determine the basic parameters of the largest fault in each source. A particular procedure is followed to identify 155 seismic sources in this area and determine the basic parameters of the largest fault in each source. Declustering has been also performed to define mainshocks in the Aegean area and the completeness of this mainshock catalogue has been determined. Results are summarized in table (1).

SEISMIC SOURCES AND MAIN SEISMIC FAULTS IN THE AEGEAN AND SURROUNDING AREA