The source process of two normal-fault earthquakes, the 3 February 2002, M6.3 Afyon, Turkey and the 7 September 1999, M5.9 Athens, Greece earthquakes are studied using regional, teleseismic and strong motion data. Detailed information derived from teleseismic waveform modeling and source time functions inversions are combined and used to forward model recorded strong ground motion. Both events presented evidence for emergence of strong directivity effects during their rupture, which greatly affected the distribution of strong ground motion. These results are indicative of the contribution of the source factor to the distribution of earthquake damage and consequently of its importance in engineering practice in the proximity of large faults, especially within urban areas
