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The August 17 1999 İzmit earthquake M7 4 Eastern Marmara
Surface Fault Rupture and Segmentation During the Kocaeli
The fault breaks of the 1999 earthquakes in Turkey and
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17 August acceleration activity aftershock associated August 17 Barka basin branch buildings calculated caused changes complex consistent damage deformation depth determined direction displacement distribution Düzce Düzce earthquake east eastern effects epicenter estimated et al extended fault rupture fault segment fault zone field Figure focal functions geometry Geophys Gölcük ground Hersek increase indicate inversion Istanbul Izmit earthquake Karadere Kocaeli Lake lateral length located magnitude mainshock mapped Marmara Sea maximum measurements mechanism motion normal faulting North Anatolian Fault northern November 12 observed obtained occurred offset parameters peak period plane propagation recorded region relative release Research response ridge Sapanca segment seismic shock shown shows slip solutions stations stepover stress strike strike-slip structures suggest surface rupture tectonic trace trench Turkey University vertical wave waveforms western Yalova