Seismicity of the Sea of Marmara (Turkey) since 1500

SUMMARY We use the earthquake history of the last 500 years to help evaluate the tectonic and hazard contexts of the1999 earthquakes at Izmit and Dzce in westernTurkey.The 20th century has been unusually active, but over the 500 year period the seismic moment release can account for the known right-lateral shear velocity across the Marmara region observed by GPS. Two areas of known late Quaternary faulting stand out as unusually quiet over this period: the northwest shore of the Sea of Marmara and the southern branch of the North Anatolian fault system between Bursa and Mudurnu.

[1]  N. Ambraseys Engineering seismology: Part II , 1988 .

[2]  N. Ambraseys,et al.  THE ASSESSMENT OF TOTAL SEISMIC MOMENT , 1999 .

[3]  Steven G. Wesnousky,et al.  Scaling differences between large interplate and intraplate earthquakes , 1986 .

[4]  Izmit (Turkey) Earthquake of 17 August 1999: First Report , 1999 .

[5]  E. Engdahl,et al.  Global teleseismic earthquake relocation with improved travel times and procedures for depth determination , 1998, Bulletin of the Seismological Society of America.

[6]  James Jackson,et al.  Active tectonics of the north and central Aegean Sea , 1991 .

[7]  J. Jackson,et al.  Seismicity and Strain in the Gulf of Corinth (Greece) Since 1694 , 1997 .

[8]  Aral I. Okay,et al.  An active, deep marine strike‐slip basin along the North Anatolian fault in Turkey , 1999 .

[9]  A. Barka,et al.  Strike‐slip fault geometry in Turkey and its influence on earthquake activity , 1988 .

[10]  N. N. Ambraseys,et al.  Some characteristic features of the Anatolian fault zone , 1970 .

[11]  C. Papazachos Anisotropic radiation modelling of macroseismic intensities for estimation of the attenuation structure of the upper crust in Greece , 1992 .

[12]  H. Kahle,et al.  GPS and geologic estimates of the tectonic activity in the Marmara Sea region, NW Anatolia , 1997 .

[13]  D. McKenzie Active tectonics of the Alpine—Himalayan belt: the Aegean Sea and surrounding regions , 1978 .

[14]  A. Barka,et al.  Slip distribution along the North Anatolian fault associated with the large earthquakes of the period 1939 to 1967 , 1996, Bulletin of the Seismological Society of America.

[15]  Anderson,et al.  Active faults in the Sea of Marmara, western Turkey, imaged by seismic reflection profiles , 1999 .

[16]  James Jackson,et al.  Faulting associated with historical and recent earthquakes in the Eastern Mediterranean region , 1998 .

[17]  N. Ambraseys,et al.  The saros–marmara earthquake of 9 August 1912 , 1987 .

[18]  Tuncay Taymaz,et al.  High-resolution seismic profiling in the Sea of Marmara (northwest Turkey): Late Quaternary sedimentation and sea-level changes , 1995 .

[19]  A. Barka,et al.  The 17 August 1999 Izmit Earthquake , 1999, Science.

[20]  James H. Dieterich,et al.  Progressive failure on the North Anatolian fault since 1939 by earthquake stress triggering , 1997 .

[21]  Göran Ekström,et al.  Evidence of bias in estimations of earthquake size , 1988, Nature.