Fault locking near Istanbul: indication of earthquake potential from InSAR and GPS observations

A sequence of large earthquakes occurred along the North Anatolian fault in the 20th century. These earthquakes, including the 1999 A degrees zmit/Duzce earthquakes, generally propagated westward towards the Marmara Sea, defining the Main Marmara fault as a potential seismic gap. It is important to conduct a detailed assessment of the seismic hazards along the main Marmara fault because the megacity Istanbul lies only approximately 10 km north of the eastern segment of the Main Marmara fault, which is referred to as the Princes' Islands Fault segment (PIF). Here, we study the locking status of this fault segment to evaluate the seismic hazard potential. For the first time, combined ascending and descending Interferometric Synthetic Aperture Radar and Global Positioning System observations were used to investigate the crustal deformation associated with the PIF. After careful corrections of the estimated ground velocity, a deformation pattern relating to fault locking near the Princes' Islands was identified. The modeling results revealed that the slip rate and locking depth of the fault segment show a clear trade-off, which were estimated as 18.9 +/- A 7.2 mm yr(-1) and 12.1 +/- A 7.0 km, respectively. With a moment accumulation rate of 1.7 +/- A 0.4 x 10(17) Nm yr(-1) (proportional to the product of slip rate and locking depth), our results imply a build-up of a geodetic moment on the PIF and therefore a potential for earthquake hazards in the vicinity of the Istanbul megacity.