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On August 17<sup>th</sup> 1999, a M<sub>w</sub> 7.4 earthquake struck the city of Izmit in the north-west of Turkey. This event was one of the most\uddevastating earthquakes of the twentieth century. The epicentre of the Izmit earthquake was on the North Anatolian Fault (NAF)\udwhich is one of the most active right-lateral strike-slip faults on earth. However, this earthquake offers an opportunity to study how\udstrain is accommodated in an inter-segment region of a large strike slip fault. In order to determine the Izmit earthquake post-seismic\udeffects, the authors modelled Coulomb stress changes of the aftershocks, as well as using the deformation measurement techniques of\udInterferometric Synthetic Aperture Radar (InSAR) and Global Navigation Satellite System (GNSS). The authors have shown that\udInSAR and GNSS observations over a time period of three months after the earthquake combined with Coulomb Stress Change\udModelling can explain the fault zone expansion, as well as the deformation of the northern region of the NAF. It was also found that\udthere is a strong agreement between the InSAR and GNSS results for the post-seismic phases of investigation, with differences less\udthan 2mm, and the standard deviation of the differences is less than 1mm

the international archives of the photogrammetry, remote sensing and spatial information sciences/international archives of the photogrammetry, remote sensing and spatial information sciences

ANALYSING POST-SEISMIC DEFORMATION OF IZMIT EARTHQUAKE WITH INSAR, GNSS AND COULOMB STRESS MODELLING