The slow slip event cycle along the Izmit segment of the North Anatolian Fault

The occurrence of aseismic creep along seismogenic faults significantly impacts seismic hazard assessment by releasing accumulated stress and reducing the slip deficit. Since the 1999 M w 7.6 Izmit earthquake on the North Anatolian Fault in Türkiye, while aseismic creep has been observed as a postseismic response to the Izmit rupture, additional slow slip events were detected in 2015 and 2016, accommodating several millimeters of relative displacement over periods of approximately one month. By automating Interferometry Synthetic Aperture Radar time series processing from 2016 to 2021 (FLATSIM project) and applying specific post-processing, we extract the tectonic signal to estimate the slip dynamics of the Izmit segment, including the detection and characterization of slow slip events. Modeling the slip distribution at depth on a 2D fault interface within a layered elastic half-space, we estimate a locking depth of 11 k m and steady creep between 2 and 5 k m . Above the steady creep zone, we identify two new shallow slow slip events in March 2018 and November 2019, with moment magnitudes of 4.3 and 4.4, respectively. Based on creepmeter measurements, we estimate a lateral propagation velocity of 6.4 k m / d a y for the 2019 event. The location of these shallow slow slip events above the sedimentary-bedrock interface suggests a critical role of variations in frictional properties in the occurrence of transient slip events. • Aseismic creep along the Izmit segment includes a steady creep from 2 to 5 km -depth, and episodic SSEs at shallower level. • From InSAR time series, we detect three SSEs (December 2016, March 2018, November 2019). • The return period of the SSEs along the segment is quantified to ∼ 1.3 y e a r s . • The moment magnitude of the 2018 and 2019 SSEs is ∼ 4.3 − 4.4 .