  The North Anatolian Fault (NAF) has produced numerous major earthquakes.
After decades of quiescence, the $\rm{M_w}$ 6.8 Elaz{\i}\u{g} earthquake
(January 24, 2020) has recently reminded us that the East Anatolian Fault (EAF)
is also capable of producing significant earthquakes. To better estimate the
seismic hazard associated with these two faults, we jointly invert
Interferometric Synthetic Aperture Radar (InSAR) and GPS data to image the
spatial distribution of interseismic coupling along the eastern part of both
the North and East Anatolian Faults. We perform the inversion in a Bayesian
framework, enabling to estimate uncertainties on both long-term relative plate
motion and coupling. We find that coupling is high and deep (0-20 km) on the
NAF and heterogeneous and superficial (0-5 km) on the EAF. Our model predicts
that the Elaz{\i}\u{g} earthquake released between 200 and 250 years of
accumulated moment, suggesting a bi-centennial recurrence time.
