“…Interferometric Synthetic Aperture Radar (InSAR) time‐series analysis is a well‐established technique for measuring ground deformation at the level of millimeters per year (Morishita et al., 2020), with spatial resolutions in the tens of meters, providing spatially continuous observations over hundreds of kilometres that are useful for regional continental tectonic studies (Elliott et al., 2016). Iran has been the focus of numerous InSAR‐based studies over the past 20 years, capturing deformation from groundwater extraction (Babaee et al., 2020; Ghorbani et al., 2022; Haghshenas Haghighi & Motagh, 2021; Motagh et al., 2017), active salt diaprism (Barnhart & Lohman, 2012; Roosta et al., 2019), and co‐ and postseismic deformation (Liu et al., 2021; Penney et al., 2015; Plattner et al., 2022). Regarding interseismic strain accumulation, a common target of InSAR analysis due to the small magnitude of the signal and the implications for seismic hazard, previous Iran InSAR studies have focused on individual fault structures such as the Main Kopet Dagh Fault (Dodds et al., 2022; Walters et al, 2013), the Main Recent Fault (Watson et al., 2022), the North Tabriz Fault (Aghajany et al., 2017; Karimzadeh et al., 2013; Rizza et al., 2013), and the Doruneh Fault (Pezzo et al., 2012).…”