Evaluating seismic hazard and understanding earthquake preparation processes require precise fault slip models which characterize the fault geometry and slip distribution. A precise fault slip model can assist in probing the accumulation and release of stress as well as the frictional behavior on the fault (Caniven et al., 2017;Collettini et al., 2011;Manighetti, 2005). Over the past decades, the temporal and spatial resolutions of the geodetic techniques which measure ground deformation have been significantly advanced. These geodetic techniques include global navigation satellite systems (GNSS), interferometric synthetic aperture radar (InSAR), optical imagery,