Fig. 4From: Determination of the dipping direction of a blind reverse fault from InSAR: case study on the 2017 Sefid Sang earthquake, northeastern IranSubsampled data points from the atmospheric corrected InSAR data that were used in the inversions, shown in kilometric Cartesian coordinates. a, b ALOS-2 ascending and descending subsampled data points, respectively. c, d Sentinel-1A ascending and descending subsampled data points, respectivelyBack to article page