Fig. 14
From: Detection of repeating earthquakes and their application in characterizing slow fault slip
Comparison of InSAR-derived slip rates and repeater-derived slip rates along the Hayward-Calaveras fault zone, California (after Chaussard et al. (2015)). a Repeater slip rates averaged over square patches compared to the modeled slip rates (inverted from InSAR-derived deformation) with same color scale (bottom). b Comparison of repeater slip rates and modeled slip rates both averaged over square patches. The red line shows a 1 to 1 linear regression and the black line shows the best-fit linear regression