Fig. 9From: Surface creep rate distribution along the Philippine fault, Leyte Island, and possible repeating of Mw ~ 6.5 earthquakes on an isolated locked patchCreep rates estimated from the average velocity fields in ascending and descending directions. The dots are the creep rate calculated from the offsets on the two sides across the fault. Lines and error bars show the average and standard deviation, respectively, of the creep rate of neighboring five profilesBack to article page