Fig. 13From: Surface creep rate distribution along the Philippine fault, Leyte Island, and possible repeating of Mw ~ 6.5 earthquakes on an isolated locked patcha Ascending and b descending simulated interferograms corresponding to the estimated fault slip distribution (Fig. 12). Black circle corresponds to the origin (Length = 0) in Fig. 12. Thick and thin green lines correspond to the location of the top and bottom sides of the fault plane, respectively. The small-scale variation of the fringes very close to the fault top is due to imperfectly smooth slip distribution that results from finite spacing of the basis slip functionsBack to article page