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Earth, Planets and Space
Fig. 5 | Earth, Planets and Space

Fig. 5

From: Simultaneous estimation of the dip angles and slip distribution on the faults of the 2016 Kumamoto earthquake through a weak nonlinear inversion of InSAR data

Fig. 5

Synthetic displacement and residual. a, b Synthetic LOS displacement for the right- (path 135–650; a) and left (path 124–700; b)-looking images, computed from the optimal slip model shown in Fig. 4. c, d Residual LOS displacement for the right- (c) and left (d)-looking images, generated by subtracting the model LOS displacement (a, b) from the observed data (Fig. 2a, b). The red lines with ticks show the model fault traces for the inversion analysis. The thick arrow shows the approximate direction of LOS vectors projected onto the horizontal plane. The thin arrow with a horizontal short line shows the approximate incidence angle. The contour interval in LOS displacement is 10 cm

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