Fig. 10From: Postseismic deformation following the 2016 Kumamoto earthquake detected by ALOS-2/PALSAR-2Quasi east–west and vertical components of average velocity that are derived from ascending and 92 descending interferograms in Fig. 9. Diamond painted in white are reference points (GEONET 960700) for the conversion of LOS displacement. Black and red solid lines are surface trace of active faults and coseismic surface ruptures. Dark green lines delineate boundary of igneous rocks.Arrows with letters are points discussed in the text. See also legend of Fig. 1, 2 and 6Back to article page