Fig. 4From: Earthquake rupture properties of the 2016 Kumamoto earthquake foreshocks (M j 6.5 and M j 6.4) revealed by conventional and multiple-aperture InSAR a LOS displacement field calculated from the constructed distributed slip model. b Residual between the observations (Fig. 2a) and the calculations (a). c, d Same as a, b, respectively, but for MAI results. e Coseismic displacements at GEONET sites. Arrows and bars represent horizontal and vertical displacements, respectively. Black and gray represent the observed and model-predicted displacements, respectively. The vertical component of site 940093, indicated by a white-colored bar, is not used for the modelingBack to article page