Fig. 3From: Surface rupture and characteristics of a fault associated with the 2011 and 2016 earthquakes in the southern Abukuma Mountains, northeastern Japan, triggered by the Tohoku-Oki earthquakeProfiles of LOS surface displacement from the 2016 event determined by differential InSAR analysis; locations are shown in Fig. 2b. a SD (surface displacement), b FD (flexure displacement), and c SD + FD (see text for definitions)Back to article page