Fig. 8From: Interseismic crustal deformation in and around the Atotsugawa fault system, central Japan, detected by InSAR and GNSSProfiles of a LOS velocities and b altitudes along AA’ in Fig. 7. Blue line indicates 30 points running average. Green solid and broken lines at ~ 30 km and ~ 21 km along the horizontal axis indicate the location of the Ushikubi and Atotsugawa faults, respectivelyBack to article page