Fig. 3From: Geologic evidence for coseismic uplift at ~ AD 400 in coastal lowland deposits on the Shimizu Plain, central JapanProfiles obtained from a ground-penetrating radar survey. The right-hand vertical axis shows two-way travel time (ns) and the left-hand vertical axis shows estimated depth (m) for a given specific inductive capacity (ν; 14.0, 9.0, and 6.0 for profiles A−B, C−D, and E−F, respectively)Back to article page