Fig. 11
From: Distribution and depth of bottom-simulating reflectors in the Nankai subduction margin
Differences between the BGHS and BSR depths, compiled from 21 seismic profiles (24,329 points). a Differences between the one-dimensional BGHS depths without considering the topographic effect and the BSR depths. The differences range from − 290 to + 200 m. The mean value and the standard deviation are 0 and 63 m, respectively. b Differences between the two-dimensional BGHS depths considering the topographic effect and the BSR depths. The differences range from − 110 to + 140 m. The mean value and the standard deviation are 12 and 38 m, respectively