Fig. 11From: Visualization of attenuation structure and faults in incoming oceanic crust of the Nankai Trough using seismic attenuation profilingActivity of faults bounding the sag pond based on Ike et al. (2008). Although present activity of the sag pond was not mentioned by Ike et al. (2008), the depressed seafloor topography implies that the faults are presently activeBack to article page