Fig. 7From: Variations in seismic velocity distribution along the Ryukyu (Nansei-Shoto) Trench subduction zone at the northwestern end of the Philippine Sea plateDepth-converted multichannel seismic section and P-wave velocity model for along-forearc lines. a ECr31, b ECr25. Enlarged seismic reflection images with interpretation for the Kerama Gap and the Miyako Saddle are also shown. The black lines in the interpretation indicate steeply dipping normal faultsBack to article page