Fig. 12From: Seismic structure of rifting in the Okinawa Trough, an active backarc basin of the Ryukyu (Nansei-Shoto) island arc–trench systemMCS depth-converted profile (top left), Vp model (middle left), and checkerboard test result with ray coverage (bottom left) for ECr21. The time sections for the three sedimentary basins in the top-left depth section are enlarged and displayed on the right. The black lines in the time sections indicate steeply dipping normal faultsBack to article page