Fig. 6From: Backarc basin oceanic crust and uppermost mantle seismic velocity structure of the Shikoku Basin, south of Japan(a) Observed record section (top) and synthetic seismograms (bottom) for the vertical geophone of OBS063 on SPr10. The position of the OBS is shown by an arrow in Figs. 1 and 3. A gain factor proportional to distance has been used to enhance the distant seismograms. The reduction velocity is 8 km/s. (b) Record section (top) and ray diagram (bottom) for OBS050 on line SPr11. Calculated travel time curves are also plotted on the record section.Back to article page