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| | Abstract | | An array measurement of earthquakes are conducted in the Wakasa bay area, for estimation deep groud S-wave velocity structure. Array consists of 5 long period seismometers with a station spacing of 2km to 5km. Phase velocities of Rayleigh waves are estimated from semblance analysis. And we estmate the deep ground S-wave velocity structure form surface to about 5km depth. |
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