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| | Abstract | | In Takada plain, on the northern coast of central Japan, where there was little information of the seismic velocity structure model, the array measurement of microtremors was carried out, and the S-wave velocity structure models are estimated at four sites. Using the estimated structure models, we calculated synthetic seismograms for M4 class earthquake, which occurred near the 2007 Niigata-ken Chuetsu-oki earthquake. The calculated waveforms show good agreement with observed one for the body wave part. |
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