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| | Abstract | | To detect temporal change of the crustal structure around Mt. Asama, the seismic interferometry method has been applied to Hi-net data. As the results, phase delay has been detected corresponded with eruptions of Mt. Asama on the auto-correlation function of stations MYT and TUM. The phase delay has been also detected corresponded with eruptions on the cross-correlation function between MYT and TUM. |
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