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| Abstract | We considered the period and amplifying characteristic for advance of the subsurface structure from the seismic bedrock to the ground surface (Senna et al.,2013). In this research, a microtremor observation was performed in low land and the plateau part in Akita and Yamagata area. We conducted a lot of microtremor observations in this area in the past. Because there is very little borehole data in this area. Microtremor data used a 'Microtremor database' of NIED. Microtremor data interpreted data by CCA method analysis as well as an array analysis by SPAC method. Underground structure model was reorganized using those data. |
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