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| Abstract | In this study, the Microtremor Survey was always inquired into after the geographical features geological features were examined enough, and the best surface velocity structure model from a peripheral basic structure to the surface was examined in a Tsukuba area. The microtremor measurement was executed about 200 points over around the Tsukuba Area. It was possible to explain, and a detailed speed structural model was able to be made about the excellence cycle about the Tsukuba Area. A detailed earthquake movement will be calculated by using this speed structural model in the future. The most appropriate amplitude will be calculated. |
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