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Publications by [Chigira M.]

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The 2004 Chuetsu earthquake (M 6.8) triggered thousands of landslides in the Miocene to Quaternary sedimentary rocks in Japan. The most common landslides were shallow disrupted landslides on steep slopes without geologic preference, but deep, coherent landslides ...
Reference: The 10th IAEG International Congress, Nottingham, United Kingdom, 6-10 September 2006, Paper number 408