Does a focal region of shallow slow earthquake become a source area of tsunami? -Approach of geophysical and geological survey for a large historical earthquake-


Yusuke Yamashita, Disaster Prevention Research Institute, Kyoto University, Kyoto, Japan, Yoshihiro Kase, Geological Survey of Hokkaido, Sapporo, Japan and Kei Ioki, AIST - National Institute of Advanced Industrial Science and Technology, Tsukuba, Japan
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