Dip distribution of Oita–Kumamoto Tectonic Line located in central Kyushu, Japan, estimated by eigenvectors of gravity gradient tensor

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作者
Shigekazu Kusumoto
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[1] University of Toyama,Graduate School of Science and Engineering for Research (Science)
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Dip distribution; Oita–Kumamoto Tectonic Line; Kumamoto earthquake; Gravity gradient tensor; Eigenvector; Futagawa fault system; Aso caldera; Hohi volcanic zone;
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