Physics
Scientist
Geophysical Institute, Faculty of Science, University of Tokyo, Tokyo, Japan
Department of Earth Science, Kanazawa University, Kanazawa, Japan
Institute for Geoscience, University of Tsukuba, Tsukuba, 305-0006, Ibaragi, Japan
Differences of Cutting Rates among Chondrites and Simulated Planetesimals
Differences of relative strength among chondrites measured by the vibrational fracturing rate
Effects of minor components on the consolidation of planetesimals and chondrites
Electrical conductivity of olivine single crystals at high temperature
Large earthquakes initiate by the acceleration of slips on the downward extensions of seismogenic faults
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