Physics
Scientist
Faculty of Education, Tokyo Gakugei University, 4-1-1 NukuiKita-machi, Koganei City, Tokyo 184-8501, Japan
Faculty of Education, Tokyo Gakugei University, Tokyo, Japan
Clay mineral reactions caused by frictional heating during an earthquake: An example from the Taiwan Chelungpu fault
Ductile fracture of fine-grained plagioclase in the brittle-plastic transition regime: implication for earthquake source nucleation
Earthquakes produce carbon dioxide in crustal faults
Effect of water on weakening preceding rupture of laboratory-scale faults: Implications for long-term weakening of crustal faults
Experimental study in the system albite-andalusite-quartz-NaCl-HCl-H 2 O at 600°C and 400 to 2000 bars
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