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Scientist
Institute of Geology and Geoinformation, National Institute of Advanced Industrial Science and Technology, Tsukuba, Japan
Depth dependent strength of the fault gouge at the Atotsugawa fault, central Japan: A possible mechanism for its creeping motion
Effect of water on weakening preceding rupture of laboratory-scale faults: Implications for long-term weakening of crustal faults
Effects of pressure on pore characteristics and permeability of porous rocks as estimated from seismic wave velocities in cores from TCDP Hole-A
Fault strength drop due to phase transitions in the pore fluid
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