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So Ozawa
University of TokyoMeeting roles in:
The gap between the seismogenic zone and Episodic Tremor and Slip explained by fluid flow and permeability structures around the mantle wedge corner
3D frictional and viscous earthquake cycle model of the Cascadia subduction zone
Simulating Injection-Induced Seismicity in Enhanced Geothermal Systems Using Models of Fluid-Induced Seismic Slip with Permeability Enhancement and Rate-and-State Friction
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