Connection between high pore-fluid pressure and frictional instability at tsunamigenic plate boundary fault of 2011 Tohoku-Oki earthquake | Scientific Reports - Nature.com
Scientific Reports - Connection between high pore-fluid pressure and frictional instability at tsunamigenic plate boundary fault of 2011 Tohoku-Oki earthquake
Wang, K. & Hu, Y. Accretionary prisms in subduction earthquake cycles: The theory of dynamic Coulomb wedge. J. Geophys. Res.111, B06410 (2006).
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