Evidence for semi-brittle flow in mantle-wedge serpentinites linked to high pore fluid pressure

Ken-ichi Hirauchi1, Ryosuke Oyanagi2, Atsushi Okamoto3, Yurina Nagata1 and Katsuyoshi Michibayashi4, (1)Shizuoka University, Shizuoka, Japan, (2)JAMSTEC Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan, (3)Tohoku University, Graduate School of Environmental Sciences, Sendai, Japan, (4)Nagoya University, Nagoya, Japan