Spatial variations in antigorite fabric across a serpentinite subduction channel : Insights from the Ohmachi Seamount, Izu-Bonin frontal arc
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- 2010-10-15
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関連論文
- Spatial variations in antigorite fabric across a serpentinite subduction channel : Insights from the Ohmachi Seamount, Izu-Bonin frontal arc
- Trench-parallel anisotropy produced by serpentine deformation in the hydrated mantle wedge