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Subduction Zone: The Water Channel to the Mantle
2007Soichi Omori, Tetsuya Komabayashi
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Numerical exploration of the dynamics of the subduction plate boundary channel 
The plate ‘interface’ at subduction zones has often been idealized as a single fault with ‘asperities’, however there is increasing evidence that plate boundary motions typically occur across a ~100-1000m channel or shear zone.Guanzhi Wang +2 more
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Magnesium isotope variation in the subduction channel
Goldschmidt2024 abstractsYongxiang Yao, Yuanyuan Xiao
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