'Slab dehydration peak' presentation slideshows

Slab-mantle decoupling and its implications for subduction zone thermal structure, fluid supply, and geophysical process

Slab-mantle decoupling and its implications for subduction zone thermal structure, fluid supply, and geophysical processes. Ikuko Wada 1,2 and Kelin Wang 1,2 ikukow@uvic.ca and kwang@nrcan.gc.ca 1 School of Earth and Ocean Sciences, University of Victoria, Canada

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