Devolatilization During Subduction
作者： M.W. Schmidt , S. Poli
DOI: 10.1016/B978-0-08-095975-7.00321-1
关键词: Geophysics 、 Mantle wedge 、 Oceanic crust 、 Petrology 、 Adakite 、 Underplating 、 Continental crust 、 Lithosphere 、 Mantle (geology) 、 Geology 、 Subduction
摘要: Subducted crust refertilizes the subarc mantle wedge as well as the deep convecting mantle. In the subarc region, mass transfer occurs mainly through fluids, melts, or supercritical …
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