Partial melting of a depleted peridotite metasomatized by a MORB-derived hydrous silicate melt – Implications for subduction zone magmatism
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DOI: 10.1016/j.gca.2020.09.001
Abstract: Abstract Recent geodynamic models and geothermometers suggest that slabs in intermediate to hot subduction zone cross the water-saturated basalt solidus, indicating that hydrous silicate melts are important agents of mass transfer from slab to mantle… read more here.
Keywords: derived hydrous; fluid; fluid saturated; hydrous silicate ... See more keywords