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• W2031506323 abstract "Abstract Mineral physics data related to the deep dehydration of stagnant slabs are summarized. The hydrogen diffusion in minerals of the mantle transition zone is not fast enough to homogenize the transition zone on the geological time scale, and hydrogen is expected to be unevenly distributed there. The hydrous fluid formed in the transition zone tends to percolate into shallower depths to form gravitationally stable hydrous magmas at the base of the upper mantle. We need further studies on the relation of intraplate volcanism above the stagnant slab and deep dehydration, because we expect the geochemical fingerprints of deep dehydration to be quite different from those of shallow dehydration from the subducting slabs." @default.
• W2031506323 created "2016-06-24" @default.
• W2031506323 creator A5006341965 @default.
• W2031506323 creator A5013582768 @default.
• W2031506323 date "2009-12-01" @default.
• W2031506323 modified "2023-09-26" @default.
• W2031506323 title "The role of water in the deep upper mantle and transition zone: dehydration of stagnant slabs and its effects on the big mantle wedge" @default.
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• W2031506323 doi "https://doi.org/10.1016/j.rgg.2009.11.006" @default.
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