Fluid-fluxed melting of mantle versus decompression melting of hydrous mantle plume as the cause of intraplate magmatism over a stagnant slab: Implications from Fukue Volcano Group, SW Japan
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DOI: 10.1016/j.lithos.2017.02.011
Abstract: Abstract The Pacific Plate subducting from the Japan Trench has accumulated in the mantle transition zone beneath NE Asia, and intraplate magmatism has been active above the stagnant Pacific slab. To understand the origin of… read more here.
Keywords: intraplate magmatism; hydrous mantle; mantle transition; slab ... See more keywords