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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

Magmatic ProcessVolcanologyEngineeringFluid-fluxed MeltingMantle DynamicMagmatismSw JapanHydrous Mantle PlumeGeologyGeochemistryIgneous ProcessPetrologyEarth ScienceMantle GeochemistryTectonics