Effects of temporal plume-slab interaction on the partial melting of the subducted oceanic crust
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文摘
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Plume–slab interaction in the subduction zones is quantitatively evaluated using numerical modeling experiments.

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Injection of a plume blob into the mantle wedge increases the slab surface temperature resulting in adakites.

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Increases in duration and thickness of the plume blob systematically contribute to slab surface temperatures.

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Subduction parameters for slab melting are suggested for first-order analysis of the plume–slab interaction.

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