Slab melting and magma formation beneath the southern Cascade arc
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文摘

δ11B values are consistent with an extensively dehydrated downgoing slab.

Most samples retain primary H2O and Cl contents derived from a hydrous slab component.

Fluids from the mantle portion of the slab cause flux melting of slab top.

Peridotite melting in the sub-arc mantle wedge is driven by hydrous slab melt addition.

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