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Which outcome occurs when a subducting plate becomes increasingly hydrated?

A)Mantle wedge melting is intensified
B)Trench rollback rate decreases sharply
C)Sediment accretionary wedge deforms less
D)Seismic coupling along fault weakens

💡 Explanation

Increased hydration of the subducting slab lowers the melting temperature of the overlying mantle wedge via flux melting, because the addition of water reduces the solidus. Therefore, mantle melting intensifies, rather than trench rollback or accretionary wedge deformation changing.

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