Fluid and mass transfer at subduction interfaces—The field metamorphic record
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文摘

Subduction interface exposures show great lithologic and structural heterogeneity.

Fluid and mass transport are focused by deformation at subduction interfaces.

Interface rocks show geochemical evidence of diverse closed- to open-system behavior.

Cycling of H2O and C is affected by metasomatic processes along the interface.

Geochemical processes at subduction interfaces could govern slab signatures in arcs.

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