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Slab-derived halogens and noble gases illuminate closed system processes controlling volatile element transport into the mantle wedge
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Halogens and noble gases of mantle peridotites from volcanic fronts are presented.

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Serpentine is a major source of water supplied to the mantle beneath volcanic fronts.

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Sedimentary pore fluids are incorporated into serpentine in a closed system.

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Halogen and noble gas signatures are preserved during subduction processes.

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