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Zinc isotope evidence for sulfate-rich fluid transfer across subduction zones

Author:
Pons, Marie-Laure  Debret, Baptiste  Bouilhol, Pierre  Delacour, Adelie  Williams, Helen  


Journal:
NATURE COMMUNICATIONS


Issue Date:
2016


Abstract(summary):

Subduction zones modulate the chemical evolution of the Earth's mantle. Water and volatile elements in the slab are released as fluids into the mantle wedge and this process is widely considered to result in the oxidation of the sub-arc mantle. However, the chemical composition and speciation of these fluids, which is critical for the mobility of economically important elements, remain poorly constrained. Sulfur has the potential to act both as oxidizing agent and transport medium. Here we use zinc stable isotopes (delta Zn-66) in subducted Alpine serpentinites to decipher the chemical properties of slab-derived fluids. We show that the progressive decrease in delta Zn-66 with metamorphic grade is correlated with a decrease in sulfur content. As existing theoretical work predicts that Zn-SO42- complexes preferentially incorporate heavy delta Zn-66, our results provide strong evidence for the release of oxidized, sulfate-rich, slab serpentinite-derived fluids to the mantle wedge.


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