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Zinc isotope evidence for sulfate-rich fluid transfer across subduction zones
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 o...
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| Veröffentlicht in: | Nat Commun |
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| Hauptverfasser: | , , , , |
| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Nature Publishing Group
2016
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| Schlagworte: | |
| Online Zugang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5171646/ https://ncbi.nlm.nih.gov/pubmed/27982033 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms13794 |
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