Zinc isotope evidence for sulfate-rich fluid transfer across subduction zones
During subduction, fluids are released into the mantle wedge, but the exact compositions of these fluids are unclear. Ponset al. by analysing zinc isotopes from serpentinite provide evidence that oxidized, sulphate rich fluids are released to the mantle wedge during subduction.
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| Autores principales: | , , , , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2016
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/38de2e76ca334534827957a1463b6f4f |
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