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No significant boron in the hydrated mantle of most subducting slabs
Boron has become the principle proxy for the release of seawater-derived fluids into arc volcanics, linked to cross-arc variations in boron content and isotopic ratio. Because all ocean floor serpentinites so far analysed are strongly enriched in boron, it is generally assumed that if the uppermost...
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| Published in: | Nat Commun |
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| Main Authors: | , , , , , , |
| Format: | Artigo |
| Language: | Inglês |
| Published: |
Nature Publishing Group UK
2018
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| Subjects: | |
| Online Access: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6214984/ https://ncbi.nlm.nih.gov/pubmed/30389930 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-07064-6 |
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