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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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Detalhes bibliográficos
Publicado no:Nat Commun
Main Authors: McCaig, Andrew M., Titarenko, Sofya S., Savov, Ivan P., Cliff, Robert A., Banks, David, Boyce, Adrian, Agostini, Samuele
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2018
Assuntos:
Acesso em linha: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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