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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Detalles Bibliográficos
Autores principales: McCaig, Andrew M., Titarenko, Sofya S., Savov, Ivan P., Cliff, Robert A., Banks, David, Boyce, Adrian, Agostini, Samuele
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6214984/
https://www.ncbi.nlm.nih.gov/pubmed/30389930
http://dx.doi.org/10.1038/s41467-018-07064-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6214984/
https://www.ncbi.nlm.nih.gov/pubmed/30389930
http://dx.doi.org/10.1038/s41467-018-07064-6

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