Boron isotope fractionation in magma via crustal carbonate dissolution

Carbon dioxide released by arc volcanoes is widely considered to originate from the mantle and from subducted sediments. Fluids released from upper arc carbonates, however, have recently been proposed to help modulate arc CO(2) fluxes. Here we use boron as a tracer, which substitutes for carbon in l...

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Detalles Bibliográficos
Autores principales: Deegan, Frances M., Troll, Valentin R., Whitehouse, Martin J., Jolis, Ester M., Freda, Carmela
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4973271/
https://www.ncbi.nlm.nih.gov/pubmed/27488228
http://dx.doi.org/10.1038/srep30774

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4973271/
https://www.ncbi.nlm.nih.gov/pubmed/27488228
http://dx.doi.org/10.1038/srep30774

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