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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...
Gardado en:
| Publicado en: | Sci Rep |
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| Main Authors: | , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
Nature Publishing Group
2016
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| Assuntos: | |
| Acceso en liña: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4973271/ https://ncbi.nlm.nih.gov/pubmed/27488228 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep30774 |
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