Silicate dissolution boosts the CO(2) concentrations in subduction fluids

Estimates of dissolved CO(2) in subduction-zone fluids are based on thermodynamic models, relying on a very sparse experimental data base. Here, we present experimental data at 1–3 GPa, 800 °C, and ∆FMQ ≈ −0.5 for the volatiles and solute contents of graphite-saturated fluids in the systems COH, SiO...

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Detalles Bibliográficos
Autores principales: Tumiati, S., Tiraboschi, C., Sverjensky, D. A., Pettke, T., Recchia, S., Ulmer, P., Miozzi, F., Poli, S.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5606994/
https://www.ncbi.nlm.nih.gov/pubmed/28931819
http://dx.doi.org/10.1038/s41467-017-00562-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5606994/
https://www.ncbi.nlm.nih.gov/pubmed/28931819
http://dx.doi.org/10.1038/s41467-017-00562-z

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