Crustal CO(2) contribution to subduction zone degassing recorded through calc-silicate xenoliths in arc lavas

Interaction between magma and crustal carbonate at active arc volcanoes has recently been proposed as a source of atmospheric CO(2), in addition to CO(2) released from the mantle and subducted oceanic crust. However, quantitative constraints on efficiency and timing of these processes are poorly est...

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Detalles Bibliográficos
Autores principales: Whitley, Sean, Gertisser, Ralf, Halama, Ralf, Preece, Katie, Troll, Valentin R., Deegan, Frances M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6584678/
https://www.ncbi.nlm.nih.gov/pubmed/31217464
http://dx.doi.org/10.1038/s41598-019-44929-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6584678/
https://www.ncbi.nlm.nih.gov/pubmed/31217464
http://dx.doi.org/10.1038/s41598-019-44929-2

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