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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...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
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| Materias: | |
| 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 |