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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...
Tallennettuna:
| Julkaisussa: | Sci Rep |
|---|---|
| Päätekijät: | , , , , , |
| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
Nature Publishing Group UK
2019
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| Aiheet: | |
| Linkit: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6584678/ https://ncbi.nlm.nih.gov/pubmed/31217464 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-019-44929-2 |
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