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Metamorphic devolatilization of subducted marine sediments and the transport of volatiles into the Earth's mantle
Volatiles, most notably CO(2), are recycled back into the Earth's interior at subduction zones(1,2). The amount of CO(2) emitted from arc volcanism appears to be less than that subducted, which implies that a significant amount of CO(2) either is released before reaching the depth at which arc...
Autores principales: | , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Nature Publishing Group UK
2001
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8127824/ https://www.ncbi.nlm.nih.gov/pubmed/11357128 http://dx.doi.org/10.1038/35077056 |