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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...

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Библиографические подробности
Опубликовано в: :Sci Rep
Главные авторы: Whitley, Sean, Gertisser, Ralf, Halama, Ralf, Preece, Katie, Troll, Valentin R., Deegan, Frances M.
Формат: Artigo
Язык:Inglês
Опубликовано: Nature Publishing Group UK 2019
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Online-ссылка: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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