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 , in addition to CO released from the mantle and subducted oceanic crust. However, quantitative constraints on efficiency and timing of these processes are poorly establis...

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Veröffentlicht in:	Scientific reports 2019-06, Vol.9 (1), p.8803
Hauptverfasser:	Whitley, Sean, Gertisser, Ralf, Halama, Ralf, Preece, Katie, Troll, Valentin R, Deegan, Frances M
Format:	Artikel
Sprache:	eng
Online-Zugang:	Volltext
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