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Kinetic Isotopic Degassing of CO2 During the 2021 Fagradalsfjall Eruption and the δ13C Signature of the Icelandic Mantle

Abstract CO2 is the first volatile to exsolve in magmatic systems and plays a crucial role in driving magma ascent and volcanic eruptions. Carbon stable isotopes serve as valuable tracers for understanding the transfer of CO2 from the melt to the gas phase during passive degassing or active eruption...

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Principais autores: Yves Moussallam, Estelle F. Rose‐Koga, Tobias P. Fischer, Guillaume Georgeais, Hyun Joo Lee, Janine Birnbaum, Melissa A. Pfeffer, Talfan Barnie, Edouard Regis
Formato: Artigo
Idioma:Inglês
Publicado: Wiley 2024-12-01
Series:Geochemistry, Geophysics, Geosystems
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Acceso en liña:https://doi.org/10.1029/2024GC011997
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