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Elsevier, Earth and Planetary Science Letters, 3-4(306), p. 306-308

DOI: 10.1016/j.epsl.2011.04.012

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Comment on ‘Conduit convection, magma mixing, and melt inclusion trends at persistent degassing volcanoes’ by Fred Witham, published in Earth Planetary Science Letters (2011) 301, 345–352

Journal article published in 2011 by N.; Istituto Nazionale di Geofisica e. Vulcanologia Sezione Pisa Pisa Italia Métrich, P.; Institut de Physique du Globe Sorbonne-Paris Cité UMR Cnrs 7154 Univ Paris Diderot Paris France Allard, A.; Istituto Nazionale di Geofisica e. Vulcanologia Sezione Pisa Pisa Italia Bertagnini ORCID, A.; Institut de Physique du Globe Sorbonne-Paris Cité UMR Cnrs 7154 Univ Paris Diderot Paris France Di Muro
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Abstract

We discuss the influence of magma mixing on the CO2-H2O behavior in magmas. ► Witham ‘s model does not fit our melt inclusion data set for Mt Etna and Stromboli. ► Magma fluxing by a deep derived CO2-rich gas better explains the CO2-H2O evolution.