CORDIS Project
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This project investigates how interactions between magma and carbonate rocks contribute to carbon dioxide emissions in volcanic regions like Mt. Etna and Popocatépetl. Through hydrothermal experiments and thermal modeling, it aims to quantify CO2 production and understand the mechanisms of gas release.
Mt.
Etna and Popocatépetl, the most important subaerial sources of volcanic CO2 show evidence of interactions with the carbonate rocks forming their sedimentary basement.
The present project aims at quantifying the contribution of magma-carbonate interactions in the upper continental crust to massive CO2 production in these volcanic areas.
Carbonate assimilation will be investigated by hydrothermal experiments and thermal modelling.
The experiments will be performed at magmatic conditions (press…
CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS
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