Argon behavior in basaltic melts in presence of a mixed H2O-CO2 fluid at upper mantle conditions

The behavior of argon in H2O-CO2 bearing basaltic melts was experimentally investigated in the pressure range 1–5GPa and at temperatures between 1350 and 1600°C. Our experimental data simulate the partitioning of argon between an Ar-H2O-CO2 bearing fluid and a silicate melt occurring during magma as...

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Veröffentlicht in:	Chemical geology 2017-01, Vol.448, p.100-109
Hauptverfasser:	Fabbrizio, A., Bouhifd, M.A., Andrault, D., Bolfan-Casanova, N., Manthilake, G., Laporte, D.
Format:	Artikel
Sprache:	eng
Schlagworte:	Argon Basalt Bearing Carbon dioxide Earth Sciences Fluid phase Mathematical models Melts Partitioning Petrography Sciences of the Universe Silicate melt Silicates Solubility
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