| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5782932 | Chemical Geology | 2017 | 43 Pages |
Abstract
The behavior of argon in H2O-CO2 bearing basaltic melts was experimentally investigated in the pressure range 1-5 GPa 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 ascent and degassing. The experimental results show several features:
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Authors
A. Fabbrizio, M.A. Bouhifd, D. Andrault, N. Bolfan-Casanova, G. Manthilake, D. Laporte,