Comparing the Effects of H2O, F, and Cl on Near-Liquidus Phase Equilibria of a Model High-Fe Basalt: Implications for Volatile Induced Mantle Melting

Details Comparing the Effects of H2O, F, and Cl on Near-Liquidus Phase Equilibria of a Model High-Fe Basalt: Implications for Volatile Induced Mantle Melting Comparing the Effects of H2O, F, and Cl on Near-Liquidus Phase Equilibria of a Model High-Fe Basalt: Implications for Volatile Induced Mantle Melting

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2064f&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2064

Computer Science

Scientific paper

We compare experimental results of a high-Fe basalt composition with
fluorine, and chlorine added independently to the effect of water on
olivine liquidus depression of basalts.

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