Partitioning of F, Cl, and H_2O Between Apatite and a Synthetic Shergottite Liquid (QUE 94201) at 1.0 GPa and 990°-1000°C

Details Partitioning of F, Cl, and H_2O Between Apatite and a Synthetic Shergottite Liquid (QUE 94201) at 1.0 GPa and 990°-1000°C Partitioning of F, Cl, and H_2O Between Apatite and a Synthetic Shergottite Liquid (QUE 94201) at 1.0 GPa and 990°-1000°C

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1247v&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1247

Computer Science

Scientific paper

Apatite/melt partitioning experiments on a QUE 94201 composition were
conducted at 1 GPa and 990°-1000°C in a piston-cylinder
press. The partition coefficients for F, Cl, and H_2O are highly
variable and seem to correlate strongly with melt F content.

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