Experimental Evidence for High Field Strength Element Incompatibility in Titaniferous Phases in Equilibrium with High Titanium Mare Basalts and Picritic Glass Melts

Details Experimental Evidence for High Field Strength Element Incompatibility in Titaniferous Phases in Equilibrium with High Titanium Mare Basalts and Picritic Glass Melts Experimental Evidence for High Field Strength Element Incompatibility in Titaniferous Phases in Equilibrium with High Titanium Mare Basalts and Picritic Glass Melts

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1956d&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1956

Physics

Scientific paper

We conducted ilmenite-high Ti melt HFSE partitioning experiments at
P-T-X relevant to the lunar mantle. Our Kds are lower than those
previously reported and we demonstrate the dependence of ilmenite-melt
HFSE Kds on the Ti content of picritic melts.

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