gsminmag Mineralogical Magazine Mineralogical Magazine 0026-461X Mineralogical Society 10.1180/minmag.1987.051.359.16 Mineralogy High-Pressure, Synthetic Loveringite-Davidite and Its Rare Earth Element Geochemistry Green T. H. Pearson N. J. School of Earth Sciences, Macquarie University, North Ryde, NSW 2113, Australia 3 1987 51 359 145 149 27 1 1986 21 4 1986 Copyright © 1987, The Mineralogical Society 1987 Abstract

Loveringite-davidite members of the crichtonite group were synthesized at high pressure and temperature (7.5 kbar, 1000–1050 °C) from a melt of TiO2 and rare earth element (REE) enriched basaltic andesite composition. Four sets of partition coefficients for La, Srn, Ho, Lu and Sr (analogue for Eu2+) were obtained. These show that light and heavy REE are readily accommodated, but the intermediate REE are discriminated against in the loveringite—davidite structure. This confirms the previously proposed two sites (A and M) for REE substitution in the crichtonite group. Additional experiments verified the stability of REE-rich crichtonite group minerals to 20 kbar, 1300 °C and 30 kbar, 1000 °C, and indicate that this phase may be an important accessory repository for the light and heavy REE in the upper mantle.

 Keywords loveringite davidite crichtonite group rare earth element geochemistry