The influence of melt composition on the partitioning of REEs, Y, Sc, Zr and Al between forsterite and melt in the system CMAS
Partition coefficients for a range of Rare Earth Elements (REEs), Y, Sc, Al and Zr were determined between forsteritic olivine (nearly end-member Mg2SiO4) and ten melt compositions in the system CaO-MgO-Al2O3-SiO2 (CMAS) at 1 bar and 1400 °C, with concen
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|Source:||Geochimica et Cosmochimica Acta|
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