1. Experimentally determined trace element partition coefficients between hibonite, melilite, spinel, and silicate melts
- Author
-
Arno Rohrbach, Stephan Klemme, Jasper Berndt, and D. C. Loroch
- Subjects
Multidisciplinary ,Materials science ,Mineral ,010504 meteorology & atmospheric sciences ,Spinel ,Trace element ,Analytical chemistry ,Melilite ,engineering.material ,lcsh:Computer applications to medicine. Medical informatics ,010502 geochemistry & geophysics ,01 natural sciences ,Silicate ,chemistry.chemical_compound ,chemistry ,Meteorite ,Chondrite ,engineering ,lcsh:R858-859.7 ,Hibonite ,Earth and Planetary Science ,lcsh:Science (General) ,lcsh:Q1-390 ,0105 earth and related environmental sciences - Abstract
This article provides new data on mineral/melt partitioning in systems relevant to the evolution of chondrites, Calcium Aluminum-Rich Inclusions (CAI) in chondrites and related meteorites. The data set includes experimentally determined mineral/melt partition coefficients between hibonite (CaAl12O19), melilite (Ca2(Al,Mg)2SiO7), spinel (MgAl2O4) and silicate melts for a wide range of trace elements: Sc, Ti, V, Cr, Co, Ni, Cu, Zn, Ga, Ge, Rb, Sr, Y, Zr, Nb, Rh, Cs, Ba, La, Ce, r, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu, Hf, Ta, W, Pb, Th and U. The experiments were performed at high temperatures (1350 °C < T < 1550 °C) and ambient pressure. The experimental run products were analyzed using electron microprobe (EMPA) and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). The partition coefficients for 38 trace elements were calculated from the LA-ICP-MS data.
- Published
- 2018