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Progress in Earth and Planetary Science
Fig. 1 | Progress in Earth and Planetary Science

Fig. 1

From: The message of oldhamites from enstatite chondrites

Fig. 1

Rare-Earth Element pattern (in grey) predicted by modeling condensation as monosulfides solid solution in oldhamite [CaS, Lodders and Fegley (1993)]. Conditions are T = 1378.6 K (0.1 K below oldhamite condensation temperature) and a nebular gas with C/O = 1.2 (reduced conditions). Also shown are the CaS/melt REE partition coefficients determined experimentally by Ingrao et al. (2019)

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