Abstract
Modeling suggests that SPA impact-induced melt extraction can strongly lower LREE in the CE-6 mantle source, but additional source heterogeneity or mineralogical controls are required to reproduce the observed MREE-HREE fractionation of CE-6 basalts.
| Original language | English |
|---|---|
| Title of host publication | 57th Lunar and Planetary Science Conference |
| Publication status | Published - Mar 2026 |
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