Fig. 4

CI-normalized REE plot of zirconolites in the granophyric clast from the lunar meteorite DEW 12007. The Eu content is below the detection limit after the interference correction. The REE pattern of the zirconolite, characterized by HREE-rich and flat HREE in this study, is similar to that of lunar granite zirconolite (Seddio et al. 2013) but different from a concave shape of the mare basalt zirconolite (Rasmussen et al. 2008). The Eu depletion in the zirconolite explains its late crystallization after plagioclase