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70826 Creator 1c5c32b11b5ad1bd9c846a77784abc38
70826 Creator 5a9f28970e2d0d0ba76f7ab60ee890ba
70826 Creator ext-149f0da76580f36a1e4df965dbeff6dc
70826 Creator ext-1822531c77c078556b6960810bb19cec
70826 Creator ext-4df4437d65a8a1e2c1da330c3bdcb605
70826 Creator ext-55f46aa1585adc858325dde6e7dda60d
70826 Creator ext-8650d4dd422516e563c44c7acf2a7ab9
70826 Creator ext-99046648ece243d33fbe658917b9bf45
70826 Creator ext-a4221ac37dd54aec040160d3df9137e4
70826 Date 2020
70826 Is Part Of repository
70826 Is Part Of p23973366
70826 abstract Accurately constraining the formation and evolution of the lunar magnesian suite is key to understanding the earliest periods of magmatic crustal building that followed accretion and primordial differentiation of the Moon. However, the origin and evolution of these unique rocks is highly debated. Here, we report on the microstructural characterization of a large (~250-μm) baddeleyite (monoclinic-ZrO<sub>2</sub>) grain in Apollo troctolite 76535 that preserves quantifiable crystallographic relationships indicative of reversion from a precursor cubic-ZrO<sub>2</sub> phase. This observation places important constraints on the formation temperature of the grain (>2,300 °C), which endogenic processes alone fail to reconcile. We conclude that the troctolite crystallized directly from a large, differentiated impact melt sheet 4,328 ± 8 Myr ago. These results suggest that impact bombardment would have played a critical role in the evolution of the earliest planetary crusts.
70826 authorList authors
70826 status peerReviewed
70826 type AcademicArticle
70826 type Article
70826 label White, L.F.; Cernok, A. ; Darling, J.R.; Whitehouse, M.J.; Joy, K.H.; Cayron, C.; Dunlop, J.; Tait, K.T. and Anand, M. (2020). Evidence of extensive lunar crust formation in impact melt sheets 4,330 Myr ago. Nature Astronomy (Early Access).
70826 Title Evidence of extensive lunar crust formation in impact melt sheets 4,330 Myr ago
70826 in dataset oro