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Titanium-rich basaltic melts on the Moon modulated by reactive flow processes

Klaver, Martijn, Klemme, Stephan, Liu, Xiao-Ning, Hin, Remco C., Coath, Christopher D., Anand, Mahesh, Lissenberg, C.Johan ORCID:, Berndt, Jasper and Elliott, Tim 2024. Titanium-rich basaltic melts on the Moon modulated by reactive flow processes. Nature Geoscience 17 , pp. 118-123. 10.1038/s41561-023-01362-5

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The origin of titanium-rich basaltic magmatism on the Moon remains enigmatic. Ilmenite-bearing cumulates in the lunar mantle are often credited as the source, but their partial melts are not a compositional match and are too dense to enable eruption. Here we use petrological reaction experiments to show that partial melts of ilmenite-bearing cumulates react with olivine and orthopyroxene in the lunar mantle, shifting the melt composition to that of the high-Ti suite. New high-precision Mg isotope data confirm that high-Ti basalts have variable and isotopically light Mg isotope compositions that are inconsistent with equilibrium partial melting. We employ a diffusion model to demonstrate that kinetic isotope fractionation during reactive flow of partial melts derived from ilmenite-bearing cumulates can explain these anomalously light Mg isotope compositions, as well as the isotope composition of other elements such as Fe, Ca and Ti. Although this model does not fully replicate lunar melt–solid interaction, we suggest that titanium-rich magmas erupted on the surface of the Moon can be derived through partial melting of ilmenite-bearing cumulates, but melts undergo extensive modification of their elemental and isotopic composition through reactive flow in the lunar mantle. Reactive flow may therefore be the critical process that decreases melt density and allows high-Ti melts to erupt on the lunar surface.

Item Type: Article
Date Type: Publication
Status: Published
Schools: Earth and Environmental Sciences
Publisher: Springer Nature
ISSN: 17520894
Date of First Compliant Deposit: 1 February 2024
Date of Acceptance: 14 December 2023
Last Modified: 18 Mar 2024 12:12

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