ArticleProceedings of the National Academy of Sciences of the United States of America2026
Isotopic evidence for volatile loss driven by South Pole-Aitken basin-forming impact.
Article in Proceedings of the National Academy of Sciences of the United States of America, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
1 citing paper in PubMed.
- Isotopic evidence for volatile loss driven by South Pole-Aitken basin-forming impact.Proceedings of the National Academy of Sciences of the United States of America · 2026Article
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Authors and funding
10 authors.
Funding
Abstract
Recent studies suggest that the lunar farside experienced a magma ocean evolution similar to that of the nearside. Thus, the nearside-farside dichotomy, such as volcanism and crustal thickness, is likely related to the South Pole-Aitken (SPA) basin-forming impact. Although the noritic clasts found in Chang'e-6 (CE6) samples may originate from crustal remelting induced by the SPA impact, how (and whether) the lunar mantle was modified by this event remains unclear. Here, we present the first high-precision iron (Fe) and potassium (K) isotopic measurements of CE6 low-Ti basalts, revealing higher δ
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