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Abstract Impact and space weathering play a key role in resurfacing the Moon, yet their effects on the lunar farside remain poorly constrained. Chang’e-6 (CE-6) samples provide a unique opportunity to understand space weathering and material redistributions within the South Pole-Aitken (SPA) Basin. Our combined cosmogenic Sm, Hf, and Cr isotope results indicate an average cosmic-ray exposure (CRE) age of ~500 Ma for the CE-6 soil.
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