Overview
- A PNAS study of four tiny basalt fragments from China's Chang'e-6 return finds enrichment in heavier potassium isotopes on the lunar far side compared with near-side basalts.
- The team reports that potassium isotope shifts cannot be explained by normal magmatic processes, pointing to evaporation of lighter isotopes during the basin-forming impact.
- Analyses compared far-side material with Apollo and Chang'e-5 near-side samples, while iron isotope differences appear consistent with magmatic effects.
- Researchers argue that impact-driven volatile loss helps explain the near side's extensive mare volcanism versus the far side's thicker crust and ancient highlands.
- Authors emphasize the conclusions are provisional given the small sample set and call for additional far-side samples to test how widespread the signature is, with potential implications for other rocky worlds shaped by giant collisions.