Overview
- The Chinese Academy of Sciences team led by Heng‑Ci Tian reports the results in PNAS using Chang'e‑6 samples from the South Pole–Aitken basin.
- High‑precision measurements find enrichment in heavier potassium isotopes, with iron only slightly heavier, relative to Apollo and Chang'e‑5 near‑side basalts.
- The isotopic pattern is inconsistent with ordinary magmatic processes and is interpreted as evaporation-driven volatile loss from a deep, extremely hot impact.
- The study proposes that the event pushed heat‑producing elements toward the near side, fostering widespread mare volcanism, while the far side remained more depleted.
- The conclusions are based on four tiny basalt fragments, so researchers emphasize the need for more far‑side samples to test how broadly this signature occurs.