Abstract
Troctolite sample 76535, collected in Serenitatis basin during Apollo 17, formed at least 50 km deep, experienced maximum shock pressures of 6 GPa, and has a 40Ar/39Ar excavation age of 4.25 Ga. Previous work attributed 76535 to the South Pole-Aitken (SPA) basin, presumably dating the SPA-impact and constraining lunar bombardment history. Here we use the iSALE-2D shock-physics code and gravity inversion modeling to determine if instead the Serenitatis impact event excavated 76535. We find nearly 140,000 km3 of material (∼2% of near-surface ejecta) matching the depth and pressure constraints of 76535 is displaced to the surface during crater collapse of a Serenitatis-like impact event. We conclude that the Serenitatis impact event possibly excavated 76535, redefining its age to 4.25 Ga, 300 My older than the consensus age based on Apollo 17 samples. This finding would provide an important anchor point where lunar chronology where bombardment flux is especially uncertain.
| Original language | English (US) |
|---|---|
| Article number | e2025GL116654 |
| Journal | Geophysical Research Letters |
| Volume | 52 |
| Issue number | 18 |
| DOIs | |
| State | Published - Sep 28 2025 |
Keywords
- geophysics
- gravitational analysis
- impact basin
- impact processes
- lunar basins
- lunar chronology
ASJC Scopus subject areas
- Geophysics
- General Earth and Planetary Sciences