Replication Data for: Evolution of Impact Basin Gravity Signatures on the Lunar Farside: A long-term Alteration Process

- We determine the size of impactors for 16 lunar far-side basins from models of isostatically compensated gravity data. - We use the elastic thickness of the lithosphere to account for isostatic relaxation of basin formation models. - Isostatic relaxation of lunar farside basins depends on impactor size and formation time and affects the gravity signature of basins.