Replication Data for: Numerical investigation of lunar basin formation constrained by gravity signature

• We provide relationships between impactor size, gravity signal and farside basin size as a function of cooling history and formation time; • Gravity anomalies serve as a measure of basin size as impacts altered morphology and crustal thickness models simplify subsurface structure; • Our basin formation models agree with the assumed formation time based on crater chronology and the estimated cooling history of the Moon.