Fig. 4: Radial profiles of the surface relief and crust-mantle interface at the end of the simulations.
From: Large impact cratering during lunar magma ocean solidification
Both panels showing for the case where a 25-km thick melt layer is present between the crust and mantle (grey outline) and when the melt layer is absent (purple outline). a impact basins forming by a 60-km diameter projectile, and b impact basins forming by a 120-km diameter projectile.
