Extended Data Fig. 8: Comparison between the original LPR profile and the migration result.
From: Lunar regolith and substructure at Chang’E-4 landing site in South Pole–Aitken basin
a, The original LPR profile; b, The migration result. The data are obtained by the high-frequency Channel-2B. The local details in the rectangles are shown in Extended Data Fig. 9.
