Extended Data Fig. 3: Comparison of the surface material of the N-WR and the L basalts.
From: Landing site of the Chang’e-6 lunar farside sample return mission from the Apollo basin
The yellow dashed line marks the extent of the wrinkle ridge. The N-WR surface is generally consistent with the color hue of the L region in the Clementine false-color composite image, the LROC WAC normalized three-band color map, the M3 data, and the titanium and iron map, respectively.
