Core Insights - The latest findings from the Chang'e 6 lunar mission reveal that the crystallization temperature of basalt on the far side of the moon, as well as the potential temperature of the lunar mantle, are lower than those on the near side, indicating that the far side's mantle is comparatively "cooler" [1][2] Group 1: Scientific Findings - The research provides geological and geochemical evidence for the temperature differences between the lunar mantle of the near side and the far side [2] - Understanding the internal characteristics of the moon, such as the mantle, is crucial for studying lunar evolution, as ancient volcanic activity on the moon was driven by material from the mantle [1]