首次揭开月球背面演化历史

Core Insights - The recent findings from China's Chang'e 6 mission have unveiled significant aspects of the Moon's far side evolution, marking a shift in understanding lunar geology and history [1][2] Group 1: Research Findings - The study reveals two distinct periods of basaltic volcanic activity on the Moon's far side, approximately 4.2 billion and 2.8 billion years ago, indicating sustained volcanic activity [2] - Ancient magnetic field data from the far side suggests that the Moon's magnetic field strength may have increased around 2.8 billion years ago, challenging the notion of a monotonous decline in lunar activity [2] - The water content in the mantle of the Moon's far side is significantly lower than that of the near side, indicating a "bifurcation" in water distribution within the Moon [2] - The basalt samples from the far side originate from a highly depleted source region, which may imply extreme depletion of the primordial lunar mantle or significant impact events that influenced the evolution of the Moon's deep layers [2] Group 2: Implications for Lunar Science - The successful outcomes of the Chang'e program exemplify the deep integration of science and engineering, positioning China to transition from a follower to a leader in planetary science [2]