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Scientists speculate that early in lunar history, when large impactors struck the Moon’s surface, causing millions of cubic kilometers of crustal debris to be ejected, denser material from the Moon’s mantle rose up beneath the impactors almost immediately, compensating for the ejected material and thus leaving no low gravity anomaly in the resulting basin. Later, however, as the Moon grew cooler and less elastic, rebound from large impactors would have been only partial and incomplete. Thus today such gravitational compensation probably would not occur: the outer layer of the Moon is too cold and stiff.
这里意思是说的三个不同时段形成的basin的gravity anomaly不同
early in lunar history会发生compensation-->那时形成的basin就have no low gravity anomaly
Later,(是指later in the lunar history),因为 Moon grew cooler and less elastic-->compensation would be partial and incomplete--》那时形成的basin就有一点gravity anomaly了
today: Moon is too cold and stiff--》compensation probably would not occur--》此时形成的basin最有gravity anomaly
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