Science (New York, N.Y.)
|December 18, 1970
PubMed
まとめ

月の内部は常に熱い状態で,冷たい外層の下の融点に近い状態に留まっています. この熱状態は,長期間の内部熱と一致し,月の地質学に影響を与えます.

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