Science (New York, N.Y.)
|December 1, 1967
PubMed
まとめ

月の土壌の分析は,0.35-0.45の多孔性と高い内部摩擦を示しています. これらの発見は,月面が超基礎隕石ではなく,酸性岩や玄武岩で構成されていることを示唆しています.

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