16X:

Science (New York, N.Y.)
|July 21, 1972
PubMed
まとめ

アポロ16号のデータを用いた月面の地図作成は,広範囲に広がる高地層の異なる地殻を明らかにしています. 結果は,高原の組成が,アノソシト型ガブロスやフェルドスパト型玄武岩に似ていることを示しており,デカルト遺跡にはこのプレマール地殻が存在することを示唆しています.

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