Science (New York, N.Y.)
|January 30, 1970
PubMed
概括

月球上的异构岩石与海岩石不同,表明高地起源于撞击喷射物. 一个拟议的模型在gabbro上面呈现一个anorthosite地,玛丽亚由岩通过地裂隙上升而形成.

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