Science (New York, N.Y.)
|October 29, 1965
PubMed
概括

来自印度洋中部山脊的低托莱伊特基岩与大西洋和太平洋的样本相匹配. 附近的一个海底山产生了不同的托莱伊特基岩,可能表明最近的低谷.

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