Science (New York, N.Y.)
|November 1, 1963
PubMed
概括

硫化晶体显示,在生长过程中,同位素比率发生变化,这表明矿石流体成分随着时间的推移而发生变化. 这一发现提供了关于密西西比河谷类型-沉积物的形成的见解.

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