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Updated: Jul 12, 2026

An Experimental Protocol for Studying Mineral Effects on Organic Hydrothermal Transformations
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Published on: August 8, 2018

来自区域化石榴石晶体的热水系统中的运输和动力学限制

B Jamtveit, R L Hervig

    Science (New York, N.Y.)
    |January 28, 1994
    PubMed
    概括

    波斯河奥斯陆裂中的热水流体变化是由石榴石化学揭示的. 氧同位素和微量元素的变化表明,岩石流体的主导地位从岩石流体转变为流星流体,可能与岩石变形有关.

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