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Updated: Jul 5, 2026

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石榴石的-分离:证据表明海洋玄武岩的深源和快速上升

T Z Latourrette, A K Kennedy, G J Wasserburg

    Science (New York, N.Y.)
    |August 6, 1993
    PubMed
    概括

    中洋山脊玄武岩和海洋岛屿玄武岩显示-230过剩,表明地幔深处开始部分融化,特别是在石榴石稳定场. 这一发现需要在海洋山脊下进行动态的融化过程.

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