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使用 Zn/Fe 系统学的弧的氧化还原状态

Cin-Ty A Lee1, Peter Luffi, Véronique Le Roux

  • 1Department of Earth Sciences, Rice University, Houston, Texas 77005, USA.

Nature
|December 3, 2010
PubMed
概括

原始弧形岩中的与铁的比率 (Zn/Fe(T)) 表明地幔氧化不仅仅是从潜水中产生的. 浅层分化,而不是地幔变化,可能导致弧形岩中较高的氧化状态.

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