mantle chemical evolution
mantle chemical evolution
地幔化学演化
以上为机器翻译结果，长、整句建议使用 人工翻译 。
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Mafic igneous rock, a widely distributed and typical mantle-derived rock, has become a major research source for revealing possible mechanisms for the chemical evolution of the mantle.
镁铁质火成岩作为分布最为广泛的典型幔源岩石，已成为探索地幔化学性状及示踪岩石圈深部过程的主要研究对象。
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