通过铁石榴石的生长释放氧气 (氧化液体),并在潜水带中循环氧气

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Updated: Jan 15, 2026

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Shuguang Song1, Shiting Ye1, Ming Tang1

  • 1SKLab-DeepMinE, MOEKLab-OBCE, School of Earth and Space Science, Peking University, Beijing 100871, China.

Science bulletin
|October 9, 2025
PubMed
概括

降温区通过在转化过程中释放氧化液体来回收氧气. 这项研究揭示了铁丰富的石榴石在压板块中,为深层地球的氧气循环和大氧气事件提供了洞察力.

关键词:
铁铁格兰尼铁格兰尼.地幔氧化氧化过程氧气循环再循环的方法减少Mn4+) 和Fe3+) 的含量,并释放氧气.潜水区复杂的潜水区.

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