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地球上的同位素循环.

Morten B Andersen1, Tim Elliott2, Heye Freymuth2

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概括

来自地球表面的回收,被氧化海洋改变,具有明显的同位素特征. 这种污染了上层地幔,影响了中海基岩,但不是海洋岛基岩,表明了更古老的地幔来源.

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科学领域:

  • 地质化学 地质化学
  • 同位素地球化学 同位素地球化学
  • 地球科学 地球科学 地球科学

背景情况:

  • 地球表面的条件对其内部组成有很大影响.
  • 的分布提供了对地球早期历史和地幔过程的洞察.
  • 大气氧气的增加影响了的流动性和运输.

研究的目的:

  • 研究全球循环的同位素特性.
  • 了解缩对地幔构成的影响.
  • 使用同位素来区分地幔来源.

主要方法:

  • 对同位素组成的分析 ((238) U / ((235) U比率).
  • 对中海基岩 (MORBs) 和海洋岛基岩 (OIBs) 的检查.
  • 对同位素数据与OIBs现有的模型年龄进行比较.

主要成果:

  • 由于海洋的氧化变化,缩呈现出高 (238) U/235) U 的比率.
  • MORB显示高 (238) U/(235) U比率,表明上层地幔被回收污染.
  • 与地球大部分相比,OIBs没有显示出明显的同位素组成,这表明地幔来源较旧.

结论:

  • 在过去的6亿年里,回收的已经明显改变了上层地幔.
  • 在OIB中的同位素系统学支持在24亿至18亿年前之间形成地幔储库.
  • 回收的独特同位素特征凸显了它在全球地质化学循环中的重要作用.