相关实验视频
Updated: Jul 8, 2026

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Hyperpolarized Xenon for NMR and MRI Applications
Published on: September 6, 2012
流的地幔和虹
1UMR CNRS 5570, Ecole Normale Supérieure et Université de Lyon 1, 69007 Lyon, France. albarede@ens-lyon.fr
概括
原始和太阳可能扩散到地球的地幔中,在耐火岩中形成水库. 这些储库解释了玄武岩中的高同位素比率,挑战了无气化下层地幔模型.
科学领域:
- 地质化学 地质化学
- 地质物理学 地质物理学
- 行星科学 行星科学
背景情况:
- 准则模型假设一个未有气体的下层地幔,但这被海洋岛屿玄武岩中回收材料的证据所挑战.
- 地幔,特别是-3 (3He) 和-4 (4He) 等同位素,很容易通过岩石过程提取,因此在肥沃的地幔岩石中长期保存不太可能.
研究的目的:
- 为地球地幔中原始和太阳的分布提出一个新模型.
- 为了解释不同类型的玄武岩中观察到的同位素比率 (3He/4He) 的变化.
主要方法:
- 这项研究主要是理论性的,提出了基于扩散和岩石特性的地化学模型.
- 它涉及解释现有地化学数据的和同位素在玄武岩.
主要成果:
- 高的3He/4He比率和太阳虹成分归因于从原始材料到耐火地幔岩石 (例如,沙丘岩) 的早期扩散.
- 这些"水库"岩石,作为原始挥发物的沉降池,解释了在海洋岛屿玄武岩和中洋山脊玄武岩中观察到的地化学特征.
- 在化过程中,这些水库的不同挖掘和拉伸导致了不同的同位素比率.
结论:
- 下层地幔可能不均脱气;相反,它含有原始挥发物的储存库.
- 这个模型调和了正规地幔模型和基岩石的地化学观测之间的明显冲突.
- 早期的地球过程,包括挥发性扩散到耐火岩中,在塑造地幔地质化学中起到了至关重要的作用.
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