在地球上层地幔中,Re-Os同位素证明了长期存在的异质性和平衡过程
Anders Meibom1, Norman H Sleep, C Page Chamberlain
1Geological and Environmental Sciences, 320 Lomita Mall, Stanford University, California 94305, USA. meibom@pangea.stanford.edu
Nature
|October 18, 2002
概括
地球的上层地幔是高度异质的,这是由于数十亿年的炼和地回收. - (Re-Os) 同位素数据揭示了一个
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
- 石化学 石化学是一门学科.
背景情况:
- 地球上层地幔的组成反映了数十亿年的地质过程.
- - (Re-Os) 同位素系统对融提取和地回收利用非常敏感.
研究的目的:
- 研究上层地幔的地化学异质性.
- 使用Re-Os同位素进行微量化提取和地物质回收.
主要方法:
- 分析了超过700种富含的金组元素合金中的同位素组成.
- 利用Re-Os同位素系统学来评估地幔演变.
主要成果:
- 奥斯同位素数据显示出广泛的高斯分布,表明极端的上层地幔异质性.
- 枯竭和丰富的地幔领域可以保持数十亿年的不平衡.
结论:
- 高度的部分融化,如中洋山脊的部分融化,是有效的Re-Os平衡所必需的.
- 高斯的同位素分布表明了"梅花布丁"地幔混合过程,而不是离散的融化枯竭事件.
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