黄同位素证据表明,地幔羽毛中没有来自地球核心的贡献
Anders Scherstén1, Tim Elliott, Chris Hawkesworth
1Department of Earth Sciences, University of Bristol, Will's Memorial Building, Queen's Road, Bristol BS8 1RJ, UK. anders.schersten@bristol.ac.uk
Nature
|January 16, 2004
概括
海洋岛基岩中的同位素不支持核心-地幔混合模型. 这表明回收的海洋地,而不是核心相互作用,解释了这些玄武岩中的同位素异常.
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:
- 海洋岛基岩 (OIBs) 中的同位素比例由两个模型解释:回收海洋地或地球外核相互作用.
- (W) 是一个 siderophile 元素,在地幔中耗尽,对核心贡献敏感.
研究的目的:
- 通过使用同位素,研究OIB源中核心-地幔混合与回收的作用.
- 通过分析夏威夷和南非岩石中的同位素数据来测试核心贡献模型.
主要方法:
- 高精度同位素分析夏威夷和南非岩石样本.
- 同位素数据与现有的同位素数据和地化学模型的比较.
主要成果:
- 在分析的样本中没有观察到负同位素值.
- 没有预测的负同位素值,这与核心-地幔混合模型相矛盾.
结论:
- 一个简单的核心-地幔混合场景被排除为奥斯同位素异常在OIBs的解释.
- 回收海洋地是OIBs来源中更合理的组成部分,解释了观察到的同位素丰富.
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