同位素证据表明Cr分裂成地球核心
Frederic Moynier1, Qing-Zhu Yin, Edwin Schauble
1Department of Geology, University of California at Davis, One Shields Avenue, Davis, CA 95616, USA. moynier@levee.wustl.edu
概括
(Cr) 在地球的化物地幔的耗尽是由于分裂成核心的结果,由光同位素丰富证明. 这种同位素签名是在早期行星积聚和氧化过程中形成的,深处的岩海洋.
科学领域:
- 地质化学 地质化学
- 行星科学 行星科学
- 同位素地球化学 同位素地球化学
背景情况:
- 原始的石 (石) 是理解陆地行星形成的关键.
- 在地球的化地幔中,诸如 (Cr) 等元素的耗尽是有争议的,主要假设是挥发性和核心分割.
研究的目的:
- 为了调查大量酸盐地球中耗尽的原因.
- 确定挥发性或核心分离是否解释了的元素和同位素分布.
主要方法:
- 在各种石中高精度测量 (Cr) 稳定同位素.
- 石同位素组成与大批酸盐地球的比较.
- 一开始的理论计算.
主要成果:
- 石Cr同位素偏离了土壤的大量酸盐值,高达每毫升0.4%.
- 酸盐地球中的Cr耗尽归因于分裂成核心.
- 确定了核心中轻Cr同位素的优先丰富.
结论:
- 地球酸盐部分的 (Cr) 耗尽是由于其优先分离到核心.
- 观察到的同位素特征表明,核心形成发生在岩海洋中部地幔深处.
- 地球的积累和日益增长的氧化作用在确定Cr同位素成分方面发挥了作用.
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