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在羽毛地幔中保存的高压核心形成的早期事件
Colin R M Jackson1,2, Neil R Bennett1, Zhixue Du1
1Geophysical Laboratory, Carnegie Institution of Washington, Washington DC 20015, USA.
Nature
|January 26, 2018
概括
地球的早期
科学领域:
- 地质化学
- 宇宙化学
- 星球科学
背景情况:
- 在地幔岩石中的 (Xe) 和 (W) 同位素异常为地球的形成提供了洞察力.
- 之前的理论将Xe异常与脱气联系起来, 但无法解释同时发生的W异常或它们的保存.
研究的目的:
- 调查 (I) 和 (Pu) 在核心形成过程中分离的作用,从而产生Xe同位素异常.
- 解释这些异常在地幔中的长期保存.
主要方法:
- 在高压和高温下测量液体铁合金和液体酸盐之间的分离.
- 早期地球核心形成过程的建模.
主要成果:
- 随着压力的增加,变得更具 siderophile (类似铁) 的.
- 高压核心形成事件导致地幔的I/Pu显著耗尽,独立于挥发性.
- 这些被耗尽的地幔部分更密集,有助于它们的保存,并解释了它们在深层地幔储库中的存在.
结论:
- 早期的高压核心形成,不仅仅是脱气,也导致了XE和W同位素异常.
- 这些发现将早期的行星分化与现代地球的可观测的地化学特征联系起来.
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