地球的收缩和其核心的分离
Bernard J Wood1, Michael J Walter, Jonathan Wade
1Macquarie University, Department of Earth and Planetary Sciences, North Ryde, New South Wales 2109, Australia. bwood@els.mq.edu.au
地球 地球 地球 地球 地球 地球
科学领域:
- 行星科学 行星科学
- 地质化学 地质化学
- 地球科学 地球科学 地球科学
背景情况:
- 地球是从行星类物质形成的,长达3千4千万年.
- 行星小核心含有金属铁,影响了地球核心的组成.
- 地幔的组成表明,在地球的增长过程中,深层岩海洋重新平衡.
研究的目的:
- 为了研究地球积累过程中的核心形成过程.
- 了解核心和地幔之间 siderophile 元素的重新平衡.
- 为了确定高压条件对地球核心组成的影响.
主要方法:
- 对当前地幔构成的分析.
- 核心-地幔分化的建模.
- 对 siderophile 元素分离的地球化学研究.
主要成果:
- 核心-地幔再平衡发生在一个深的岩海洋 (>400公里).
- 随着地球的生长,氧化条件随着时间的推移而增加.
- 地球的核心含有更多的低原子数元素 (例如,,氧),而不是小行星核心.
结论:
- 地球的核心形成涉及高压下重要的金属酸盐再平衡.
- 岩海洋阶段对于建立当今核心和地幔组成至关重要.
- 积聚过程和高压形成了一个独特的,富含轻元素的地球核心.
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