太阳系早期的水活动:来自Orgueil CI石的Sr同位素证据
J D Macdougall1, G W Lugmair, J F Kerridge
1Scripps Institution of Oceanography, University of California, San Diego, La Jolla 92093, USA.
Nature
|January 19, 1984
概括
CI石中的碳酸盐是在太阳系历史早期形成的,在母体形成后不久. 然而,一些硫酸盐似乎更年轻,这表明随着时间的推移,复杂的水性变化过程.
科学领域:
- 太空化学 太空化学
- 行星科学 行星科学
- 石学是指石学,也就是石学.
背景情况:
- CI石是太阳系早期物质的罕见样本.
- 它们含有由水性变化形成的二次矿物质.
- 这种改变的时间以前是未知的.
研究的目的:
- 为了确定CI石中水性变化的时间.
- 为了研究二次矿物阶段的形成.
主要方法:
- 测量了Sr同位素组成和87Rb/86Sr比率.
- 分析了来自Orgueil石的碳酸盐和硫酸盐相.
主要成果:
- 碳酸盐沉积与母体形成同时发生或不久之后发生 (100亿年内).
- 一些硫酸阶段显示出最近形成的证据.
结论:
- 在CI石母体中,早期的水性活动显著.
- 后来的水性事件也发生了,导致硫酸盐的形成.
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