同位素对地幔,地和碳酸的同质性
Z D Sharp1, J D Barnes, A J Brearley
1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA. zsharp@unm.edu
Nature
|April 27, 2007
概括
地球的同位素比率在石,地幔和地中是一致的,这挑战了以前关于不同太阳星云储存和行星分化的理论. 这一发现简化了我们对的起源和分布的理解.
科学领域:
- 地质化学 地质化学
- 太空化学 太空化学
- 同位素地质学的同位素.
背景情况:
- 与太阳和石丰富相比,地球上 (Cl) 的含量显著减少.
- 了解Cl分布和同位素比率是解释这些耗尽和地球挥发性库存的关键.
- 之前的研究表明,在不同的行星储库中,同位素的比例不同.
研究的目的:
- 为了研究地球地幔,地和石中稳定的同位素比率 (37Cl/35Cl).
- 为了确定在地沉积物中是否存在与地质年龄相关的同位素变异.
- 重新评估地球形成,分化和挥发性积累的模型.
主要方法:
- 使用质谱学高精度测量稳定的同位素比率 (delta37Cl).
- 对各种地质样本的分析,包括地幔外石,地岩,不同年龄的沉积物和碳酸.
主要成果:
- 在碳酸,地幔和地之间的37Cl/35Cl比率中没有发现显著差异.
- 对古代至最近地沉积物的分析显示,与地质年龄没有系统的同位素变化.
- 在地球历史上,地幔和地的delta37Cl值一直保持不变.
结论:
- 缺少同位素变异驳斥了对的同位素上不同的星云储存库的存在.
- 在地球的分化过程中 (包括核心形成) 的同位素分化对于来说是可以忽略的.
- 在地球地中没有显著的晚期添加同位素独特的含挥发物.
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