地球地幔的同位素组成
M Bonifacie1, N Jendrzejewski, P Agrinier
1Equipe de Physico-Chimie des Fluides, Géologiques, Institut de Physique du Globe de Paris (IPGP) and Université Paris, Diderot (UPD), CNRS-INSU-Unité Mixte de Recherche (UMR) 7154, 75251 Paris Cedex 05, France. bonifaci@gps.caltech.edu
概括
大多数海洋岩显示污染,同位素比率 (delta37Cl) 显示海水或盐水的影响. 不被污染的地幔来源的delta37Cl值明显低于地表水库.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 石化学 石化学是一门学科.
背景情况:
- 中洋脊基岩 (MORBs) 中的 (Cl) 稳定同位素组成 (delta37Cl) 提供了对地幔过程的洞察力.
- 了解Cl的来源和循环对于破译地球的挥发性库存至关重要.
研究的目的:
- 为了研究MORBs中Cl含量和delta37Cl之间的关系.
- 为了确定未被污染的MORB源地幔的delta37Cl特征.
- 评估海洋岩中的地污染程度.
主要方法:
- 在22个MORB样本中分析稳定同位素组成 (delta37Cl).
- 德尔塔37Cl值与大量Cl含量的相关性.
主要成果:
- 在MORBs中delta37Cl和Cl含量之间存在正相关性.
- 高达37Cl,富含Cl的玄武岩被富含Cl的物质污染,如海水或盐水.
- 低delta37Cl,Cl贫岩代表了较少受污染的,地幔衍生的岩石.
结论:
- 大多数,如果不是所有的海洋岩都在某种程度上受到污染.
- 在MORB源地幔中,与地表水库 (~0每毫米) 相比,Delta37Cl (~=-1.6每毫米) 的含量明显较低.
- 同位素的差异表明,地球历史上的Cl同位素净分离或晚期的37Cl丰富的挥发性添加.
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