238U/235U 在陆地含矿物质中的系统学
Joe Hiess1, Daniel J Condon, Noah McLean
1NERC Isotope Geoscience Laboratory, British Geological Survey, Keyworth, Nottinghamshire, UK. jies@bgs.ac.uk
概括
238/235的比率不是恒定的,这挑战了它在矿物测年过程中的使用. 新的测量揭示了变化,影响了-的地质年代学和我们对地球构成的理解.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 射线测量约会的方法
背景情况:
- 当今的238/235比对-地质年代学和宇宙年代学至关重要.
- 以前假设的137.88的不变比已被用于计算陆地矿物年龄,没有不确定性.
研究的目的:
- 调查陆地矿物中当前的-238/-235比率的变化.
- 评估这种变异性对-地质时代学和宇宙时代学的影响.
主要方法:
- 在58个不同的石质样本中对含矿物进行了高精度的-238/-235比率测量.
- 分析包括一系列矿物类型以捕获同位素变异.
主要成果:
- 在整个样本中观察到238/235值的显著范围超过5每毫升.
- 没有发现与石油遗传,世俗或区域趋势的明确相关性,这表明局部分离.
- 岩石矿物之间的差异表明,238 / 235 分割发生在岩石温度下.
结论:
- 238 / 235的比率是明显变化的,需要在地质计时计算中进行调整.
- 中238/235的平均值为137.818±0.045 (2σ),代表了陆地的同位素组成和可变性.
- 这种观察到的分布在很大程度上代表了平均地和大量地球的-238/-235组成.
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