相关实验视频
Updated: Jul 18, 2026

10:42
Preparing an Isotopically Pure 229Th Ion Beam for Studies of 229mTh
Published on: May 3, 2019
在加 - 克拉梅德克岛弧下化的动态推断来自 (231) Pa - 235) U系统学
1Laboratoire de Geochimie et Cosmochimie, Institut de Physique du Globe de Paris-CNRS, UMR7579, 4 Place Jussieu, 75252 Paris Cedex 05, France. Department of Earth Sciences, The Open University, Milton Keynes MK7 6AA, UK.
概括
在加-克尔马德克岩中研究-231与-235的比率,揭示了不同的液体添加和部分化的历史. 加的岩显示了6万年前的流体添加,而克尔马德克的岩表明了过度印制的化效应.
科学领域:
- 地质化学 地质化学
- 同位素地质年代学 同位素地质年代学
- 火山学 火山学是一门学科.
背景情况:
- 加 - 克尔马德克岛屿弧提供了一个自然实验室,用于研究地幔过程.
- 放射性不平衡,例如-231和-235之间的放射性不平衡,为地质事件的时间尺度提供了洞察力.
研究的目的:
- 在加和克拉马德克弧岩中区分流体添加和部分融化的时间和机制.
- 为了利用 (231) Pa-(235) U 不平衡作为地幔源过程的追踪器.
主要方法:
- 测量来自加和克拉马德克弧的岩中的231Pa-235U比率.
- 在俯冲区动态和岩生成的背景下对同位素数据的解释.
主要成果:
- 加岩的231Pa/235U比率低于1,这与大约6万年前从潜水板中添加的液体相一致.
- 克尔马德克岩显示 (231) Pa/235) U比率> 1,表明部分化过程已经覆盖了液体添加的影响.
结论:
- 该 (231) Pa-(235) U系统有效地区分流体主导和融化主导的地幔源在弧度设置中.
- 岛屿弧岩记录了流体岩石相互作用和融化生成的复杂历史,在弧的不同段落有不同的签名.
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