弧形岩石中的U-Th同位素:从被压缩的地中转移元素的含义
Hawkesworth1, Turner, McDermott
1C. J. Hawkesworth, S. P. Turner, D. W. Peate, and P. van Calsteren are with the Department of Earth Sciences, The Open University, Milton Keynes, MK7 6AA, UK. F. McDermott is with the Department of Geology, University College, Dublin, Eire.
概括
-同位素揭示了从浸层构造板块中流体和沉积物转移的速度. 岛屿弧形火山岩石表明流体调动,而沉积物对弧形岩石中的有显著的贡献.
科学领域:
- 地质化学 地质化学
- 同位素地球化学 同位素地球化学
- 构造学 构造学 构造学 构造学
背景情况:
- 俯冲区对于地球地的回收至关重要.
- 了解从输入板块到地幔的物质转移是解读弧形岩的关键.
- (U) 和 (Th) 的同位素为地质过程提供了强大的标志物.
研究的目的:
- 用岛弧火山岩来研究从下降板块到地幔的流体和沉积物转移速度.
- 量化潜沉积物对弧岩构成的贡献.
- 为了确定流体和沉积物融化运输的时间尺度.
主要方法:
- 在岛屿弧火山岩中分析-Th-Nd同位素系统学.
- 在流体变化过程中利用和的差移动性.
- 解释同位素共变 (例如,Th/Ce与143Nd/144Nd) 以区分来源.
主要成果:
- 在液体中很容易被调动,而的移动性较低.
- Th/Ce和143Nd/144Nd之间的负相关性表明,下降板块的沉积物输入很大.
- 据估计,流体的转移时间为30,000-120,000年,而沉积物融化的转移时间为数百万年.
- 只有大约30%的沉降沉积物回到地.
结论:
- 岛屿弧火山学记录了潜水过程中流体和沉积物回收的复杂相互作用.
- 独特的同位素特征突出显示了流体与沉积物化的不同运输机制.
- 古代地的组成反映了不同的地生成过程,影响了平均U/Th比率.
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