铜同位素证据表明硫化物分离和下层地沉积在形成大陆地的过程中
Sheng-Ao Liu1, Roberta L Rudnick2, Wen-Ran Liu1
1State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China.
Science advances
|September 6, 2023
概括
铜在形成过程中被从大陆地中去除,通过硫化物中的轻铜同位素的分离. 这一过程使得大陆地的铜量减少,并且富含更重的同位素.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 同位素地质学的同位素.
背景情况:
- 大陆地的铜 (Cu) 含量相对于其岩源 (弧形岩) 显著减少.
- 在大陆地形成过程中造成这种气体枯竭的机制尚不清楚.
- 了解Cu的去除对于理解地的进化和元素循环至关重要.
研究的目的:
- 阐明了从发展中大陆地中去除铜的过程.
- 为了研究的同位素分离中的潜水区和地内分化的作用.
- 为了确定铜在大陆弧形形成过程中的命运.
主要方法:
- 在各种地质样本中分析铜 (Cu) 同位素组成.
- 调查含量及其与较低地岩中的同位素特征的相关性.
- 在弧形岩石,下层地的岩石积聚物和差异化岩石中检查同位素.
主要成果:
- 降温区过程和地幔融显示在弧形岩石中有限的Cu同位素分离.
- 下层地岩中的异质Cu同位素组成与Cu含量负相关,表明硫化物分离.
- 下层地的岩石堆积物呈现出轻量的Cu同位素组成,而差异化的岩石在Cu同位素中很重.
结论:
- 弧形岩的地内分化导致同位素轻硫化物的分离和积累.
- 硫化物丰富的岩石积聚物的造优先从地中去除轻Cu.
- 这一过程导致大陆地,其铜量减少,并富含更重的Cu同位素.
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