富含REE的性酸盐岩的地幔来源可以通过大陆衍生的沉积物沉降来丰富
Kun-Feng Qiu1, Zheng-Yu Long2, Rolf L Romer3
1State Key Laboratory of Geological Processes and Mineral Resources, Frontiers Science Center for Deep-time Digital Earth, School of Earth Sciences and Resources, China University of Geosciences, Beijing, China. kunfengqiu@qq.com.
Nature communications
|December 17, 2025
概括
稀土元素 (REE) 沉积物源自地幔的丰富,由潜入的大陆沉积物引起. 这一过程在石质层地幔中创造了肥沃的领域,从而形成了富含REE的性岩石.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 经济地质学 地质学
背景情况:
- 性酸盐入侵是稀土元素 (REEs) 的重要来源.
- 负责产生REE丰富的性岩的地幔丰富的起源尚未完全理解.
- 了解这一过程对于定位和开发关键金属资源至关重要.
研究的目的:
- 为了研究性岩的地幔源中的元体丰富过程.
- 为了澄清稀土元素 (REE) 在性酸盐入中的丰富的来源.
- 为了确定沉降材料在产生REE沉积物的作用.
主要方法:
- 从性复合物中分析Li-Ba-Sr-Nd同位素数据.
- 地化学建模以测试不同的地幔丰富场景.
- 专注于中国北方克拉顿的REE矿床.
主要成果:
- 北中国地中的性复合体表现出类似的Li-Ba-Sr-Nd同位素特征.
- 改变的海洋地或蛇形的回收不能解释观察到的同位素特征.
- 要复制地质化学数据,需要对来自大陆的沉积物进行俯冲.
结论:
- 沉降的,经过气候变化的大陆沉积物是REE丰富的性岩地幔丰富的主要来源.
- 这些沉积物降低了岩层地幔的固体,形成了肥沃的领域.
- 大陆沉积物回收是地球关键金属预算的一个关键因素.
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