地融化和大陆由地底层在汇聚边界的地底层抬起
Zhipeng Zhou1,2,3, Hans Thybo4,5,6, Irina M Artemieva7,8,9
1SinoProbe Lab, Chinese Academy of Geological Sciences, 100037, Beijing, China.
Nature communications
|October 19, 2024
概括
东亚纳托利亚高原的东部
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地质化学 地质化学
背景情况:
- 高原上升机制,特别是在西藏和安第斯山脉,与部分融化区域有关.
- 东安纳托利亚高原 (EAP) 具有类似的升起特征,但其深层结构仍然不明.
研究的目的:
- 为了研究东亚纳托利亚高原的深层地质物理结构.
- 了解部分融化和 magma 在高原升起中的作用.
主要方法:
- 构建一个80公里深的地质物理模型,跨越EAP.
- 集成地震接收器功能,重力数据,地震断层扫描,磁电流,地热和地化学模型.
主要成果:
- 在EAP中确定20公里厚的下层地层和10公里厚的中层地层.
- 在这些地层内检测部分融化口袋.
- 在Neo-Tethys板块回滚和断裂后,通过静态平衡来提高EAP的解释.
结论:
- 地的加厚,由融和地底板驱动,对于高原的升起至关重要.
- 这些发现对了解EAP,安第斯山脉和西藏的升起过程有意义.
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