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Updated: Jun 14, 2025

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相关的地和地幔融化文件原始西藏高原生长
Wei Li1,2, Rizheng He3, Xiaohui Yuan2
1School of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China.
National science review
|September 6, 2024
概括
霍西尔盆地 霍西尔盆地
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
- 地震学 地震学
背景情况:
- 在西藏高原北部的霍西尔盆地的快速升起和岩性被争论,特别是地球深层过程和地表海拔变化之间的联系.
- 由于其偏远的位置,Hoh-Xil盆地以前没有被地震网络研究过.
研究的目的:
- 为了研究西藏高原下方的地和上层地幔结构.
- 了解推动西藏高原生长的机制.
主要方法:
- 使用线性地震阵列在霍希尔盆地进行环境噪声断层扫描.
- 开发一个三维S波速度 (VS) 模型.
主要成果:
- 在西藏高原北部发现了一个广泛的部分融的中间地,与南部的孤立口袋形成鲜明对比.
- 最上层地幔的低S波速度异常与地中的异常以及霍希尔盆地暴露的年轻岩石异常存在空间相关性.
结论:
- 西藏高原的增长很可能是由石层地幔的移除驱动的.
- 这一过程助长了岩,导致高原的扩张.
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