西藏中部地区的兴起和向西扩张
Chenyuan Zhao1,2, Lin Ding1,2, Zhongyu Xiong1
1State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China.
National science review
|April 22, 2025
概括
喜马拉雅-西藏高原 (HTP) 在伊纪显著上升,西藏中央山谷 (CTV) 向西呈现逐步上升. 这种升起是由从东到西的渐进石层层分层驱动的.
科学领域:
- 地质科学 地质科学
- 古生物学的古生物学
- 地质物理学 地质物理学
背景情况:
- 了解喜马拉雅-西藏高原 (HTP) 的代增长对于地力学研究至关重要.
- 高地平原的时空演变,特别是古西藏中藏谷 (CTV),是正在进行的辩论的主题.
研究的目的:
- 重建西藏东部卢龙盆地的升起历史.
- 为了调查古世中藏谷的范围和地形演变.
- 阐明HTP形成背后的地力学机制.
主要方法:
- 放射测量地质年代学
- 对植物组合 (Luolong Flora) 的分析
- 氧气和聚集的同位素古高度测量.
- 古磁力学,磁力学和地震断层扫描.
主要成果:
- 卢龙盆地经历了从0.6公里 (54-46万年前) 到2.9公里 (44万年前) 的提升.
- 纪CTV延伸到西藏东部,东部和西部斜坡较高的山谷底.
- 有证据表明,拉萨地下岩层的东向西分层逐步发生.
结论:
- 该HTP的现代结构是由一个逐步的,东向西的石质层分层过程造成的.
- 龙盆地的升起和CTV向东的延伸为HTP的代增长提供了关键的见解.
- 这些发现有助于理解HTP地区的构造学,地形和气候之间的相互作用.
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