西藏高原的地质演变
Leigh H Royden1, B Clark Burchfiel, Robert D van der Hilst
1Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 01890, USA. lhroyden@mit.edu
概括
西藏高原是西藏的高原.
科学领域:
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
- 板块构造学板块构造学是什么意思
背景情况:
- 印度与欧亚大陆的碰撞在大约5000万年前开始了西藏高原的形成.
- 在西藏西部和中部发生了地缩,岩层碎片向西太平洋和印度尼西亚挤出.
- 太平洋沟迁移在15-20万年前放缓,影响了碎片挤出.
研究的目的:
- 为了提供一个更广泛的地质背景,西藏高原的进化超越印度-欧亚洲碰撞.
- 研究构造事件与高原结构发展之间的关系.
- 了解推动西藏东部地表升起和地加厚的机制.
主要方法:
- 对地质演变和构造过程的分析.
- 解释地缩和石质层碎片挤出的解释.
- 太平洋沟迁移与高原变形的相关性.
主要成果:
- 撞击后发生了地缩和石质层挤出.
- 太平洋快速沟迁移的停止与挤出速度减缓相吻合.
- 西藏东部的快速地表升起和地加厚是深层地向东流的结果.
结论:
- 西藏高原的演化与印度-欧亚洲碰撞之外的更广泛的构造事件有关.
- 地震道内的深层地流可能推动了西藏东部的升起和加厚.
- 这些过程标志着西藏向适应变形的现代结构系统的过渡.
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