在西藏东部由于构造学和岩石学而导致的地青少年和重制
Tianyu Zheng1,2, Yumei He3,4
1Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences (CAS), Beijing, 100029, China.
Scientific reports
|October 17, 2024
概括
西藏的构造加厚揭示了中层地中低速层和青少年的下层地. 这些结构是由岩石和碰撞形成的,解释了西藏的结构.
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
- 地球科学 地球科学 地球科学
背景情况:
- 西藏地的加厚是印度-欧亚大陆碰撞的直接后果.
- 了解地的细微结构对于破译地生长和再加工的过程至关重要.
研究的目的:
- 构建和分析西藏东部和周边地区的地结构.
- 根据其精细的结构,调查西藏地的起源和演变.
主要方法:
- 采用深度域接收器功能成像来构建地结构.
主要成果:
- 在地中部识别出广泛的低速层.
- 在下层地中观察到交替的高和低速度结构.
- 检测到下层地底部速度的区域变化和地的整体厚度.
结论:
- 提出下层地是未成年,是由大陆碰撞期间的岩石和构造活动形成的.
- 将区域差异归因于构造学位置和参与青少年地形成的独特地材料.
- 暗示中层地中低速层是微大陆组装过程中弧形岩形成的结果.
- 他们得出结论,构造压缩和岩石运动推动了西藏地的幼稚性质和重新加工.
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