印度板块的低角度沉降和东喜马拉雅山脉下方的巨型岩层几何
Ling Bai1,2, Hongru Li1,2, Zhiwen Chen1,2
1State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China.
东喜马拉雅地区的大型地震是由于北南压缩和印度板块轻微的压力造成的. 这就解释了该地区频繁的地震活动和山脉升起.
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:
- 东喜马拉雅山脉经历了频繁的大型地震,原因是活跃的洲际收和罢工滑动.
- 现有的解释不能完全解释冲击滑动,板块收和地震产生之间的相互作用.
研究的目的:
- 调查东喜马拉雅地区聚合板块的区域应力场和结构特征.
- 为该地区频繁发生的地震提供全面的解释.
主要方法:
- 在东喜马拉雅山脉部署新的宽带地震阵列.
- 对地震焦点机制的分析,以确定区域应力场.
- 印度地和板块界面的详细结构分析.
主要成果:
- 区域应力场的特点是主要的北南水平压缩.
- 印度地表现出低角度俯冲,与主要喜马拉雅推力的平坦斜坡几何学.
- 发现了印第安板块轻微推下印度板块的证据.
结论:
- 北南压缩和印度板块的轻微压力解释了东喜马拉雅地区发生的大规模地震.
- 这些机制也解释了该地区观察到的广泛的山脉升起.
- 这些发现为东喜马拉雅山脉的地震危险和构造过程提供了新的视角.
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