喜马拉雅"弧"的形状:一个圆被语法冲击滑动断层尖端固定在一起
Liqing Jiao1, Paul Tapponnier2, Aurélie Coudurier-Curveur Mccallum3
1SinoProbe Lab, Chinese Academy of Geological Sciences, Beijing 100037, China.
概括
在喜马拉雅山脉.
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
- 地质测量是指地质测量.
背景情况:
- 印度和亚洲的碰撞推动了喜马拉雅山脉的形成.
- 了解构造变形的区域差异至关重要.
研究的目的:
- 研究喜马拉雅语法对区域构造学和地震活动的影响.
- 为了模拟喜马拉雅山脉生长范围的演变.
主要方法:
- 跨喜马拉雅地质数据的分析.
- 检查表面断层和地震历史.
- 离散元件 范围增长的建模.
主要成果:
- 印度/亚洲汇合的方向是N20°E,但表面断层在语法和尼泊尔之间有很大的差异.
- 与尼泊尔相比,缩短速率和地震回归时间在近语法中明显较低.
- 喜马拉雅山脉的生长表现出圆形模式,受边界冲滑断层的影响.
结论:
- 喜马拉雅语法控制区域构造变形和地震行为.
- 圆范围的增长是由固定的冲击滑动断层驱动的,解释了观察到的推力和地震性的变化.
- 在喜马拉雅山东部和西部频繁发生大地震的预测可能被高估了.
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