与2019年里奇克雷斯特地震序列附近的断裂相关的表面变形
Xiaohua Xu1, David T Sandwell2, Lauren A Ward3
1Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, USA. xix016@ucsd.edu.
概括
卫星雷达在2019年里奇克雷斯特地震附近发现了数百个新的地断裂. 许多断层显示出意想不到的逆行移位,
科学领域:
- 地质学
- 构造学
- 遥感技术
背景情况:
- 准确的地震危险模型需要了解地应变分布和检测毫米级变形.
- 卫星雷达干扰测量 (InSAR) 对于监测大面积的表面变形至关重要.
研究的目的:
- 分析2019年里奇克雷斯特地震后的地应变模式和断裂行为.
- 调查新发现的骨折中观察到的前进和逆向位移的机制.
主要方法:
- 利用卫星雷达观测识别和绘制线性应变度 (断裂).
- 记录并分析了169个已确定的骨折的移位和宽度.
- 开发了一个物理模型来解释观察到的断裂移位模式.
主要成果:
- 在2019年里奇克雷斯特地震周围确定了数百个以前未被绘制的线性应变度.
- 观察到大多数断层呈现出逐渐的移位,
- 显著数量的断层显示逆行移位, 与普遍的构造压力相反.
结论:
- 这项研究提出了一种模型,解释了在地骨折中观察到的渐进和逆向移位.
- 一个关键的含义是,在众多预先存在的断层上,显著的构造压力被摩擦滑动所适应.
- 这一发现对地震危险建模和理解断层系统行为有重大影响.
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