2016年和2022年门地震的源模型及其构造影响由InSAR揭示
Xixuan Bai1, Bingqiang Zhang1, Aizhi Guo2
1School of Civil Engineering and Architecture, Wuhan Institute of Technology, 693 Xiongchu Avenue, Wuhan 430074, China.
使用Sentinel-1A SAR数据调查2022年门地震,发现它与2016年地震有关. 这种地震活动可能加速了应力释放和西藏高原向东扩张.
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
- 遥感 遥感 遥感 遥感
背景情况:
- 海断层系统适应了西藏高原向东的扩张.
- 有限的地质测量数据阻碍了对区域构造学的理解.
研究的目的:
- 调查2022年6.7兆瓦和2016年5.9兆瓦的门元地震. 调查2022年6.7兆瓦和2016年5.9兆瓦的门元地震.
- 使用InSAR.分析故障几何和源模型.
主要方法:
- 使用 Sentinel-1A SAR图像进行地震分析.
- 应用大气误差校正,以提高InSAR数据的准确性.
- 开发了地震事件的源模型.
主要成果:
- 改善了InSAR对2016年地震的重震变形的准确性.
- 2016年事件的库伦压力可能促进了Lenglongling断层的罢工滑动.
- 2022年地震的断层可能将Lenglongling和Tuolaishan断层连接起来.
结论:
- 2022年地震的破裂可能将西部的Lenglongling断层与东部的Tuolaishan断层联系起来.
- 这一事件可能引发了深层次的余震,并加速了压力释放.
- 这种地震活动有助于理解西藏高原构造学.
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