Detailed three-dimensional fault model of the 2022 M(w) 6.6 Luding earthquake reveals seismic hazard potential in the southeastern Tibetan plateau

2022年M(w) 6.6级泸定地震的详细三维断层模型揭示了青藏高原东南部的地震灾害潜力。

阅读:1

Abstract

The detailed 3D fault model and further seismic rupture behavior analysis and fault mechanics simulation based on it are important and meaningful. A strong Mw 6.6 earthquake occurred in Luding, Sichuan, on 5 September 2022, the epicenter was located near the Y-shaped junction of the Xianshuihe Fault Zone (XSHF), the Longmen Shan Fault Zone (LMSF), and the Anninghe Fault Zone (ANHF). To date, a detailed 3D fault model has not been established for this earthquake, preventing a 3D Coulomb stress change (ΔCFS) calculation for further seismic potential analysis. Therefore, first we build a detailed 3D fault model of the earthquake and then we compute ΔCFS in the surrounding areas. Based on 3D modeling technics, we establish a 3D model of the main faults using previously published relocated earthquake catalog and focal mechanism solutions; including the Moxi segment (f(1)) of the XSHF, the Daduhe fault (f(2)) and two previously unknown faults (f(3) and f(4)). The 3D ΔCFS indicates that the strike-slip mainshock of the Luding earthquake significantly triggered two M > 5 dip-slip aftershocks. Moreover, it caused a remarkable increase in ΔCFS and hence a notable enhancement in seismic hazard in the northern ANHF.

特别声明

1、本页面内容包含部分的内容是基于公开信息的合理引用;引用内容仅为补充信息,不代表本站立场。

2、若认为本页面引用内容涉及侵权,请及时与本站联系,我们将第一时间处理。

3、其他媒体/个人如需使用本页面原创内容,需注明“来源:[生知库]”并获得授权;使用引用内容的,需自行联系原作者获得许可。

4、投稿及合作请联系:info@biocloudy.com。