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

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<sub>1</sub>) of the XSHF, the Daduhe fault (f<sub>2</sub>) and two previously unknown faults (f<sub>3</sub> and f<sub>4</sub>). 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.

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Publication Details

Journal
Scientific Reports
Published
2025-07-16
DOI
https://doi.org/10.1038/s41598-025-11553-2
Primary Topic
earthquake and tectonic studies
Type
article
Field-Weighted Citation Impact
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article

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

Xuhang Yang, Guanshen Liu, Yann Klinger, Renqi Lu et al.
Scientific Reports
earthquake and tectonic studies
article

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

Xuhang Yang, Guanshen Liu, Yann Klinger, Renqi Lu, Yiduo Liu, Wei Wang, Jinyu Zhang, Fang Xu, Zhaowu Guo
article en

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<sub>1</sub>) of the XSHF, the Daduhe fault (f<sub>2</sub>) and two previously unknown faults (f<sub>3</sub> and f<sub>4</sub>). 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.

Scientific ReportsVol. 15(1)
Centre National de la Recherche Scientifique (FR), Institut de physique du globe de Paris (FR), Chinese Academy of Sciences (CN), Institute of Mountain Hazards and Environment (CN), China Earthquake Administration (CN)
China Scholarship Council
Climate action
Openalex Percentile: Top 81%
earthquake and tectonic studies
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