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

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 Xianshu...

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Main Authors: Fang Xu, Renqi Lu, Jinyu Zhang, Yann Klinger, Yiduo Liu, Xuhang Yang, Guanshen Liu, Wei Wang, Zhaowu Guo
Format: Article
Language:English
Published: Nature Portfolio 2025-07-01
Series:Scientific Reports
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Online Access:https://doi.org/10.1038/s41598-025-11553-2
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author Fang Xu
Renqi Lu
Jinyu Zhang
Yann Klinger
Yiduo Liu
Xuhang Yang
Guanshen Liu
Wei Wang
Zhaowu Guo
author_facet Fang Xu
Renqi Lu
Jinyu Zhang
Yann Klinger
Yiduo Liu
Xuhang Yang
Guanshen Liu
Wei Wang
Zhaowu Guo
author_sort Fang Xu
collection DOAJ
description 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 (f1) of the XSHF, the Daduhe fault (f2) and two previously unknown faults (f3 and f4). 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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institution Kabale University
issn 2045-2322
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publishDate 2025-07-01
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spelling doaj-art-11c4cd78056f446a853c86aab8244e782025-08-20T03:45:53ZengNature PortfolioScientific Reports2045-23222025-07-0115111410.1038/s41598-025-11553-2Detailed three-dimensional fault model of the 2022 M w 6.6 Luding earthquake reveals seismic hazard potential in the southeastern Tibetan plateauFang Xu0Renqi Lu1Jinyu Zhang2Yann Klinger3Yiduo Liu4Xuhang Yang5Guanshen Liu6Wei Wang7Zhaowu Guo8State Key Laboratory of Earthquake Dynamics and Forecasting, Institute of Geology, China Earthquake AdministrationState Key Laboratory of Earthquake Dynamics and Forecasting, Institute of Geology, China Earthquake AdministrationState Key Laboratory of Earthquake Dynamics and Forecasting, Institute of Geology, China Earthquake AdministrationUniversite Paris Cite, Institut Physique du Globe de Paris, CNRSKey Laboratory of Mountain Hazards and Surface Processes, Institute of Mountain Hazards and Environment, Chinese Academy of SciencesState Key Laboratory of Earthquake Dynamics and Forecasting, Institute of Geology, China Earthquake AdministrationState Key Laboratory of Earthquake Dynamics and Forecasting, Institute of Geology, China Earthquake AdministrationState Key Laboratory of Earthquake Dynamics and Forecasting, Institute of Geology, China Earthquake AdministrationState Key Laboratory of Earthquake Dynamics and Forecasting, Institute of Geology, China Earthquake AdministrationAbstract 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 (f1) of the XSHF, the Daduhe fault (f2) and two previously unknown faults (f3 and f4). 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.https://doi.org/10.1038/s41598-025-11553-2Luding M w 6.6 earthquakeXianshuihe fault zoneSoutheastern Tibetan plateau3D fault modelCoulomb stress changeSeismic hazard analysis
spellingShingle Fang Xu
Renqi Lu
Jinyu Zhang
Yann Klinger
Yiduo Liu
Xuhang Yang
Guanshen Liu
Wei Wang
Zhaowu Guo
Detailed three-dimensional fault model of the 2022 M w 6.6 Luding earthquake reveals seismic hazard potential in the southeastern Tibetan plateau
Scientific Reports
Luding M w 6.6 earthquake
Xianshuihe fault zone
Southeastern Tibetan plateau
3D fault model
Coulomb stress change
Seismic hazard analysis
title Detailed three-dimensional fault model of the 2022 M w 6.6 Luding earthquake reveals seismic hazard potential in the southeastern Tibetan plateau
title_full Detailed three-dimensional fault model of the 2022 M w 6.6 Luding earthquake reveals seismic hazard potential in the southeastern Tibetan plateau
title_fullStr Detailed three-dimensional fault model of the 2022 M w 6.6 Luding earthquake reveals seismic hazard potential in the southeastern Tibetan plateau
title_full_unstemmed Detailed three-dimensional fault model of the 2022 M w 6.6 Luding earthquake reveals seismic hazard potential in the southeastern Tibetan plateau
title_short Detailed three-dimensional fault model of the 2022 M w 6.6 Luding earthquake reveals seismic hazard potential in the southeastern Tibetan plateau
title_sort detailed three dimensional fault model of the 2022 m w 6 6 luding earthquake reveals seismic hazard potential in the southeastern tibetan plateau
topic Luding M w 6.6 earthquake
Xianshuihe fault zone
Southeastern Tibetan plateau
3D fault model
Coulomb stress change
Seismic hazard analysis
url https://doi.org/10.1038/s41598-025-11553-2
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