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

被引:0
作者
Xu, Fang [1 ,2 ]
Lu, Renqi [1 ]
Zhang, Jinyu [1 ]
Klinger, Yann [2 ]
Liu, Yiduo [3 ]
Yang, Xuhang [1 ]
Liu, Guanshen [1 ]
Wang, Wei [1 ]
Guo, Zhaowu [1 ]
机构
[1] China Earthquake Adm, Inst Geol, State Key Lab Earthquake Dynam & Forecasting, Beijing, Peoples R China
[2] Univ Paris Cite, CNRS, Inst Phys Globe Paris, Paris, France
[3] Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Hazards & Surface Proc, Chengdu, Peoples R China
关键词
Luding M-w 6.6 earthquake; Xianshuihe fault zone; Southeastern Tibetan plateau; 3D fault model; Coulomb stress change; Seismic hazard analysis; COULOMB STRESS EVOLUTION; SLIP-RATES; EASTERN BOUNDARY; WESTERN SICHUAN; LONGMEN SHAN; YUNNAN; SEQUENCE; CHINA; DEFORMATION; BEHAVIOR;
D O I
10.1038/s41598-025-11553-2
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
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 (Delta CFS) calculation for further seismic potential analysis. Therefore, first we build a detailed 3D fault model of the earthquake and then we compute Delta CFS 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 Delta CFS 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 Delta CFS and hence a notable enhancement in seismic hazard in the northern ANHF.
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页数:14
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共 64 条
[1]  
[Anonymous], ABOUT US
[2]   Fourier-domain Green's function for an elastic semi-infinite solid under gravity, with applications to earthquake and volcano deformation [J].
Barbot, Sylvain ;
Fialko, Yuri .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2010, 182 (02) :568-582
[3]   Three-dimensional imaging of active structures using earthquake aftershocks: the Northridge thrust, California [J].
Carena, S ;
Suppe, J .
JOURNAL OF STRUCTURAL GEOLOGY, 2002, 24 (04) :887-904
[4]   Late Quaternary Slip-rates and Slip Partitioning on the Southeastern Xianshuihe Fault System, Eastern Tibetan Plateau [J].
Chen Guihua ;
Xu Xiwei ;
Wen Xueze ;
Chen Yue-Gau .
ACTA GEOLOGICA SINICA-ENGLISH EDITION, 2016, 90 (02) :537-554
[5]  
陈运泰, 2013, [中国科学. 地球科学, Scientia Sinica Terrae], V43, P1064
[6]  
China Earthquake Disaster Prevention Center, 1999, Catalog of Modern Earthquakes in China from 1912 To 1990 AD, Ms≥4.7
[7]  
[邓起东 DENG Qidong], 2008, [地震地质, Seismology and Geology], V30, P1
[8]   Seismic remote sensing for the earthquake source process and near-source strong shaking: A case study of the October 16, 1999 hector mine earthquake [J].
Dreger, D ;
Kaverina, A .
GEOPHYSICAL RESEARCH LETTERS, 2000, 27 (13) :1941-1944
[9]   Dynamic earthquake rupture simulations on nonplanar faults embedded in 3D geometrically complex, heterogeneous elastic solids [J].
Duru, Kenneth ;
Dunham, Eric M. .
JOURNAL OF COMPUTATIONAL PHYSICS, 2016, 305 :185-207
[10]   Earthquake triggering by static, dynamic, and postseismic stress transfer [J].
Freed, AM .
ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, 2005, 33 :335-367