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DOI10.1016/j.tecto.2020.228538
A hybrid source mechanism of the 2017 Mw 6.5 Jiuzhaigou earthquake revealed by the joint inversion of strong-motion, teleseismic and InSAR data
Zheng A.; Yu X.; Xu W.; Chen X.; Zhang W.
发表日期2020
ISSN00401951
卷号789
英文摘要As occurred during the tourist season, the 2017 Mw 6.5 Jiuzhaigou (China) earthquake led to destructive damages. The seismogenic fault of this event was merely speculated to be the northern extension of the Huya fault, while no apparent surface ruptures were discovered in the field investigation. Previous studies and released moment tensor solutions indicated the Jiuzhaigou earthquake was dominated by left-lateral strike slip with partial normal-slip component. It seems unintelligible that the normal slip occurred in this event as the epicenter was located near the boundary of convergent blocks. Hence, a reasonable and elaborate source rupture model is necessary to investigate such a blind fault and the role it plays in the complex fault system of this region. Combining space-based geodetic, teleseismic or regional seismic observations can provide detailed information about earthquake ruptures. We first attempted to determine the fault geometry using the Bayesian approach with synthetic aperture radar interferograms (InSAR). And then the fault geometry was refined based on the relocated aftershock distribution, and a two-segment fault model was constructed. Based on the two-segment model, we resolved the source rupture process of the 2017 Jiuzhaigou earthquake through the joint inversion of strong-motion, teleseismic body-wave and InSAR data. The inversion results reveal a hybrid source mechanism, in which normal and thrust slips coexist besides the strike-slip component. We suggest that the eastward motion with the extrusion of the lower crustal flow in the northeastern margin of the Bayan Har block is responsible for such a faulting behavior. The co-seismic Coulomb stress changes show a significant stress loading in the western segment of the Tazang fault, increasing its seismic hazard. Due to the lack of aftershocks to the southeast of the seismogenic fault, the probably enhanced seismicity in the northern segment of the Huya fault is also worth further attention. © 2020 Elsevier B.V.
关键词Finite fault modelInSARJiuzhaigou earthquakeJoint inversionTectonic implications
英文关键词Bayesian networks; Earthquake effects; Synthetic aperture radar; Aftershock distributions; Complex fault system; Coulomb stress changes; Lower crustal flows; Moment tensor solutions; Source rupture process; Strike-slip component; Teleseismic body waves; Faulting; aftershock; data inversion; earthquake epicenter; earthquake event; earthquake magnitude; earthquake mechanism; fault slip; fault zone; interferometry; satellite data; seismic hazard; seismic source; strong motion; synthetic aperture radar; tectonic setting; teleseismic wave; China; Sichuan
语种英语
来源期刊Tectonophysics
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/207918
作者单位School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China; Department of Earth and Space Sciences, Southern University of Science and Technology, Shenzhen, China; College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, China; School of Geosciences and Info-Physics, Central South University, Changsha, China; Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring (Central South University), Ministry of Education, Changsha, China
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Zheng A.,Yu X.,Xu W.,et al. A hybrid source mechanism of the 2017 Mw 6.5 Jiuzhaigou earthquake revealed by the joint inversion of strong-motion, teleseismic and InSAR data[J],2020,789.
APA Zheng A.,Yu X.,Xu W.,Chen X.,&Zhang W..(2020).A hybrid source mechanism of the 2017 Mw 6.5 Jiuzhaigou earthquake revealed by the joint inversion of strong-motion, teleseismic and InSAR data.Tectonophysics,789.
MLA Zheng A.,et al."A hybrid source mechanism of the 2017 Mw 6.5 Jiuzhaigou earthquake revealed by the joint inversion of strong-motion, teleseismic and InSAR data".Tectonophysics 789(2020).
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