Quadratic Stress Drop Model of the 2013 Mw 6.6 Lushan Earthquake and Aftershocks Triggered by Blind Thrust Events

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作者
Qiu Zhong
Jian Lin
Baoping Shi
Wenhao Shen
机构
[1] Innovation Academy of South China Sea Ecology and Environmental Engineering,Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology
[2] Chinese Academy of Sciences,Department of Ocean Science and Engineering
[3] Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou),Department of Geology and Geophysics
[4] Southern University of Science and Technology,College of Earth Science
[5] Woods Hole Oceanographic Institution,Ministry of Emergency Management
[6] University of Chinese Academy of Sciences,undefined
[7] National Institute of Natural Hazards,undefined
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Stress drop model; Coulomb stress changes; aftershock triggering; Lushan earthquake; friction coefficient;
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摘要
To reveal the distribution pattern of aftershocks of the Mw 6.6 Lushan earthquake on April 20, 2013, we analyzed finite-source slip models from seismic waveform inversions and calculated the stress changes on and off the main rupture. In the spatial domain, the fitted coseismic slip–stress relation on subfaults is much closer to the quadratic stress drop model than to the uniform stress model. In the wavenumber domain, the slip and stress change spectrum decay asymptotically as k−3 and k−2, respectively, where k is the wavenumber. And in this domain, we also find that the prediction of a quadratic stress drop model matches data better than a uniform stress drop model. In addition, we studied the effective friction coefficient on the fault. Aftershocks were clustered around a relatively narrow zone that counters the main rupture plane. The narrow zone has a main rupture width with a standard deviation of 2.7 km for M ≥ 3 events. For 12 M ≥ 4.8 aftershocks, approximately 33% of nodal planes were calculated to be located in the zone of positive shear stress changes, while 83% were in the zone of positive normal stress changes (unclamp), suggesting a high effective friction coefficient μ′\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\mu }^{^{\prime}}$$\end{document}≥ 0.8 on the main fault. Combined with the investigation in aftershocks triggered by blind thrust events at Whittier Narrows (USA), Zemmouri (Algeria), and Gorkha (Nepal), we suggest that the correlation between aftershocks and positive Coulomb stress changes increases with the effective friction coefficient μ′\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\mu \mathrm{^{\prime}}$$\end{document}, and the effective friction coefficient and normal stress changes play an important role in aftershock triggering of blind thrust events.
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页码:1147 / 1157
页数:10
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