Numerical simulations of earthquake rupture induced by pressure perturbationOAEI
Numerical simulations of earthquake rupture induced by pressure perturbation
The subsurface fluid injection can cause pressure increase within faults,leading to earthquake occur-rences.However,the factors controlling earthquake rupture due to pressure perturbation remain poorly understood.To resolve this problem,we simulate the physical processes of earthquake nucleation and rupture on strike-slip faults perturbated by pressure migration based on the slip-weakening law.Mul-tiple kinds of factors,including background stress,fluid injection rates,the area of the pressurized region,fault geometry,and fault friction coefficients,are considered in our simulations.Our simulation results reveal that the ratio of shear stress to normal stress rather than their absolute values controls the rupture behavior.With the large stress ratios,high injection rates,and large pressurized areas,earthquakes are prone to propagate as runaway ruptures.Additionally,faults with large aspect ratios of length to width are also favorable for causing runaway ruptures.In contrast,the factors of fault strike,dip angles and friction coefficients have minor influence on rupture behavior.
Bingquan Ren;Caijun Xu;Guoyan Jiang;Lei Yang
School of Geodesy and Geomatics,Wuhan University,Wuhan 430079,ChinaSchool of Geodesy and Geomatics,Wuhan University,Wuhan 430079,China||Key Laboratory of Geospace Environment and Geodesy,Ministry of Education,Wuhan University,Wuhan 430079,China||Key Laboratory of Geophysical Geodesy,Ministry of Natural Resources,Wuhan 430079,China
Induced seismicityFinite element simulationRupture mode
《大地测量与地球动力学(英文版)》 2024 (005)
477-487 / 11
This work is co-supported by the National Natural Science Foundation of China under Grants(42130101,42074007)and the Fundamental Research Funds for the Central Universities under Grants 2042023kf1035.We thank the editor and one anonymous reviewer for their constructive comments which have led to an improved manuscript.
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