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DOI10.1126/science.aaw7354
Fluid-induced aseismic fault slip outpaces pore-fluid migration
Bhattacharya P.; Viesca R.C.
发表日期2019
ISSN0036-8075
起始页码464
结束页码468
卷号364期号:6439
英文摘要Earthquake swarms attributed to subsurface fluid injection are usually assumed to occur on faults destabilized by increased pore-fluid pressures. However, fluid injection could also activate aseismic slip, which might outpace pore-fluid migration and transmit earthquake-triggering stress changes beyond the fluid-pressurized region.We tested this theoretical prediction against data derived from fluid-injection experiments that activated and measured slow, aseismic slip on preexisting, shallow faults.We found that the pore pressure and slip history imply a fault whose strength is the product of a slip-weakening friction coefficient and the local effective normal stress. Using a coupled shear-rupture model, we derived constraints on the hydromechanical parameters of the actively deforming fault. The inferred aseismic rupture front propagates faster and to larger distances than the diffusion of pressurized pore fluid. © 2019 American Association for the Advancement of Science. All rights reserved.
英文关键词dip-slip fault; earthquake event; fault slip; fluid injection; hydromechanics; porewater; prediction; pressure field; seismic method; Article; diffusion; fluid induced aseismic fault slip outpaces pore fluid migration; friction; physical phenomena; prediction; pressure; priority journal; stress
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/243040
作者单位Department of Civil and Environmental Engineering, Tufts University, Medford, MA 02155, United States; School of Earth, Ocean, and Climate Sciences, Indian Institute of Technology Bhubaneswar, Argul, Odisha, 752050, India
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Bhattacharya P.,Viesca R.C.. Fluid-induced aseismic fault slip outpaces pore-fluid migration[J],2019,364(6439).
APA Bhattacharya P.,&Viesca R.C..(2019).Fluid-induced aseismic fault slip outpaces pore-fluid migration.Science,364(6439).
MLA Bhattacharya P.,et al."Fluid-induced aseismic fault slip outpaces pore-fluid migration".Science 364.6439(2019).
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