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- W1575777612 abstract "The strength of active fault zones comprises the shear stress level required to cause fault slip. This parameter is fundamental in understanding the physics of earthquakes and assessing earthquake hazards. This chapter discusses available evidence and current ideas about fault zone strength and energetics. It outlines the general physical conditions prevailing in the Earth around active faults and summarizes the observational features of faulting and earthquake occurrence. The chapter also explores the usage of fault zone observations to infer various measures of fault shear stress. Further, it describes the assessment of the average shear stress state near faults, importance of stress heterogeneity in faulting processes and its implications. Active faults are stressed by forces applied in the adjacent lithosphere, forces applied at or near plate boundaries because of the motions of the plates as well as those caused by lateral density contrasts within the lithosphere. Parts of some active faults, particularly those at major plate boundaries, slip aseismically, keeping fault zone shear stresses at about the same levels." @default.
- W1575777612 created "2016-06-24" @default.
- W1575777612 creator A5065211715 @default.
- W1575777612 creator A5069652378 @default.
- W1575777612 date "2002-01-01" @default.
- W1575777612 modified "2023-10-13" @default.
- W1575777612 title "35 Strength and energetics of active fault zones" @default.
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- W1575777612 doi "https://doi.org/10.1016/s0074-6142(02)80238-8" @default.
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