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- W1618223280 abstract "This chapter summarizes experimental observations and related theoretical developments of faulted and intact rock properties related to earthquake nucleation, failure, and dynamic slip. It primarily considers earthquakes occurring in the brittle crust. Intermediate and deep-focus earthquakes having unique mechanical considerations are discussed. Further, the chapter focuses on repeatable laboratory observations and their direct implications for fault strength and stability. Natural faults in the Earth's crust are zones of localized shear that are inherently weaker than the surrounding intact rock. Slip can occur slowly as aseismic creep or rapidly as earthquakes with long interevent times during which little or no slip occurs. Crustal faults exhibit complex and irregular geometry, typically fractal in nature that includes irregular, interlocked surfaces, offset segments, bends, and junctions. Experimental and theoretical rock mechanics studies greatly influence the understanding of earthquakes and related crustal processes. Many key theoretical advances have either originated or been tested and refined through observations of brittle deformation under controlled laboratory conditions. Various parameters that affect strength of both fault surfaces and intact rock include mineralogy, porosity, cementation, packing geometry of gouge, and surface roughness." @default.
- W1618223280 created "2016-06-24" @default.
- W1618223280 creator A5053478711 @default.
- W1618223280 creator A5078703695 @default.
- W1618223280 date "2002-01-01" @default.
- W1618223280 modified "2023-10-14" @default.
- W1618223280 title "32 Rock failure and earthquakes" @default.
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