Experimental studies of compaction and dilatancy during frictional sliding on faults containing gouge
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Cited by (108)
Fracturing and pore-fluid distribution in the Marlborough region, New Zealand from body-wave tomography: Implications for regional understanding of the Kaikōura area
2022, Earth and Planetary Science LettersCitation Excerpt :Without such a process, fractures from the immature stage of fault development would continue to exist throughout maturation (Fig. 10). Fault healing, which is commonly observed after earthquakes, often results in reduced fracture concentration from processes such as crack closure, compaction, and healing of microcracks (Morrow and Byerlee, 1989; Brantley et al., 1990; Sleep and Blanpied, 1992; Segall and Rice, 1995; Li and Vidale, 2001; Li et al., 2004). It is not clear which of these processes operate in the Marlborough region.
Modeling connected granular media: Particle bonding within the level set discrete element method
2021, Computer Methods in Applied Mechanics and EngineeringDilatancy-induced fluid pressure drop during dynamic rupture: Direct experimental evidence and consequences for earthquake dynamics
2020, Earth and Planetary Science LettersFracture-induced pore fluid pressure weakening and dehydration of serpentinite
2019, TectonophysicsCitation Excerpt :% water added arises from the presence of pressurized fluids in the fault zones. In lower pressure experiments (≤300 MPa), strain weakening of sheet silicates during frictional sliding sometimes occurs during fabric development (e.g., Morrow and Byerlee, 1989). This weakening arises from the rotation of grains into a preferred orientation that aligns the weak basal planes (Haines et al., 2013).