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• W4323652015 abstract "Earthquakes occur because faults weaken with increasing slip and slip rate. Thermal pressurization (TP) of trapped pore fluids is deemed to be a widespread coseismic fault weakening mechanism. Yet, due to technical challenges, experimental evidence of TP is limited. Here, by exploiting a novel experimental configuration, we simulate seismic slip pulses (slip rate 2.0 m/s) on dolerite-built faults under pore fluid pressures up to 25 MPa. We measure transient sharp weakening, down to almost zero friction and concurrent with a spike in pore fluid pressure, which interrupts the exponential-decay slip weakening. The interpretation of mechanical and microstructural data plus numerical modeling suggests that wear and local melting processes in experimental faults generate ultra-fine materials to seal the pressurized pore water, causing transient TP spikes. Our work suggests that, with wear-induced sealing, TP may also occur in relatively permeable faults and could be quite common in nature." @default.
• W4323652015 created "2023-03-10" @default.
• W4323652015 creator A5047876949 @default.
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• W4323652015 date "2023-03-08" @default.
• W4323652015 modified "2023-09-30" @default.
• W4323652015 title "Coseismic fault sealing and fluid pressurization during earthquakes" @default.
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• W4323652015 doi "https://doi.org/10.1038/s41467-023-36839-9" @default.
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