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- W3048683783 abstract "Abstract After an earthquake, faults can recover strength through fault healing, but the mechanisms responsible are not well understood. Seismic slip may induce sintering, a bonding process between solid particles in contact under high temperatures without melting, which could produce a fault rock with elevated strength and chemical stability. Here we present results from electron microscope analyses that show a typical sintered structure in a black disk-shaped rock from the Chelungpu fault, Taiwan. This structure is experimentally reproducible in simulated fault material, prepared from the local host-rock, by heating at 800–900 °C. Through thermal and kinetic analyses of experimental materials, we show that sintering is an exothermic process which can generate energy to enhance post-slip thermochemical reactions in the fault. We propose that sintering substantially contributes to earthquake energetics and fault healing and that its occurrence can be a useful indicator of past seismic slip." @default.
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- W3048683783 date "2020-08-13" @default.
- W3048683783 modified "2023-10-07" @default.
- W3048683783 title "Generation of sintered fault rock and its implications for earthquake energetics and fault healing" @default.
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- W3048683783 doi "https://doi.org/10.1038/s43247-020-0004-z" @default.
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