While sliding at seismic slip-rates of ∼1 m/s, natural faults undergo an abrupt decrease of shear stress called dynamic weakening. Asperity-scale (
CITATION STYLE
Cornelio, C., Spagnuolo, E., Aretusini, S., Nielsen, S., Passelègue, F., Violay, M., … Di Toro, G. (2022). Determination of Parameters Characteristic of Dynamic Weakening Mechanisms During Seismic Faulting in Cohesive Rocks. Journal of Geophysical Research: Solid Earth, 127(7). https://doi.org/10.1029/2022JB024356
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