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THERMO- AND HYDRO-MECHANICAL PROCESSES ALONGFAULTS DURING RAPID SLIP (2009)
It is suggested that the two primary dynamic weakening mechanisms during seismic slip, are then as follows: (1) Flash heating at highly stressed frictional micro-contacts, and (2) Thermal pressurization of fault-zone pore fluid. Both have characteristics which promote extreme localization of shear.
Reference:
"Meso-Scale Shear Physics in Earthquake and Landslide Mechanics"
"Meso-Scale Shear Physics in Earthquake and Landslide Mechanics"
Organization:
Department of Earth and Planetary Sciences and School of Engineering andApplied Sciences, Harvard University, Cambridge, MA, USA
Department of Earth and Planetary Sciences and School of Engineering andApplied Sciences, Harvard University, Cambridge, MA, USA
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