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Simulation of the Influence of Rate- and State-dependent Friction on the Macroscopic Behavior of Complex Fault Zones with the Lattice Solid Model |
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| Authors: | S Abe J H Dieterich P Mora D Place |
| Institution: | QUAKES, Department of Earth Sciences, The University of Queensland, Brisbane, Australia. E-mail: steffen@quakes.uq.edu.au, AU US Geological Survey Organisation (USGS), Menlo Park CA. E-mail: jdieterich@usgs.gov, AU QUAKES, Department of Earth Sciences, The University of Queensland, Brisbane, Australia. E-mail: mora@quakes.uq.edu.au, AU QUAKES, Department of Earth Sciences, The University of Queensland, Brisbane, Australia. E-mail: place@quakes.uq.edu.au, AU |
| Abstract: | -- In order to understand the earthquake nucleation process, we need to understand the effective frictional behavior of faults with complex geometry and fault gouge zones. One important aspect of this is the interaction between the friction law governing the behavior of the fault on the microscopic level and the resulting macroscopic behavior of the fault zone. Numerical simulations offer a possibility to investigate the behavior of faults on many different scales and thus provide a means to gain insight into fault zone dynamics on scales which are not accessible to laboratory experiments. Numerical experiments have been performed to investigate the influence of the geometric configuration of faults with a rate- and state-dependent friction at the particle contacts on the effective frictional behavior of these faults. The numerical experiments are designed to be similar to laboratory experiments by Dieterich and Kilgore (1994) in which a slide-hold-slide cycle was performed between two blocks of material and the resulting peak friction was plotted vs. holding time. Simulations with a flat fault without a fault gouge have been performed to verify the implementation. These have shown close agreement with comparable laboratory experiments. The simulations performed with a fault containing fault gouge have demonstrated a strong dependence of the critical slip distance Dc on the roughness of the fault surfaces and are in qualitative agreement with laboratory experiments. |
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