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Rupture dynamics of a planar fault in a 3D elastic medium: Rate- and slip-weakening friction
162
Citations
36
References
1998
Year
EngineeringFault GeologyMechanical EngineeringFracture MechanicsMechanicsSpontaneous PropagationPlanar FaultEarthquake EngineeringSeismic CycleShear ZoneSolid MechanicsEarthquake RuptureElastic MediumFault GeometryGeomechanicsCrack FormationDynamic Crack PropagationRupture DynamicsMechanics Of MaterialsBiem Formulation
Abstract We propose a new boundary integral equation method (BIEM) to model the spontaneous propagation of rupture on a planar fault embedded in a homogeneous elastic medium. The BIEM formulation is very compact and fast in computation, so that we are able to study the effect of different slip- and rate-dependent friction laws on dynamic shear fault propagation. We simulated a spontaneous rupture by a sudden break of asperity under two friction laws, rate and/or slip weakening. We examined both long and circular asperities. The long asperity model corresponds to the 2D anti-plane or in-plane problem. The obtained result shows that slip-weakening friction is important at the crack tip, and rate-weakening friction plays an important role in the healing stage. If slip-weakening friction is strong stress drops gradually at the crack tip. On the other hand, if rate-weakening friction is strong stress drops abruptly, but it stops suddenly and sometimes stress recovers. This sudden stop of rupture produces a heterogeneous stress distribution, which will in turn produce aftershocks. Finally, we studied a realistic asperity model in which rupture starts from a small patch and then propagates with finite rupture speed. Depending on the asperity size healing can occur even without rate-weakening friction. This is due to very strong healing waves produced by the edges of the asperity.
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