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16/9/2011UCERF3 / EQ Simulators Workshop ViscoSim Fred Pollitz USGS, Menlo Park
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26/9/2011UCERF3 / EQ Simulators Workshop Representation of Fault Friction Static frictional stress Dynamic frictional stress Arrest stress Dynamic overshoot parameter: Stress reduction parameter: = s - a D = s - a )/( s - d )
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36/9/2011UCERF3 / EQ Simulators Workshop Representation of Fault Friction
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46/9/2011UCERF3 / EQ Simulators Workshop Representation of Viscoelasticity Pa s 3 x Pa s
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136/9/2011UCERF3 / EQ Simulators Workshop Approximations to Elastodynamics Representation of inertia –None Representation of rupture propagation –Cascade model
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146/9/2011UCERF3 / EQ Simulators Workshop Fault Interaction
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156/9/2011UCERF3 / EQ Simulators Workshop # Viscoelastic Greens functions = x 3721 [map points] X 16 [source depths] X 16 [obs. depths] x 11 [sample times] x 6 [stress tensor components] = 6 x 10 7
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166/9/2011UCERF3 / EQ Simulators Workshop Twenty consecutive M>6.7 ruptures M6.9
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176/9/2011UCERF3 / EQ Simulators Workshop M7.2
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186/9/2011UCERF3 / EQ Simulators Workshop M7.0
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196/9/2011UCERF3 / EQ Simulators Workshop M7.6
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206/9/2011UCERF3 / EQ Simulators Workshop M6.7
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216/9/2011UCERF3 / EQ Simulators Workshop M7.5
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226/9/2011UCERF3 / EQ Simulators Workshop M7.6
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236/9/2011UCERF3 / EQ Simulators Workshop M7.2
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246/9/2011UCERF3 / EQ Simulators Workshop M6.7
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256/9/2011UCERF3 / EQ Simulators Workshop M6.7
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266/9/2011UCERF3 / EQ Simulators Workshop M7.7
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276/9/2011UCERF3 / EQ Simulators Workshop M7.3
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286/9/2011UCERF3 / EQ Simulators Workshop M7.5
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296/9/2011UCERF3 / EQ Simulators Workshop M7.3
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306/9/2011UCERF3 / EQ Simulators Workshop M7.3
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316/9/2011UCERF3 / EQ Simulators Workshop M7.2
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326/9/2011UCERF3 / EQ Simulators Workshop M6.7
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336/9/2011UCERF3 / EQ Simulators Workshop M7.2
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366/9/2011UCERF3 / EQ Simulators Workshop Simulator parameters Dynamic overshoot parameter: Stress reduction parameter: = s - a D = s - a )/( s - d ) Shape of slip-weakening curve Mantle viscosity m
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376/9/2011UCERF3 / EQ Simulators Workshop Results with ViscoSim Fault system behavior is sensitive to simple parameters Simulations capture Gutenberg-Richter and characteristic-earthquake behavior Characteristic magnitude and mean recurrence interval may exhibit a systematic dependence on mantle viscosity
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