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024 7 _ |a 10.1103/PhysRevLett.121.234302
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100 1 _ |a Brener, Efim A.
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245 _ _ |a Unstable Slip Pulses and Earthquake Nucleation as a Nonequilibrium First-Order Phase Transition
260 _ _ |a College Park, Md.
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520 _ _ |a The onset of rapid slip along initially quiescent frictional interfaces, the process of “earthquake nucleation,” and dissipative spatiotemporal slippage dynamics play important roles in a broad range of physical systems. Here we first show that interfaces described by generic friction laws feature stress-dependent steady-state slip pulse solutions, which are unstable in the quasi-1D approximation of thin elastic bodies. We propose that such unstable slip pulses of linear size L∗ and characteristic amplitude are “critical nuclei” for rapid slip in a nonequilibrium analogy to equilibrium first-order phase transitions and quantitatively support this idea by dynamical calculations. We then perform 2D numerical calculations that indicate that the nucleation length L∗ exists also in 2D and that the existence of a fracture mechanics Griffith-like length LG
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700 1 _ |a Aldam, Michael
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700 1 _ |a Barras, Fabian
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700 1 _ |a Molinari, Jean-François
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700 1 _ |a Bouchbinder, Eran
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773 _ _ |a 10.1103/PhysRevLett.121.234302
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