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| Hauptseite > Publikationsdatenbank > Unstable Slip Pulses and Earthquake Nucleation as a Nonequilibrium First-Order Phase Transition > print |
| Hauptseite > Publikationsdatenbank > Unstable Slip Pulses and Earthquake Nucleation as a Nonequilibrium First-Order Phase Transition > print |
| 001 | 859605 | ||
| 005 | 20210130000330.0 | ||
| 024 | 7 | _ | |a 10.1103/PhysRevLett.121.234302 |2 doi |
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| 100 | 1 | _ | |a Brener, Efim A. |0 P:(DE-HGF)0 |b 0 |e Corresponding author |
| 245 | _ | _ | |a Unstable Slip Pulses and Earthquake Nucleation as a Nonequilibrium First-Order Phase Transition |
| 260 | _ | _ | |a College Park, Md. |c 2018 |b APS |
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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 Bouchbinder, Eran |0 P:(DE-HGF)0 |b 4 |
| 773 | _ | _ | |a 10.1103/PhysRevLett.121.234302 |g Vol. 121, no. 23, p. 234302 |0 PERI:(DE-600)1472655-5 |n 23 |p 234302 |t Physical review letters |v 121 |y 2018 |x 1079-7114 |
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