Slip Complexity in a Crustal-Plane Model of an Earthquake Fault

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Slip Complexity in a Crustal-Plane Model of an Earthquake Fault.

We study numerically the behavior of a two-dimensional elastic plate (a crustal plane) that terntinates along one of its edges at a fault boundary. Slip-weakening friction at the boundary, inertial dynamics in the bulk, and uniform slow loading via elastic coupling to a substrate combine to produce a complex, deterministically chaotic sequence of slipping events. We observe a power-law distribo...

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Slip complexity in earthquake fault models.

We summarize studies of earthquake fault models that give rise to slip complexities like those in natural earthquakes. For models of smooth faults between elastically deformable continua, it is critical that the friction laws involve a characteristic distance for slip weakening or evolution of surface state. That results in a finite nucleation size, or coherent slip patch size, h*. Models of sm...

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Slip complexity in dynamic models of earthquake faults.

We summarize recent evidence that models of earthquake faults with dynamically unstable friction laws but no externally imposed heterogeneities can exhibit slip complexity. Two models are described here. The first is a one-dimensional model with velocity-weakening stick-slip friction; the second is a two-dimensional elastodynamic model with slip-weakening friction. Both exhibit small-event comp...

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ژورنال

عنوان ژورنال: Physical Review Letters

سال: 1996

ISSN: 0031-9007,1079-7114

DOI: 10.1103/physrevlett.77.972