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• W1505093060 abstract "A new earthquake model of spatiotemporal dynamics is introduced. In contrast to many other earthquake models, this one does not contain a velocity-weakening frictional force, and is thus an alternative to the Burridge-Knopoff earthquake model. Dissipation in our model occurs only through viscous forces acting in the presence of a non-dissipative random potential. Both small localized and large delocalized events are observed. The scaling behavior of the event probability distribution is found to be non-universal and distinct from that found in other earthquake models. The system loses instability as the strength of the pulling spring becomes large enough. It also shows transitions from behavior exhibiting a wide range of magnitudes of slipping events to showing a narrow range scale in which only large events occur for a certain range of parameters. Effects of varying system size, boundary conditions and pulling speed were investigated." @default.
• W1505093060 created "2016-06-24" @default.
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• W1505093060 date "1997-01-01" @default.
• W1505093060 modified "2023-09-22" @default.
• W1505093060 title "Modeling the Spatiotemporal Dynamics of Earthquakes with a Conservative Random Potential and a Viscous Force" @default.
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• W1505093060 doi "https://doi.org/10.1007/978-1-4613-8500-4_21" @default.
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