Scaling in a cellular automaton model of earthquake faults

Simple item page
dc.creatorAnghel, M.
dc.creatorKlein, W.
dc.creatorRundle, J. B.
dc.creatorMartins, J. S. S'a
dc.date2000-02-29
dc.date.accessioned2026-07-07T02:36:54Z
dc.date.available2026-07-07T02:36:54Z
dc.descriptionWe present theoretical arguments and simulation data indicating that the scaling of earthquake events in models of faults with long-range stress transfer is composed of at least three distinct regions. These regions correspond to three classes of earthquakes with different underlying physical mechanisms. In addition to the events that exhibit scaling, there are larger ``breakout'' events that are not on the scaling plot. We discuss the interpretation of these events as fluctuations in the vicinity of a spinodal critical point.
dc.description5 pages, 2 figures
dc.identifierhttps://arxiv.org/abs/cond-mat/0002459
dc.identifierhttp://arxiv.org/abs/cond-mat/0002459
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/16097
dc.subjectStatistical Mechanics
dc.titleScaling in a cellular automaton model of earthquake faults
dc.typetext

Files

Collections

arXiv