Origin and Nonuniversality of the Earthquake Interevent Time Distribution

Sarah Touati, Mark Naylor, and Ian G. Main
Phys. Rev. Lett. 102, 168501 – Published 24 April 2009

Abstract

Many authors have modeled regional earthquake interevent times using a gamma distribution, whereby data collapse occurs under a simple rescaling of the data from different regions or time periods. We show, using earthquake data and simulations, that the distribution is fundamentally a bimodal mixture distribution dominated by correlated aftershocks at short waiting times and independent events at longer times. The much-discussed power-law segment often arises as a crossover between these two. We explain the variation of the distribution with region size and show that it is not universal.

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  • Received 9 January 2009

DOI:https://doi.org/10.1103/PhysRevLett.102.168501

©2009 American Physical Society

Authors & Affiliations

Sarah Touati*, Mark Naylor, and Ian G. Main

  • School of GeoSciences, University of Edinburgh, Grant Institute, The King’s Buildings, West Mains Road, Edinburgh EH9 3JW, United Kingdom

  • *s.touati-2@sms.ed.ac.uk

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Vol. 102, Iss. 16 — 24 April 2009

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