Earthquake statistics in a Block Slider Model and a fully dynamic Fault Model

We examine the event statistics obtained from two differing simplified models for earthquake faults. The first model is a reproduction of the Block-Slider model of Carlson et al. (1991), a model often employed in seismicity studies. The second model is an elastodynamic fault model based upon the Lat...

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Main Authors: D. Weatherley, S. Abe
Format: Article
Language:English
Published: Copernicus Publications 2004-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/11/553/2004/npg-11-553-2004.pdf
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spelling doaj-7e975815d70a4ea08267e10ecc8f27252020-11-24T23:27:03ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462004-01-01115/6553560Earthquake statistics in a Block Slider Model and a fully dynamic Fault ModelD. WeatherleyS. AbeWe examine the event statistics obtained from two differing simplified models for earthquake faults. The first model is a reproduction of the Block-Slider model of Carlson et al. (1991), a model often employed in seismicity studies. The second model is an elastodynamic fault model based upon the Lattice Solid Model (LSM) of Mora and Place (1994). We performed simulations in which the fault length was varied in each model and generated synthetic catalogs of event sizes and times. From these catalogs, we constructed interval event size distributions and inter-event time distributions. The larger, localised events in the Block-Slider model displayed the same scaling behaviour as events in the LSM however the distribution of inter-event times was markedly different. The analysis of both event size and inter-event time statistics is an effective method for comparative studies of differing simplified models for earthquake faults.http://www.nonlin-processes-geophys.net/11/553/2004/npg-11-553-2004.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. Weatherley
S. Abe
spellingShingle D. Weatherley
S. Abe
Earthquake statistics in a Block Slider Model and a fully dynamic Fault Model
Nonlinear Processes in Geophysics
author_facet D. Weatherley
S. Abe
author_sort D. Weatherley
title Earthquake statistics in a Block Slider Model and a fully dynamic Fault Model
title_short Earthquake statistics in a Block Slider Model and a fully dynamic Fault Model
title_full Earthquake statistics in a Block Slider Model and a fully dynamic Fault Model
title_fullStr Earthquake statistics in a Block Slider Model and a fully dynamic Fault Model
title_full_unstemmed Earthquake statistics in a Block Slider Model and a fully dynamic Fault Model
title_sort earthquake statistics in a block slider model and a fully dynamic fault model
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2004-01-01
description We examine the event statistics obtained from two differing simplified models for earthquake faults. The first model is a reproduction of the Block-Slider model of Carlson et al. (1991), a model often employed in seismicity studies. The second model is an elastodynamic fault model based upon the Lattice Solid Model (LSM) of Mora and Place (1994). We performed simulations in which the fault length was varied in each model and generated synthetic catalogs of event sizes and times. From these catalogs, we constructed interval event size distributions and inter-event time distributions. The larger, localised events in the Block-Slider model displayed the same scaling behaviour as events in the LSM however the distribution of inter-event times was markedly different. The analysis of both event size and inter-event time statistics is an effective method for comparative studies of differing simplified models for earthquake faults.
url http://www.nonlin-processes-geophys.net/11/553/2004/npg-11-553-2004.pdf
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