<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.nonlin-processes-geophys.net/inc/npg/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Nonlinear Processes  in Geophysics</journal_title>
		<journal_url>www.nonlin-processes-geophys.net</journal_url>
		<issn>1023-5809</issn>
		<eissn>1607-7946</eissn>
		<volume_number>2</volume_number>
		<issue_number>3/4</issue_number>
		<publication_year>1995</publication_year>
	</journal>
	<doi>10.5194/npg-2-131-1995</doi>
	<article_url>http://www.nonlin-processes-geophys.net/2/131/1995/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/2/131/1995/npg-2-131-1995.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/2/131/1995/npg-2-131-1995.pdf</fulltext_pdf>
	<start_page>131</start_page>
	<end_page>135</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Size-frequency relation of earthquakes in load-transfer models of fracture</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. B. Gómez</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>D. Iñiguez</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>A. F. Pacheco</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Geological Sciences, University College London, Gower Street, London WC1 6BT,U.K.</affiliation>
		<affiliation numeration="2" content_type="html">Departamento de Física Teórica, Universidad de Zaragoza, 50009 Zaragoza, Spain</affiliation>
	</affiliations>
	<abstract content_type="html">Using Monte Carlo simulations of the process of breaking in arrays of
elements with load-transfer rules, we have obtained the size- frequency relation of the
avalanches occurring in 1- and 2-dimensional stochastic fracture models. The resulting
power-law behaviour resembles the Gutenberg-Richter law for the relation between the size
(liberated energy) of earthquakes and their number frequency. The value of the power law
exponent is calculated as a function of the degree of stress dissipation present in the
model. The degree of dissipation is implemented in a straightforward and simple way by
assuming that only a fraction of the stress is transferred in each breaking event. The
models are robust with respect to the degree of dissipation and we observe a consistent
power-law behaviour for a broad range of dissipation values, both in ID and 2D. The value
of the power-law exponent is similar to the phenomenological &lt;i&gt;b&lt;/i&gt;- value (0.8
&lt;u&gt;&amp;lt;&lt;/u&gt; b &lt;u&gt; &amp;lt;&lt;/u&gt; 1.1) for
intermediate magnitude earthquakes.</abstract>
	<references>
	</references>
</article>

