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<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>9</volume_number>
		<issue_number>5/6</issue_number>
		<publication_year>2002</publication_year>
	</journal>
	<doi>10.5194/npg-9-513-2002</doi>
	<article_url>http://www.nonlin-processes-geophys.net/9/513/2002/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/9/513/2002/npg-9-513-2002.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/9/513/2002/npg-9-513-2002.pdf</fulltext_pdf>
	<start_page>513</start_page>
	<end_page>519</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">A minimalist model of characteristic earthquakes</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Vázquez-Prada</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>Á. González</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. B. Gómez</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>A. F. Pacheco</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Faculty of Sciences, University of Zaragoza, Pedro Cerbuna, 12, 50009 Zaragoza, Spain</affiliation>
	</affiliations>
	<abstract content_type="html">In a spirit akin to
      the sandpile model of self-organized criticality, we present a simple
      statistical model of the cellular-automaton type which simulates the role
      of an asperity in the dynamics of a one-dimensional fault. This model
      produces an earthquake spectrum similar to the characteristic-earthquake
      behaviour of some seismic faults. This model, that has no parameter, is
      amenable to an algebraic description as a Markov Chain. This possibility
      illuminates some important results, obtained by Monte Carlo simulations,
      such as the earthquake size-frequency relation and the recurrence time of
      the characteristic earthquake.</abstract>
	<references>
	</references>
</article>

