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<!DOCTYPE article SYSTEM "http://www.nat-hazards-earth-syst-sci.net/inc/nhess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Natural Hazards and Earth System Science</journal_title>
		<journal_url>www.nat-hazards-earth-syst-sci.net</journal_url>
		<issn>1561-8633</issn>
		<eissn>1684-9981</eissn>
		<volume_number>1</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2001</publication_year>
	</journal>
	<doi>10.5194/nhess-1-145-2001</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/1/145/2001/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/1/145/2001/nhess-1-145-2001.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/1/145/2001/nhess-1-145-2001.pdf</fulltext_pdf>
	<start_page>145</start_page>
	<end_page>158</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">The pecularities of shear crack pre-rupture evolution and distribution of seismicity before strong earthquakes</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Kiyashchenko</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>V. Troyan</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Physics Department, St. Petersburg State University, 1 Ulianovskaya Street, St. Petersburg, 198 504, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">Several
      methods are presently suggested for investigating pre-earthquake evolution
      of the regions of high tectonic activity based on analysis of the
      seismicity spatial distribution. Some precursor signatures are detected
      before strong earthquakes: decrease in fractal dimension of the continuum
      of earthquake epicenters, cluster formation, concentration of seismic
      events near one of the nodal planes of the future earthquake, and others.
      In the present paper, it is shown that such peculiarities are typical of
      the evolution of the shear crack network under external stresses in
      elastic bodies with inhomogeneous distribution of strength. The results of
      computer modeling of crack network evolution are presented. It is shown
      that variations of the fractal dimension of the earthquake epicenters’
      continuum and other precursor signatures contain information about the
      evolution of the destruction process towards the main rupture.</abstract>
	<references>
	</references>
</article>

