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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>4</volume_number>
		<issue_number>5/6</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/nhess-4-691-2004</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/4/691/2004/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/4/691/2004/nhess-4-691-2004.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/4/691/2004/nhess-4-691-2004.pdf</fulltext_pdf>
	<start_page>691</start_page>
	<end_page>695</end_page>
	<publication_date>2004-11-03</publication_date>
	<article_title content_type="html">Information entropy analysis of seismicity of Umbria-Marche region (Central Italy)</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Telesca</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>V. Lapenna</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Lovallo</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Methodologies for Environmental Analysis, National Research Council, Tito, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">We investigated by means of nonlinear tools the temporal distribution of
1983-2003 seismicity of the Umbria-Marche region, Central Italy, that was
struck by a strong event (M=5.8) on 26 September 1997. Information entropy
analysis has been performed over the full and the aftershock-depleted
catalogue. We analysed the series of the interevent times between successive
earthquakes and the series of their magnitudes. The time evolution of this
measure shows a clear anomalous behaviour in correspondence with the
stronger event, more evident in the full catalogue than in the
aftershock-depleted one.</abstract>
	<references>
	</references>
</article>

