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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>1</issue_number>
		<publication_year>2002</publication_year>
	</journal>
	<doi>10.5194/npg-9-31-2002</doi>
	<article_url>http://www.nonlin-processes-geophys.net/9/31/2002/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/9/31/2002/npg-9-31-2002.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/9/31/2002/npg-9-31-2002.pdf</fulltext_pdf>
	<start_page>31</start_page>
	<end_page>35</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Self-sustained oscillator as a model for explosion quakes at Stromboli Volcano</article_title>
	<authors>
		<author numeration="1" affiliations="1,3">
			<name>S. De Martino</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>C. Godano</name>
		</author>
		<author numeration="3" affiliations="1,3">
			<name>M. Falanga</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Physics, Salerno University, Via S. Allende, Baronissi (SA) 84084 Italy</affiliation>
		<affiliation numeration="2" content_type="html">Dipartimento di Scienze Ambientali, II Universita’ di Napoli, Caserta, Italy</affiliation>
		<affiliation numeration="3" content_type="html">INFM unita’ di Salerno, 84081 Baronissi (SA), Italy</affiliation>
	</affiliations>
	<abstract content_type="html">We analyze seismic
      signals produced by explosion-quakes at Stromboli Volcano. We use standard
      nonlinear procedures to search a low-order effective dynam-ics. The
      dimension of the reconstructed phase space depends on the number of
      samples. Namely larger time lengths cor-respond to dynamical systems of
      different complexity. If we restrict the analysis to the signal associated
      directly to the source (Chouet et al., 1997), we obtain a phase space
      dimen-sion equal to two. We reproduce this part of the signal with a
      simple single self-sustained oscillator.</abstract>
	<references>
	</references>
</article>

