<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "https://jats.nlm.nih.gov/nlm-dtd/publishing/3.0/journalpublishing3.dtd">
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">NPG</journal-id>
<journal-title-group>
<journal-title>Nonlinear Processes in Geophysics</journal-title>
<abbrev-journal-title abbrev-type="publisher">NPG</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Nonlin. Processes Geophys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1607-7946</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/npg-11-545-2004</article-id>
<title-group>
<article-title>Investigating the spatial variability of the time-scaling properties in Italian seismicity</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Telesca</surname>
<given-names>L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lapenna</surname>
<given-names>V.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Methodologies for Environmental Analysis, National Research Council, Tito Scalo (PZ), Italy</addr-line>
</aff>
<pub-date pub-type="epub">
<day>16</day>
<month>11</month>
<year>2004</year>
</pub-date>
<volume>11</volume>
<issue>5/6</issue>
<fpage>545</fpage>
<lpage>552</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2004 L. Telesca</copyright-statement>
<copyright-year>2004</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://npg.copernicus.org/articles/11/545/2004/npg-11-545-2004.html">This article is available from https://npg.copernicus.org/articles/11/545/2004/npg-11-545-2004.html</self-uri>
<self-uri xlink:href="https://npg.copernicus.org/articles/11/545/2004/npg-11-545-2004.pdf">The full text article is available as a PDF file from https://npg.copernicus.org/articles/11/545/2004/npg-11-545-2004.pdf</self-uri>
<abstract>
<p>Significant power-law long-range correlated structures have been identified
in the Italian seismicity from 1983 to 2003. We performed the Allan Factor
Analysis and the Detrended Fluctuation Analysis on both the full and the
aftershock-depleted seismic data, extracted by the INGV (National Institute
of Geophysics and Volcanology) instrumental catalog.Our findings suggest that (i) the time-scaling behaviour
characterizes mainly the Apennine chain; (ii) the time-correlated behaviour
of the seismicity is persistent, and this implies that the dynamics
underlying the seismic phenomenology is characterized by the presence of
&quot;positive feedback mechanisms&quot;; (iii) significant time correlation is not
simply related with the mainshock/aftershock mechanisms.</p>
</abstract>
<counts><page-count count="8"/></counts>
</article-meta>
</front>
<body/>
<back>
</back>
</article>