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<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>8</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/nhess-8-123-2008</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/8/123/2008/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/8/123/2008/nhess-8-123-2008.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/8/123/2008/nhess-8-123-2008.pdf</fulltext_pdf>
	<start_page>123</start_page>
	<end_page>128</end_page>
	<publication_date>2008-02-25</publication_date>
	<article_title content_type="html">Electrical precursors of earthquakes in Aegean Sea during the last decade (1997&amp;ndash;2007)</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. Dologlou</name>
			<email>edologl@phys.uoa.gr</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>V. Hadjicontis</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>C. Mavromatou</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Solid State Section, Department of Physics, University of Athens, Panepistimiopolis, Zografos 157 84 Athens, Greece</affiliation>
	</affiliations>
	<abstract content_type="html">The purpose of this study is to investigate some properties of the Seismic
Electric Signals (SES) that preceded large earthquakes which occurred in the
Aegean Sea (24&amp;ndash;27)&amp;deg; E, (37&amp;ndash;40)&amp;deg; N, during the last decade.
Our main interest is focused on the important parameter of the lead time
&amp;Delta;&lt;I&gt;t&lt;/I&gt;, which is the time difference between the occurrence of the
earthquake and the detection of the associated SES signal. Two groups of
lead times, a short (i.e. &amp;Delta;&lt;I&gt;t&lt;/I&gt;~ some weeks) and a long one
(&amp;Delta;&lt;I&gt;t&lt;/I&gt;~ some months) have been observed. We examine whether this
difference could be related to the regional tectonics. Furthermore the
property of SES selectivity is discussed.</abstract>
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