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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>13</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/npg-13-409-2006</doi>
	<article_url>http://www.nonlin-processes-geophys.net/13/409/2006/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/13/409/2006/npg-13-409-2006.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/13/409/2006/npg-13-409-2006.pdf</fulltext_pdf>
	<start_page>409</start_page>
	<end_page>412</end_page>
	<publication_date>2006-08-11</publication_date>
	<article_title content_type="html">Fractal analysis for the ULF data during the 1993 Guam earthquake to study prefracture criticality</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Y. Ida</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. Hayakawa</name>
			<email>hayakawa@whistler.ee.uec.ac.jp</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Electronic Engineering, The University of Electro-Communications, 1-5-1 Chofugaoka, Chofu, Tokyo, 182-8585, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">An extremely large earthquake (with magnitude of 8.2) happened on
8 August 1993 near the Guam island, and ultra-low-frequency (ULF) (frequency
less than 1 Hz) electromagnetic fields were measured by 3-axis induction
magnetometers at an observing station (with the epicentral distance of 65 km)
with sampling frequency of 1 Hz. In order to study electromagnetic signature
of prefracture criticality, we have undertaken the fractal (mono-fractal)
analysis by means of the Higuchi&apos;s method for the ULF data during the 1993
Guam earthquake. Then, it is found that the fractal dimension exhibits five
maxima 99, 75, 52, 21, and 9&amp;ndash;4 days before the earthquake main shock, which
suggests the ULF electromagnetic signature of nonlinear evolution (in the
sense of self-organized criticality) taking place in the lithosphere just
before the 1993 large Guam earthquake. That is, there take place step-like
changes in the lithosphere during the long-term of the order of several
months before the main shock.</abstract>
	<references>
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</article>

