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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>6</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/npg-13-681-2006</doi>
	<article_url>http://www.nonlin-processes-geophys.net/13/681/2006/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/13/681/2006/npg-13-681-2006.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/13/681/2006/npg-13-681-2006.pdf</fulltext_pdf>
	<start_page>681</start_page>
	<end_page>693</end_page>
	<publication_date>2006-12-12</publication_date>
	<article_title content_type="html">Oscillations in critical shearing, application to fractures in glaciers</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Pralong</name>
			<email>pralong@vaw.baug.ethz.ch</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratory of Hydraulics, Hydrology and Glaciology, Swiss Federal Institute of Technology, 8092 Zürich, Switzerland</affiliation>
	</affiliations>
	<abstract content_type="html">Many evidences of oscillations accompanying the acceleration of critical
  systems have been reported. These oscillations are usually related to
  discrete scale invariance properties of the systems and exhibit a
  logarithmic periodicity. In this paper we propose another explanation for
  these oscillations in the case of shearing fracture. Using a continuum
  damage model, we show that oscillations emerge from the anisotropic
  properties of the cracks in the shearing fracture zone. These oscillations
  no longer exhibit a logarithmic but rather a power-law periodicity. The
  power-periodic oscillation is a more general formulation. Its reduces to a
  log-periodic oscillation when the exponent of the power-law
  equals one. We apply this model to fit the measured displacements of
  unstable ice masses of hanging glaciers for which data are available.
  Results show that power-periodic oscillations adequately fit the
  observations.</abstract>
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</article>

