<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>R.A. Harris</dc:contributor>
  <dc:creator>D.J. Andrews</dc:creator>
  <dc:date>2005</dc:date>
  <dc:description>A particular solution for slip on an interface between different elastic materials, the wrinkle-like slip pulse, propagates in only one direction with reduced normal compressive stress. More general solutions, and natural earthquakes, need not share those properties. In a 3D dynamic model with a drop in friction and heterogeneous initial stress, the wrinkle-like slip pulse is only a small part of the solution. Rupture propagation is determined primarily by the potential stress drop, not by the wrinkle-like slip pulse. A 2D calculation with much finer resolution shows that energy loss to friction might not be significantly reduced in the wrinkle-like slip pulse. Copyright 2005 by the American Geophysical Union.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1029/2005GL023996</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>The wrinkle-like slip pulse is not important in earthquake dynamics</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>