<?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. L. Wesson</dc:contributor>
  <dc:contributor>W.L. Ellsworth</dc:contributor>
  <dc:creator>R. Robinson</dc:creator>
  <dc:date>1974</dc:date>
  <dc:description>Residuals for P-wave traveltimes at a seismograph station near Bear Valley, California, for small, precisely located local earthquakes at distances of 20 to 70 kilometers show a sharp increase of nearly 0.3 second about 2 months before a magnitude 5.0 earthquake that occurred within a few kilometers of the station. This indicates that velocity changes observed elsewhere premonitory to earthquakes, possibly related to dilatancy, occur along the central section of the San Andreas fault system.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.184.4143.1281</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Association for the Advancement of Science</dc:publisher>
  <dc:title>Variation of P-wave velocity before the Bear Valley, California, earthquake of 24 February 1972</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>