<?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>T.V. McEvilly</dc:contributor>
  <dc:creator>W. H. Bakun</dc:creator>
  <dc:date>1979</dc:date>
  <dc:description>Moderate-sized earthquakes (Richter magnitude ML 5 1/2) have occurred four times this century (1901, 1922, 1934, and 1966) on the San Andreas fault near Parkfield in central California. In many respects the June 1966 sequence was a remarkably detailed repetition of the June 1934 sequence, suggesting a recurring recognizable pattern of stress and fault zone behavior.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.205.4413.1375</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Association for the Advancement of Science</dc:publisher>
  <dc:title>Earthquakes near Parkfield, California: Comparing the 1934 and 1966 sequences</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>