<?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>John Hillhouse</dc:contributor>
  <dc:contributor>Robert J. Fleck</dc:contributor>
  <dc:contributor>David M. Miller</dc:contributor>
  <dc:contributor>David C. Buesch</dc:contributor>
  <dc:contributor>Andrew J. Cyr</dc:contributor>
  <dc:contributor>Kevin M. Schmidt</dc:contributor>
  <dc:creator>Geoffrey Phelps</dc:creator>
  <dc:date>2017</dc:date>
  <dc:description>To add to the regional paleomagnetic data documenting block rotation in eastern California, we determined the age and paleomagnetic rotation of the Broadwell Mesa basalt, a basalt in the Bristol Mountains, CA as part of an effort to constrain the timing and rotation of blocks adjacent to the fault. The east-striking sinistral Broadwell Mesa fault cuts and separates the basalt into two outcrops. An 40Ar/39Ar  date from the northern outcrop yields an age of 5.46 ± 0.04 Ma. Two sites consisting of 40 paleomagnetic cores from the basalt indicate the basalt is reversely magnetized and that there has been no significant rotation (&lt; 11º) between the two basalt outcrops.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>Desert Studies Center, California State University at Fullerton</dc:publisher>
  <dc:title>Analysis of the age and paleomagnetic orientation of the Broadwell Mesa Basalt, Bristol Mountains, CA</dc:title>
  <dc:type>text</dc:type>
</oai_dc:dc>