<?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>Michael R. Elliot</dc:contributor>
  <dc:contributor>Thomas D. Gilmore</dc:contributor>
  <dc:contributor>Robert K. Mark</dc:contributor>
  <dc:contributor>Evelyn B. Newman</dc:contributor>
  <dc:contributor>John C. Tinsley III</dc:contributor>
  <dc:contributor>D.D. Jackson</dc:contributor>
  <dc:contributor>W.B. Lee</dc:contributor>
  <dc:contributor>C.-C. Liu</dc:contributor>
  <dc:creator>Robert O. Castle</dc:creator>
  <dc:date>1981</dc:date>
  <dc:description>&lt;p&gt;We disagree with several of the arguments cited by Jackson &lt;i&gt;et al&lt;/i&gt;. in support of their view that "the inference of wide-spread aseismic uplift in southern California is not justified" (1). Specifically, the striking correlation shown in figure 1 of Jackson &lt;i&gt;et al&lt;/i&gt;. (1) is an artifact of the construction, the rod calibration data are atypical, the cited regression techniques are of doubtful value, and the geologically and geodetically determined uplift rates are inappropriately compared.&lt;br&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.213.4504.246</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Association for the Advancement of Science</dc:publisher>
  <dc:title>Aseismic uplift in California</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>