<?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>J.P. Bradbury</dc:contributor>
  <dc:contributor>R. M. Forester</dc:contributor>
  <dc:contributor>G. Singh</dc:contributor>
  <dc:contributor>R.S. Sternberg</dc:contributor>
  <dc:creator>Vera Markgraf</dc:creator>
  <dc:date>1984</dc:date>
  <dc:description>Paleomagnetic analysis of samples from the original 600-m-long core from the San Agustin Plains, New Mexico, showed an unquestionable reversal stratigraphy dating the record back to at least 1.6 my. Analysis of pollen, ostracodes, and algae of a duplicate sample section in the vicinity of the original coring site and spanning the last 18,000 yr B.P. shows a much higher resolution than the earlier results. ?? 1984.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/0033-5894(84)90027-9</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>San Agustin Plains, New Mexico: Age and paleoenvironmental potential reassessed</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>