<?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>Bruce F. Houghton</dc:contributor>
  <dc:contributor>M. A. Lanphere</dc:contributor>
  <dc:contributor>I.A. Nairn</dc:contributor>
  <dc:creator>B.J. Hobden</dc:creator>
  <dc:date>1996</dc:date>
  <dc:description>New K-Ar age determinations indicate that the exposed portion of the Tongariro volcanic complex has grown steadily since at least 275 ka, with intervals of vigorous cone growth at 210-200.130-70. and 25 ka to the present day.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1080/00288306.1996.9514701</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Taylor and Francis</dc:publisher>
  <dc:title>Growth of the Tongariro volcanic complex: New evidence from K-Ar age determinations</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>