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<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>L.J. Patrick Muffler</dc:contributor>
  <dc:contributor>Michael A. Clynne</dc:contributor>
  <dc:contributor>Duane E. Champion</dc:contributor>
  <dc:creator>Brent D. Turrin</dc:creator>
  <dc:date>2007</dc:date>
  <dc:description>&lt;p&gt;&lt;sup&gt;40&lt;/sup&gt;&lt;span&gt;Ar/&lt;/span&gt;&lt;sup&gt;39&lt;/sup&gt;&lt;span&gt;Ar ages on the Hat Creek Basalt (HCB) and stratigraphically related lava flows show that latest Pleistocene tholeiitic basalt with very low K&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O can be dated reliably. The HCB underlies &amp;sim;&amp;nbsp;15&amp;nbsp;ka glacial gravel and overlies four andesite and basaltic andesite lava flows that yield&amp;nbsp;&lt;/span&gt;&lt;sup&gt;40&lt;/sup&gt;&lt;span&gt;Ar/&lt;/span&gt;&lt;sup&gt;39&lt;/sup&gt;&lt;span&gt;Ar ages of 38&amp;nbsp;&amp;plusmn;&amp;nbsp;7&amp;nbsp;ka (Cinder Butte; 1.65% K&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O), 46&amp;nbsp;&amp;plusmn;&amp;nbsp;7&amp;nbsp;ka (Sugarloaf Peak; 1.85% K&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O), 67&amp;nbsp;&amp;plusmn;&amp;nbsp;4&amp;nbsp;ka (Little Potato Butte; 1.42% K&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O) and 77&amp;nbsp;&amp;plusmn;&amp;nbsp;11&amp;nbsp;ka (Potato Butte; 1.62% K&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O). Given these firm age brackets, we then dated the HCB directly. One sample (0.19% K&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O) clearly failed the criteria for plateau-age interpretation, but the inverse isochron age of 26&amp;nbsp;&amp;plusmn;&amp;nbsp;6&amp;nbsp;ka is seductively appealing. A second sample (0.17% K&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O) yielded concordant plateau, integrated (total fusion), and inverse isochron ages of 26&amp;nbsp;&amp;plusmn;&amp;nbsp;18, 30&amp;nbsp;&amp;plusmn;&amp;nbsp;20 and 24&amp;nbsp;&amp;plusmn;&amp;nbsp;6&amp;nbsp;ka, all within the time bracket determined by stratigraphic relations; the inverse isochron age of 24&amp;nbsp;&amp;plusmn;&amp;nbsp;6&amp;nbsp;ka is preferred. As with all isotopically determined ages, confidence in the results is significantly enhanced when additional constraints imposed by other isotopic ages within a stratigraphic context are taken into account.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.yqres.2007.02.004</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Robust 24 ± 6 ka &lt;sup&gt;40&lt;/sup&gt;Ar/&lt;sup&gt;39&lt;/sup&gt;Ar age of a low-potassium tholeiitic basalt in the Lassen region of NE California</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>