<?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>C. E. Hedge</dc:contributor>
  <dc:contributor>H.H. Thomas</dc:contributor>
  <dc:contributor>T.W. Stern</dc:contributor>
  <dc:creator>R. C. Pearson</dc:creator>
  <dc:date>1966</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Radiometric ages have been measured on&amp;nbsp;&lt;/span&gt;rocks&lt;span&gt;&amp;nbsp;of a crystalline terrane that includes ancient gneisses and migmatites, two granitic batholiths (&lt;/span&gt;St&lt;span&gt;.&amp;nbsp;&lt;/span&gt;Kevin&lt;span&gt;&amp;nbsp;&lt;/span&gt;Granite&lt;span&gt;&amp;nbsp;and&amp;nbsp;&lt;/span&gt;granite&lt;span&gt;&amp;nbsp;of Cross Creek), and various minor intrusive&amp;nbsp;&lt;/span&gt;rocks&lt;span&gt;. A whole-&lt;/span&gt;rock&lt;span&gt;&amp;nbsp;Rb-Sr isochron age on the&amp;nbsp;&lt;/span&gt;St&lt;span&gt;.&amp;nbsp;&lt;/span&gt;Kevin&lt;span&gt;&amp;nbsp;&lt;/span&gt;Granite&lt;span&gt;&amp;nbsp;establishes it as 1390 ± 60 m.y. old. Mineral ages on the&amp;nbsp;&lt;/span&gt;St&lt;span&gt;.&amp;nbsp;&lt;/span&gt;Kevin&lt;span&gt;&amp;nbsp;and numerous other&amp;nbsp;&lt;/span&gt;rocks&lt;span&gt;&amp;nbsp;are either about the same as the&amp;nbsp;&lt;/span&gt;St&lt;span&gt;.&amp;nbsp;&lt;/span&gt;Kevin&lt;span&gt;&amp;nbsp;whole-&lt;/span&gt;rock&lt;span&gt;&amp;nbsp;age or younger by as much as 200 m.y., even where the relative age is known to be older. Some minor&amp;nbsp;&lt;/span&gt;Precambrian&lt;span&gt;&amp;nbsp;intrusive masses that are probably younger than&amp;nbsp;&lt;/span&gt;St&lt;span&gt;.&amp;nbsp;&lt;/span&gt;Kevin&lt;span&gt;&amp;nbsp;&lt;/span&gt;Granite&lt;span&gt;&amp;nbsp;yield mica ages within analytical error of the&amp;nbsp;&lt;/span&gt;St&lt;span&gt;.&amp;nbsp;&lt;/span&gt;Kevin&lt;span&gt;&amp;nbsp;age, indicating that these&amp;nbsp;&lt;/span&gt;rocks&lt;span&gt;&amp;nbsp;can be younger than the&amp;nbsp;&lt;/span&gt;granite&lt;span&gt;&amp;nbsp;by only a few tens of millions of years. The mica ages, both Rb-Sr and K-Ar, are thought to be minimal, but a K-Ar age of 2020 m.y. on horn-blende probably reflects excess argon. Mica ages from all&amp;nbsp;&lt;/span&gt;rocks&lt;span&gt;&amp;nbsp;known geologically to be older than&amp;nbsp;&lt;/span&gt;St&lt;span&gt;.&amp;nbsp;&lt;/span&gt;Kevin&lt;span&gt;&amp;nbsp;&lt;/span&gt;Granite&lt;span&gt;&amp;nbsp;are low and are interpreted as heating ages reflecting intrusion of the&amp;nbsp;&lt;/span&gt;granite&lt;span&gt;, in some cases modified further by heating during Laramide time. In this area,&amp;nbsp;&lt;/span&gt;Precambrian&lt;span&gt;&amp;nbsp;intrusion and deformation had largely ended by 1200 or 1300 m.y. ago. Plutonism, represented here by the&amp;nbsp;&lt;/span&gt;St&lt;span&gt;.&amp;nbsp;&lt;/span&gt;Kevin&lt;span&gt;&amp;nbsp;&lt;/span&gt;Granite&lt;span&gt;&amp;nbsp;and elsewhere by the Silver Plume and other granites, probably accounts for the numerous mineral ages of about 1300 m.y. previously reported from&amp;nbsp;&lt;/span&gt;Colorado&lt;span&gt;&amp;nbsp;although weak regional metamorphism may also have been a factor.&amp;nbsp;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/0016-7606(1966)77[1109:GOTSKG]2.0.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Geological Society of America</dc:publisher>
  <dc:title>Geochronology of the St. Kevin granite and neighboring precambrian rocks, northern Sawatch Range, Colorado</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>