<?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>G. Brent Dalrymple</dc:contributor>
  <dc:contributor>Robert L. Smith</dc:contributor>
  <dc:creator>Marvin A. Lanphere</dc:creator>
  <dc:date>1975</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Rhyolite domes and rhyolite and basalt flows near Coso Hot Springs in the Coso Range, California, give K-Ar ages that range from about 0.04 ± 0.02 m.y. to 0.96 ± 0.19 m.y. Most of the units appear to be between 0.05 and 0.15 m.y. old. The total volume of erupted rhyolitic magma is about 2.4 km&lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;. The age, volume, and composition of these volcanic rocks indicate that the Coso volcanic field is a potential geothermal resource area.&amp;nbsp;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/0091-7613(1975)3&lt;339:KAOPRV&gt;2.0.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>GeScience World</dc:publisher>
  <dc:title>K-Ar ages of Pleistocene rhyolitic volcanism in the Coso Range, California</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>