<?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>Ronald C. Johnson</dc:contributor>
  <dc:creator>Vito F. Nuccio</dc:creator>
  <dc:date>1986</dc:date>
  <dc:description>&lt;p&gt;The ability of rock to generate oil and gas is directly related to the type and quantity of kerogen and to its thermal maturity; therefore, thermal maturity is a commonly used tool for oil and gas exploration. &amp;nbsp;The purpose of this study ws to provide a thermal-maturity map for the lower part of the Upper Cretaceous Mesaverde Group in the eastern part of the Uinta Basin. &amp;nbsp;Prior to this study, thermal-maturity data were not available for the Uinta Basin. &amp;nbsp;This study uses coal rank to show the thermal maturity of the associated rocks. &amp;nbsp;The map was prepared in cooperation with the U.S. Department of Energy under its western gas sands project.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/mf1842</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Thermal maturity map of the lower part of the Upper Cretaceous Mesaverde Group, Uintah Basin, Utah</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>