<?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:creator>Thomas M. Finn</dc:creator>
  <dc:date>2007</dc:date>
  <dc:description>Seventy-eight samples collected from marine shales from 
the Cretaceous Mowry Shale, the lower part of the Frontier 
Formation, and the lower shaly and upper sandy members 
of the Cody Shale in the Wind River Basin, Wyoming, were 
analyzed using Rock-Eval and total organic carbon analysis 
to determine the source rock potential. Results indicate 
that the Mowry Shale has a generative potential based on 
organic richness that is considered to be fair to very good, 
and hydrogen indices and S&lt;sub&gt;2&lt;/sub&gt;
/S&lt;sub&gt;3&lt;/sub&gt;
 ratios indicate a capability to 
generate both oil and gas. Maps of the Mowry indicate that 
it is most organic rich and oil-prone in the eastern part of the 
basin. Results of total organic carbon and Rock-Eval analyses 
for the Frontier Formation indicate that it is composed of 
mainly type III gas-prone kerogen, with organic richness 
levels that are generally poor to fair. Results of similar 
analyses of samples from the lower shaly member of the 
Cody Shale show a generative potential ranging from fair to 
excellent, and hydrogen indices and S&lt;sub&gt;2&lt;/sub&gt;
/S&lt;sub&gt;3&lt;/sub&gt;
 ratios indicate that 
it is capable of generating both oil and gas. Maps showing 
the distribution of kerogen types and organic richness for 
the lower shaly member of the Cody Shale are similar to the 
Mowry and show that lower shaly member of the Cody is 
more organic rich and more oil-prone in the eastern part of the 
basin. Analyses of samples of the upper sandy member of the 
Cody Shale indicate that it has little or no potential as a source 
rock. Thermal maturity mapping based on vitrinite reflectance 
measurements in the coal-bearing post-Cody Upper 
Cretaceous and Paleocene rocks shows that Upper Cretaceous 
marine shales in the deeper parts of the Wind River Basin are 
thermally mature to overmature with respect to hydrocarbon 
generation.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ds69J8</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological  Survey</dc:publisher>
  <dc:title>Source rock potential of upper cretaceous marine shales in the Wind River Basin, Wyoming: Chapter 8 in &lt;i&gt;Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming&lt;/i&gt;</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>