<?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>A.W. Langer</dc:contributor>
  <dc:creator>Thomas A. Ryer</dc:creator>
  <dc:date>1980</dc:date>
  <dc:description>&lt;div&gt;&lt;div id="12458224" class="article-section-wrapper js-article-section js-content-section  " data-section-parent-id="0"&gt;&lt;p&gt;The ratio of the thicknesses of a layer of peat and the coal bed formed from that peat has been calculated for a bituminous coal bed in central Utah. The method used involves comparison of the thickness of peat eroded by a laterally migrating channel system with the thickness of coal now absent from the outcrop. The peat:coal thickness ratio calculated by this method is approximately 11:1.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1306/212F7B44-2B24-11D7-8648000102C1865D</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>SEPM</dc:publisher>
  <dc:title>Thickness change involved in the peat-to- coal transformation for a bituminous coal of Cretaceous age in central Utah</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>