<?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>Norbert Lee Archbold</dc:creator>
  <dc:date>1956</dc:date>
  <dc:description>&lt;p&gt;This study was made to determine whether any relationship exists between lithology or vanadium-uranium deposits and calcium carbonate content in the Salt Wash member of the Morrison formation of Jurassic age. Results indicate that altered gray-green mudstone contains less carbonate than does unaltered red-brown mudstone. No significant difference exists between the carbonate content of unaltered light red sandstone and altered light gray sandstone. Within the sandstone there are carbonate-rich zones adjacent to contacts with mudstone. Calcium carbonate content and ore grade are not related, although carbonate-rich zones parallel the ore bodies. These carbonate-rich zones may possibly be used as an ore guide. The present distribution of calcium carbonate could have resulted from early diagenesis with later redistribution during mineralization.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr562</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Relationships of calcium carbonate to lithology and vanadium-uranium deposits in Salt Wash sandstone of southwestern Colorado</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>