<?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>Karen Lund</dc:contributor>
  <dc:contributor>Snir Attia</dc:contributor>
  <dc:contributor>Jonathan Andrew Funk</dc:contributor>
  <dc:contributor>Kyle Eastman</dc:contributor>
  <dc:contributor>Joshua Mark Rosera</dc:contributor>
  <dc:contributor>Jonathan Saul Caine</dc:contributor>
  <dc:contributor>Eric D. Anderson</dc:contributor>
  <dc:creator>Sean Patrick Gaynor</dc:creator>
  <dc:date>2025</dc:date>
  <dc:description>&lt;p&gt;Tertiary ore deposits in the Rocky Mountains physiographic province primarily formed through magmatic-hydrothermal processes associated with shifting tectonics and lithospheric conditions. Important deposit types in the province are calc-alkaline and Climaxtype porphyry; high-, medium-, and low-sulfidation epithermal; alkalic magmatic; carbonate replacement; tungsten skarn and vein; and sandstone uranium. Province wide, there is diachroneity from north to south among both ore-forming and magmatic events.&amp;nbsp;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>Society for Geology Applied to Mineral Deposits</dc:publisher>
  <dc:title>Tertiary metallogeny of the Rocky Mountains Province, USA</dc:title>
  <dc:type>text</dc:type>
</oai_dc:dc>