<?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>Bradley S. Van Gosen</dc:contributor>
  <dc:contributor>Nora K. Foley</dc:contributor>
  <dc:creator>Gilpin R. Robinson Jr.</dc:creator>
  <dc:date>2006</dc:date>
  <dc:description>This presentation on the geology of ultramafic-hosted talc-magnesite deposits was given at the 42nd Forum on the Geology of Industrial Minerals, May 7-13, 2006, in Asheville, North Carolina (USA). Talc is a soft inert industrial mineral commodity commonly used as a component or filler in ceramic, paint, paper, plastic, roofing, and electrical applications. Ultramafic-hosted talc-magnesite deposits are important sources of talc. </dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr20061229</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Geological Survey (U.S.)</dc:publisher>
  <dc:title>Ultramafic-Hosted Talc-Magnesite Deposits</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>