<?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>D. D. Eberl</dc:contributor>
  <dc:creator>G. Whitney</dc:creator>
  <dc:date>1982</dc:date>
  <dc:description>The talc-like gel was treated between 300o and 550oC at 1 kbar for 7, 30, 50, 120 and 200 days. The trends suggest that stevensite and/or corrensite are the stable minerals at &lt;450oC. At 500o- 550oC, talc is stable.-K.A.R.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>Mineralogical Society of America</dc:publisher>
  <dc:title>Mineral paragenesis in the talc-water experimental hydrothermal system.</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>