<?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>D. R. Wones</dc:creator>
  <dc:date>1967</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Phlogopite reacts to form orthorhombic kalsilite, leucite, forsterite and fluid (H&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O) at 1012 ± 7°&lt;/span&gt;&lt;i&gt;C&lt;/i&gt;&lt;span&gt;, 400 bars pressure, and 905 ± 5°&lt;/span&gt;&lt;i&gt;C&lt;/i&gt;&lt;span&gt;&amp;nbsp;at 100 bars pressure. The heat of reaction is 39 ± 4 kcal compared to 44 ± 6kcal for the reaction of annite to form orthorhombic kalsilite, leueite, fayalite and fluid (H&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O). The results are consistent with earlier experiments, but not with the interpretations of those experiments.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/0016-7037(67)90064-6</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>A low pressure investigation of the stability of phlogopite</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>