<?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>E-An Zen</dc:creator>
  <dc:date>1965</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;The solubilities&amp;nbsp;&lt;/span&gt;in&lt;span&gt;&amp;nbsp;the&amp;nbsp;&lt;/span&gt;system&lt;span&gt;&amp;nbsp;CaSO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;span&gt;-&lt;/span&gt;NaCl&lt;span&gt;-H&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O,&amp;nbsp;&lt;/span&gt;at&lt;span&gt;&amp;nbsp;1 atm&amp;nbsp;&lt;/span&gt;pressure&lt;span&gt;&amp;nbsp;and&amp;nbsp;&lt;/span&gt;35°&lt;span&gt;,&amp;nbsp;&lt;/span&gt;50°&lt;span&gt;, and 70°C, have been determined by approaching the&amp;nbsp;&lt;/span&gt;solubility&lt;span&gt;&amp;nbsp;curves from both the undersaturation and supersaturation sides. The experimental runs are of long duration, as much as 3 months; these rates should be commensurate with those of the appropriate geological processes, and so the results should be directly applicable to the interpretation of evaporite deposits.&amp;nbsp;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1093/petrology/6.1.124</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Oxford University Press</dc:publisher>
  <dc:title>Solubility measurements in the system CaSO4-NaCL-H2O at 35°, 50°, and 70°cand one atmosphere pressure</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>