<?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. L. Graf</dc:contributor>
  <dc:contributor>B.F. Jones</dc:contributor>
  <dc:creator>R.J. Anderson</dc:creator>
  <dc:date>1966</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;The linear relation observed in a log Ca&lt;/span&gt;&lt;sup&gt;++&lt;/sup&gt;&lt;span&gt;&amp;nbsp;versus log Br&lt;/span&gt;&lt;sup&gt;-&lt;/sup&gt;&lt;span&gt;&amp;nbsp;plot for subsurface Cl&lt;/span&gt;&lt;sup&gt;-&lt;/sup&gt;&lt;span&gt;&amp;nbsp;waters is attributed to ultrafiltration by shale of sea water and fresh water that have passed through sedimentary rocks since their formation. Reactions between these solutions and sedimentary minerals, particularly dolomitization, must have contributed additional Ca&lt;/span&gt;&lt;sup&gt;++&lt;/sup&gt;&lt;span&gt;&amp;nbsp;to solution.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.153.3744.1637</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Association for the Advancement of Science</dc:publisher>
  <dc:title>Calcium and bromide contents of natural waters</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>