<?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>T. S. Presser</dc:contributor>
  <dc:contributor>M. Saines</dc:contributor>
  <dc:contributor>P. Dickson</dc:contributor>
  <dc:contributor>A. F. K. Van Groos</dc:contributor>
  <dc:creator>I. Barnes</dc:creator>
  <dc:date>1982</dc:date>
  <dc:description>&lt;div id="abstracts" class="Abstracts u-font-serif"&gt;&lt;div id="aep-abstract-id6" class="abstract author"&gt;&lt;div id="aep-abstract-sec-id7"&gt;&lt;p id="simple-para.0010"&gt;Highly-alkaline (pH &amp;gt; 12.5) meteoric waters of a Ca&lt;sup&gt;2+&lt;/sup&gt;OH&lt;sup&gt;−&lt;/sup&gt;-type issue from naturally calcined bituminous marl. The cold (16.5 ≤&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;T&lt;/i&gt;(°C) ≤ 19.1) waters are super-saturated with minerals thought to be of high-temperature origin.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/0009-2541(82)90024-9</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Geochemistry of highly basic calcium hydroxide groundwater in Jordan</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>