<?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>A.R. Kinkel Jr.</dc:creator>
  <dc:date>1962</dc:date>
  <dc:description>&lt;p&gt;&lt;span class="ScopusTermHighlight"&gt;Massive&lt;/span&gt;&lt;span&gt;&amp;nbsp;and disseminated pyrrhotite-chalcopyrite-pyrite&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;ore&lt;/span&gt;&lt;span&gt;&amp;nbsp;replaced a fault zone in Precambrian&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;Carolina&lt;/span&gt;&lt;span&gt;&amp;nbsp;Gneiss of Keith (1). Closely following&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;sulfide&lt;/span&gt;&lt;span&gt;&amp;nbsp;deposition, vein sulfides and silicates in the wall rock were&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;recrystallized&lt;/span&gt;&lt;span&gt;&amp;nbsp;under a rising temperature gradient to coarse-grained unoriented aggregates that contain late pyrite porphyroblasts in pyrrhotite. Boudinage, dilation, and flow structures are common.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.2113/gsecongeo.57.7.1116</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Society of Economic Geologists</dc:publisher>
  <dc:title>The ore knob massive sulfide copper deposit, North Carolina: An example of recrystallized ore</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>