<?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.H. Richter</dc:contributor>
  <dc:creator>K. J. Murata</dc:creator>
  <dc:date>1961</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Petrographic and chemicoal studies of a suite of rocks from the&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;Uwekahuna&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;laccolith&lt;/span&gt;&lt;span&gt;&amp;nbsp;of&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;Kilauea&lt;/span&gt;&lt;span&gt;&amp;nbsp;Volcano show that the original mafic tholeiitic magma differentiated into tholeiitic picrite, tholeiitic olivine gabbro, and an aphanitic rock approaching quartz-basalt&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;composition. Mechanisms involved were an initial gravity settling of olivine and a final filter pressing of the residual liquid. The range of composition represented by the rocks of the&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;laccolith&lt;/span&gt;&lt;span&gt;&amp;nbsp;is as great as that found among all hitherto analysed lavas of the volcano.&amp;nbsp;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1093/petrology/2.3.424</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Oxford University Press</dc:publisher>
  <dc:title>Magmatic differentiation in the Uwekahuna Laccolith, Kilauea Caldera, Hawaii</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>