<?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>J. Fitzpatrick</dc:creator>
  <dc:date>1986</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Florencite-(Nd) [(Nd,Ce)Al&lt;/span&gt;&lt;span class="sub"&gt;3&lt;/span&gt;&lt;span&gt;(PO&lt;/span&gt;&lt;span class="sub"&gt;4&lt;/span&gt;&lt;span&gt;)&lt;/span&gt;&lt;span class="sub"&gt;2&lt;/span&gt;&lt;span&gt;(OH)&lt;/span&gt;&lt;span class="sub"&gt;6&lt;/span&gt;&lt;span&gt;], was first described by Milton and Bastron (1971) from fracture surfaces in weathered cherts of the Franciscan Complex, south of Sausalito in Marin County, California. Florencite-(Nd) occurred there as a moderate-brown pulverulent earthy material; individual crystals were not discernible under microscopic examination. A semi-quantitative spectrographic analysis showed the presence of Nd (3 wt. %) and Ce (0.5 wt. %). No powder data for florencite-(Nd) exists in the current powder diffraction file.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1017/S0885715600012021</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Cambridge University Press</dc:publisher>
  <dc:title>Powder X-ray diffraction of florencite-(Nd)</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>