<?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>P. B. Barton Jr.</dc:contributor>
  <dc:contributor>G. Kullerud</dc:contributor>
  <dc:creator>Brian J. Skinner</dc:creator>
  <dc:date>1959</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Redeterminations of the relation between the composition and unit-cell size of Fe-bearing sphalerites, necessitated because of partial oxidation of the FeS sample used in earlier measurements, are presented. It is noted that the Fe-ZnS solvus curve may also require revision and should be used with caution, particularly for temperature determinations in the higher ranges.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.2113/gsecongeo.54.6.1040</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>GeoScienceWorld</dc:publisher>
  <dc:title>Effect of FeS on the unit cell edge of sphalerite, a revision</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>