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<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>Jay M. Thompson</dc:contributor>
  <dc:creator>Amanda Souders</dc:creator>
  <dc:date>2025</dc:date>
  <dc:description>&lt;p&gt;Re-Os geochronology is a powerful tool to directly date sulphide mineralisation using phases such as molybdenite, pyrite and chalcopyrite. We present a snapshot of a method in development utilizing laser ablation inductively coupled-plasma ‘triple quad’ mass spectrometry (LA-ICP-MS/MS) for Re-Os geochronology of molybdenite. While traditional LA-(MC)-ICP-MS measurements are limited by the &amp;gt;90% isobaric interference correction of parent radioactive &lt;sup&gt;187&lt;/sup&gt;Re on radiogenic daughter &lt;sup&gt;187&lt;/sup&gt;Os, the MS/MS technology minimizes this correction through careful instrument tuning and use of a (CH&lt;sub&gt;4&lt;/sub&gt; + H&lt;sub&gt;2&lt;/sub&gt; + He) reaction gas mixture to mass shift &lt;sup&gt;187&lt;/sup&gt;Os away from &lt;sup&gt;187&lt;/sup&gt;Re. We demonstrate the potential of the MS/MS technique by presenting robust Re-Os dates for three different molybdenite samples ranging in age from ~28 to 1520 Ma.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>Society for Geology Applied to Mineral Deposits (SGA)</dc:publisher>
  <dc:title>Re-Os geochronology of molybdenite by LA-ICP-MS/MS</dc:title>
  <dc:type>text</dc:type>
</oai_dc:dc>