<?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>Gary P. Landis</dc:contributor>
  <dc:creator>Albert H. Hofstra</dc:creator>
  <dc:date>2013</dc:date>
  <dc:description>Burlinson (2013) questions the veracity of the H&lt;sub&gt;2&lt;/sub&gt; concentrations reported for fluid inclusion extracts from minerals in the Idaho cobalt belt (Table 2; Landis and Hofstra, 2012) and suggests that they are an analytical artifact of electron-impact mass spectrometry. He also declares that H&lt;sub&gt;2&lt;/sub&gt; should not be present in fluid inclusions because it is invariably lost by diffusion and is never detected in fluid inclusions by laser Raman. We welcome this opportunity to reply and maintain that the reported H&lt;sub&gt;2&lt;/sub&gt; contents are accurate. Below we explain why Burlinson’s criticisms are invalid.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.2113/econgeo.108.5.1213</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>SEG</dc:publisher>
  <dc:title>Ore genesis constraints on the Idaho cobalt belt from fluid inclusion gas, noble gas isotope, and ion ratio analyses--a reply</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>