<?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>Michael T. Styles</dc:contributor>
  <dc:contributor>Cliff D. Taylor</dc:contributor>
  <dc:contributor>Roger M. Key</dc:contributor>
  <dc:contributor>Wilfried Bauer Wilfried</dc:contributor>
  <dc:contributor>A Vonimanitra Ralison Vonimanitra</dc:contributor>
  <dc:creator>Peter E. J Pitfield</dc:creator>
  <dc:date>2009</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Microchemical characterisation of bedrock and placer gold grains from six gold districts within the Archaean domains and intervening Neoproterozoic Anaboriana-Manampotsy belt of northern and east-central Madagascar show few opaque inclusions (e.g pyrrhotite, Bi tellurides) but wide range of Ag contents (40wt%). Some districts exhibit multiple source populations of grains. The &amp;lsquo;greenstone belt&amp;rsquo; terranes have an orogenic gold signature locally with an intrusion-related to epithermal overprint. Proterozoic metasediments with felsic to ultramafic bodies yield dominantly intrusion-related gold. A high proportion of secondary gold (&amp;lt;0.5wt% Ag) is related to recycling of paleoplacers and erosion of post-Gondwana planation surfaces and indicates that some mesothermal gold systems were already partially to wholly removed by erosion by the PermoTriassic.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>James Cook University School of Earth &amp; Environmental Studies. Economic Geology Research Unit</dc:publisher>
  <dc:title>Gold deposit styles and placer gold characterisation in northern and east-central Madagascar</dc:title>
  <dc:type>text</dc:type>
</oai_dc:dc>