<?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>Carol A. Finn</dc:contributor>
  <dc:contributor>Eric D. Anderson</dc:contributor>
  <dc:contributor>Dwight Bradley</dc:contributor>
  <dc:contributor>Mohamed Joud</dc:contributor>
  <dc:contributor>Ahmed Taleb Mohamed</dc:contributor>
  <dc:contributor>John D. Horton</dc:contributor>
  <dc:contributor>Craig A. Johnson</dc:contributor>
  <dc:contributor>Mohammed Bouabdellah</dc:contributor>
  <dc:contributor>John F. Slack</dc:contributor>
  <dc:creator>Cliff D. Taylor</dc:creator>
  <dc:date>2016</dc:date>
  <dc:description>&lt;p&gt;High-grade hematitic iron ores (of HIF, containing 60-65 wt%Fe) have been mined in Mauritania since 1952 from Superior-type iron deposits of the F'derik-Zouerate district. &amp;nbsp;Depletion of the high-grade ores in recent years has resulted in new exploration projects focused on lower-grade magnetite ores occurring in Algoma-type banded iron formation (of BIF, containing ca. 35 wt% Fe). &amp;nbsp;Mauritania is the seventeenth largest iron producer in the world and currently has about 1.1 Gt of crude iron ore reserves.&amp;nbsp;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/978-3-319-31733-5</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer</dc:publisher>
  <dc:title>The F'derik-Zouerate iron district: Mesoarchean and Paleoproterozoic iron formation of the Tiris Complex, Islamic Republic of Mauritania</dc:title>
  <dc:type>chapter</dc:type>
</oai_dc:dc>