<?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:creator>Eric R. Force</dc:creator>
  <dc:date>1975</dc:date>
  <dc:description>&lt;p&gt;Titanium minerals in amounts equivalent to a significant portion of present world production are moved but not recovered from mines of other commodities. Resources of this type total in the millions of tons of contained TiO&lt;sub&gt;2&lt;/sub&gt;. Among the possible sources for byproduct titanium are (1) ilnenite and minor rutile detrital concentrations in deposits of tin, monazite, phosphate, gold, platinum, uranium, and sand andgravel; (2) leucoxenitized ilmenite and, locally, rutile in some 13 bauxites; (3) rutilo in porphyry copper and related deposits; (14) 14 rutile in kyanite deposits; and (5) perovskite and other titanium minerals in deposits of niobium, apatite, and nepheline in nepheline syenites.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr7534</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Titanium minerals in deposits of other minerals</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>