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  <titleInfo>
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    <title>granito Los Ratones como posible fuente de flúor en la formación de sistemas epitermales, Sierra de Fiambalá, Catamarca</title>
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  <name type="personal">
    <namePart>De La Hoz, Mauro</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Coniglio, Jorge</namePart>
  </name>
  <name type="personal">
    <namePart>Kirschbaum, Alicia</namePart>
  </name>
  <name type="corporate">
    <namePart>Instituto Superior de Correlación Geológica</namePart>
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  <note>Relevamiento: 2014.</note>
  <note>Artículo en pdf (SCG 30_2_77.pdf)</note>
  <subject>
    <topic>Fluor</topic>
  </subject>
  <subject>
    <topic>Granito</topic>
  </subject>
  <subject>
    <topic>Metalogénesis</topic>
  </subject>
  <subject>
    <topic>Sistema epitermal</topic>
  </subject>
  <subject authority="lcsh">
    <geographic>Catamarca</geographic>
  </subject>
  <subject authority="lcsh">
    <geographic>Plutón Los Ratones</geographic>
  </subject>
  <subject authority="lcsh">
    <geographic>Sierra De Fiambalá</geographic>
  </subject>
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    <titleInfo>
      <title>Serie Correlación Geológica. INSUGEO</title>
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    <identifier type="issn">1514-4186</identifier>
    <part>
      <text>vol.30, no.2, p.77-92</text>
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