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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACLN : Articles dans des revues avec comité de lecture non répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="normal" font="default" size="100%">Michel, D.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Giuliani, Gaston</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Pulz, G.M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Jost, H.</style>
          </author>
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      <titles>
        <title>Multistage gold deposition in the Archaean Maria Lazara gold deposit (Goias, Brazil)</title>
        <secondary-title>Mineralium Deposita</secondary-title>
      </titles>
      <pages>94-97</pages>
      <keywords>
        <keyword>GEOCHIMIE</keyword>
        <keyword>OR</keyword>
        <keyword>GITOLOGIE</keyword>
        <keyword>MINERALOGIE</keyword>
        <keyword>PARAGENESE</keyword>
        <keyword>BRESIL</keyword>
        <keyword>GOIAS</keyword>
        <keyword>MARIA LAZARA REGION</keyword>
      </keywords>
      <dates>
        <year>1994</year>
      </dates>
      <call-num>fdi:41481</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Mineralium Deposita</full-title>
      </periodical>
      <isbn>0026-4598</isbn>
      <number>29</number>
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          <url>https://www.documentation.ird.fr/hor/fdi:41481</url>
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      <abstract>The Maria Lazara gold deposit in the Archaean Guarinos greenstone belt, central Brazil, consists of quartz-carbonate veins formed in a ductile shear zone. Study of the sulphides and gold-bearing quartz-carbonate veins and veinlets of the potassic hydrothermal alteration zone reveals two stages of ore paragenesis. The first stage corresponds to S-rich arsenopyrite deposition and the second one to the precipitation of As-rich arsenopyrite and Bi-Te-Au-S phases. Modes of occurrence, textures and Ag contents of native gold define two types of gold. The first type is native gold with Ag contents greater than 5 wt % postdating the S-rich arsenopyrites. The second type has Ag contents less than 3 wt % and is contemporaneous with Bi-Te-S phases. (Résumé d'auteur)</abstract>
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