<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" 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:title>Multistage gold deposition in the Archaean Maria Lazara gold deposit (Goias, Brazil)</dc:title>
  <dc:creator>Michel, D.</dc:creator>
  <dc:creator>/Giuliani, Gaston</dc:creator>
  <dc:creator>Pulz, G.M.</dc:creator>
  <dc:creator>Jost, H.</dc:creator>
  <dc:subject>GEOCHIMIE</dc:subject>
  <dc:subject>OR</dc:subject>
  <dc:subject>GITOLOGIE</dc:subject>
  <dc:subject>MINERALOGIE</dc:subject>
  <dc:subject>PARAGENESE</dc:subject>
  <dc:description>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. (R&#xE9;sum&#xE9; d'auteur)</dc:description>
  <dc:date>1994</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:41481</dc:identifier>
  <dc:identifier>fdi:41481</dc:identifier>
  <dc:identifier>Michel D., Giuliani Gaston, Pulz G.M., Jost H.. Multistage gold deposition in the Archaean Maria Lazara gold deposit (Goias, Brazil). 1994,  94-97</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>BRESIL</dc:coverage>
  <dc:coverage>GOIAS</dc:coverage>
</oai_dc:dc>
