1 Ocak 2021 Dergi makalesi Açık Erişim

Kahya, Asuman; Kuscu, Ercan; Yenice, Firdevs Irem

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  <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/239038</identifier>
  <creators>
    <creator>
      <creatorName>Kahya, Asuman</creatorName>
      <givenName>Asuman</givenName>
      <familyName>Kahya</familyName>
      <affiliation>Gen Directorate Mineral Res &amp; Explorat, TR-06800 Ankara, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Kuscu, Ercan</creatorName>
      <givenName>Ercan</givenName>
      <familyName>Kuscu</familyName>
      <affiliation>Demir Export AS, TR-06800 Ankara, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Yenice, Firdevs Irem</creatorName>
      <givenName>Firdevs Irem</givenName>
      <familyName>Yenice</familyName>
      <affiliation>Gen Directorate Mineral Res &amp; Explorat, TR-06800 Ankara, Turkey</affiliation>
    </creator>
  </creators>
  <titles>
    <title>Genesis Of The Zebra Dolomites And Relation To Carbonate - Hosted Au - Ag - Zn +/- Pb Deposits In The Maden Village (Ulukisla - Nigde), Central Taurides, South Turkey</title>
  </titles>
  <publisher>Aperta</publisher>
  <publicationYear>2021</publicationYear>
  <dates>
    <date dateType="Issued">2021-01-01</date>
  </dates>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/239038</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.19111/bulletinofmre.877977</relatedIdentifier>
  </relatedIdentifiers>
  <rightsList>
    <rights rightsURI="http://www.opendefinition.org/licenses/cc-by">Creative Commons Attribution</rights>
    <rights rightsURI="info:eu-repo/semantics/openAccess">Open Access</rights>
  </rightsList>
  <descriptions>
    <description descriptionType="Abstract">Zebra dolomites and carbonate - hosted Au - Ag - Zn +/- Pb deposits of Maden village is located in the shelf type carbonate rocks of the Bolkar Mountains. The Zebra dolomite (ZD) locally form and there is no evidence for relation between dolomitization and mineralization. Maden village ZD is characterized by parallel light and dark bands that have similar mineralogy and chemistry by petrographic and SEM + EDX investigation. The delta C-13 (V - PDB) composition of the Zebra dolomite from 2.59 parts per thousand to 2.72 parts per thousand and the delta O-18 (V - PDB) values of the Zebra dolomite from -11.39 parts per thousand to -14.88 parts per thousand. These isotopic values show that the source of oxygen and carbon was derived from marine carbonates and freshwater carbonates. Fluid inclusion studies on Zebra dolomite show homogenization temperatures of 80 degrees C - 180 degrees C. Based on petrographic, isotope values and fluid inclusion study, we can say that the dolomitization occurred during the late diagentic conditions prior mineralization.</description>
  </descriptions>
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