1 Ocak 2009 Dergi makalesi Açık Erişim

Boztug, D.; Jonckheere, R. C.; Heizler, M.; Ratschbacher, L.; Harlavan, Y.; Tichomirova, M.

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  <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/41609</identifier>
  <creators>
    <creator>
      <creatorName>Boztug, D.</creatorName>
      <givenName>D.</givenName>
      <familyName>Boztug</familyName>
      <affiliation>Cumhuriyet Univ, Dept Geol Engn, TR-58140 Sivas, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Jonckheere, R. C.</creatorName>
      <givenName>R. C.</givenName>
      <familyName>Jonckheere</familyName>
      <affiliation>TU Bergakad Freiberg, Inst Geol, D-09599 Freiberg, Sachsen, Germany</affiliation>
    </creator>
    <creator>
      <creatorName>Heizler, M.</creatorName>
      <givenName>M.</givenName>
      <familyName>Heizler</familyName>
      <affiliation>NM Tech, New Mexico Bur Geol &amp; Mineral Resources, Socorro, NM 87801 USA</affiliation>
    </creator>
    <creator>
      <creatorName>Ratschbacher, L.</creatorName>
      <givenName>L.</givenName>
      <familyName>Ratschbacher</familyName>
      <affiliation>TU Bergakad Freiberg, Inst Geol, D-09599 Freiberg, Sachsen, Germany</affiliation>
    </creator>
    <creator>
      <creatorName>Harlavan, Y.</creatorName>
      <givenName>Y.</givenName>
      <familyName>Harlavan</familyName>
      <affiliation>Geol Survey Israel, IL-95501 Jerusalem, Israel</affiliation>
    </creator>
    <creator>
      <creatorName>Tichomirova, M.</creatorName>
      <givenName>M.</givenName>
      <familyName>Tichomirova</familyName>
      <affiliation>Tech Univ Bergakad Freiberg, Inst Mineral, D-09596 Freiberg, Sachsen, Germany</affiliation>
    </creator>
  </creators>
  <titles>
    <title>Timing Of Post-Obduction Granitoids From Intrusion Through Cooling To Exhumation In Central Anatolia, Turkey</title>
  </titles>
  <publisher>Aperta</publisher>
  <publicationYear>2009</publicationYear>
  <dates>
    <date dateType="Issued">2009-01-01</date>
  </dates>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/41609</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1016/j.tecto.2008.05.035</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">The Middle to Late Cretaceous central Anatolian granitoids intrude the supra-subduction zone-type central Anatolian ophiolite and medium- to high-grade metasediments of central Anatolian crystalline complex and are overlain by Late Palaeocene to Early/Middle Eocene sediments. Their single-zircon Pb-207-Pb-206 evaporation ages define three clusters: (I) Cenomanian-Turonian (weighted-mean age: 94.9 +/- 3.4 Ma), (2) Turonian-Santonian (85.5 +/- 5.5 Ma) and (3) Campanian (74.9 +/- 3.8 Ma). Their hornblende and biotite Ar-40-Ar-39 and K-Ar cooling ages cluster around 80-65 Ma. The close hornblende and biotite ages reflect rapid exhumation of a mid-crustal section during the Campanian-Maastrichtian. Early to Middle Palaeocene (57-62 Ma) apatite fission-track age clusters date the tail end of this exhumation episode. It is proposed that the central Anatolian granitoid melts were generated in a post-collisional extensional setting following the docking of an oceanic island arc onto the Tauride-Anatolide platform. Campanian-Maastrichtian to Early/Middle Palaeocene rapid exhumation event is considered to result from continent-continent collisions between Eurasian plate and the Tauride-Anatolide platform along the Izmir-Ankara-Erzincan suture zone. (C) 2008 Elsevier B.V. All rights reserved.</description>
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