1 Ocak 2011 Dergi makalesi Açık Erişim

Candan, O.; Koralay, O. E.; Akal, C.; Kaya, O.; Oberhansli, R.; Dora, O. O.; Konak, N.; Chen, F.

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  <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/18591</identifier>
  <creators>
    <creator>
      <creatorName>Candan, O.</creatorName>
      <givenName>O.</givenName>
      <familyName>Candan</familyName>
      <affiliation>Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Koralay, O. E.</creatorName>
      <givenName>O. E.</givenName>
      <familyName>Koralay</familyName>
      <affiliation>Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Akal, C.</creatorName>
      <givenName>C.</givenName>
      <familyName>Akal</familyName>
      <affiliation>Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Kaya, O.</creatorName>
      <givenName>O.</givenName>
      <familyName>Kaya</familyName>
      <affiliation>Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Bornova, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Oberhansli, R.</creatorName>
      <givenName>R.</givenName>
      <familyName>Oberhansli</familyName>
      <affiliation>Univ Potsdam, Inst Erd &amp; Umweltwissensch, D-14476 Potsdam, Germany</affiliation>
    </creator>
    <creator>
      <creatorName>Dora, O. O.</creatorName>
      <givenName>O. O.</givenName>
      <familyName>Dora</familyName>
      <affiliation>Dokuz Eylul Univ, Muhendisl Fak, Jeol Muh Bol, Buca Izmir, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Konak, N.</creatorName>
      <givenName>N.</givenName>
      <familyName>Konak</familyName>
      <affiliation>Maden Tetk &amp; Arama Genel Mudurlugu, Jeol Araltirmalari Birimi, Cankaya, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Chen, F.</creatorName>
      <givenName>F.</givenName>
      <familyName>Chen</familyName>
      <affiliation>Univ Sci &amp; Technol China, Chinese Acad Sci, Key Lab Crust Mantle Mat &amp; Environm, Hefei 230026, Peoples R China</affiliation>
    </creator>
  </creators>
  <titles>
    <title>Supra-Pan-African Unconformity Between Core And Cover Series Of The Menderes Massif/Turkey And Its Geological Implications</title>
  </titles>
  <publisher>Aperta</publisher>
  <publicationYear>2011</publicationYear>
  <dates>
    <date dateType="Issued">2011-01-01</date>
  </dates>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/18591</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1016/j.precamres.2010.09.010</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">Well-preserved primary contact relationships between a Late Proterozoic metasedimentary and the metagranitic core and Palaeozoic cover series of the Menderes Massif have been recognized in the eastern part of the Cine submassif on a regional-scale. Metaconglomerates occur as laterally discontinuous channel-fill bodies close the base of the metaquartzarenite directly above the basement. The pebbles in the metaconglomerates consist mainly of different types of tourmaline-rich leucocratic granitoids, tourmalinite and schist in a sandy matrix. Petrographic features, geochemical compositions and zircon radiometric ages (549.6 +/- 3.7-552.3 +/- 3.1 Ma) of the diagnostic clasts of the metaconglomerates (e.g. leucocratic granitoids and tourmalinites) show excellent agreement with their in situ equivalents (549.0 +/- 5.4 Ma) occurring in the Pan-African basement as stocks and veins.</description>
  </descriptions>
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