1 Ocak 2016 Dergi makalesi Açık Erişim

Faris, Mahmoud; El Sheikh, Hassan; Shaker, Fatma

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  <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/61115</identifier>
  <creators>
    <creator>
      <creatorName>Faris, Mahmoud</creatorName>
      <givenName>Mahmoud</givenName>
      <familyName>Faris</familyName>
      <affiliation>Tanta Univ, Fac Sci, Dept Geol, Tanta, Egypt</affiliation>
    </creator>
    <creator>
      <creatorName>El Sheikh, Hassan</creatorName>
      <givenName>Hassan</givenName>
      <familyName>El Sheikh</familyName>
      <affiliation>Benha Univ, Dept Geol, Fac Sci, Banha 13518, Egypt</affiliation>
    </creator>
    <creator>
      <creatorName>Shaker, Fatma</creatorName>
      <givenName>Fatma</givenName>
      <familyName>Shaker</familyName>
      <affiliation>Benha Univ, Dept Geol, Fac Sci, Banha 13518, Egypt</affiliation>
    </creator>
  </creators>
  <titles>
    <title>Calcareous Nannofossil Biostratigraphy Of The Marine Oligocene And Miocene Succession In Some Wells In Northern Egypt</title>
  </titles>
  <publisher>Aperta</publisher>
  <publicationYear>2016</publicationYear>
  <dates>
    <date dateType="Issued">2016-01-01</date>
  </dates>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/61115</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1007/s12517-016-2445-3</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">Twelve calcareous nannofossil biozones of Late Oligocene-Late Miocene in Northern Egypt were defined and correlated with their corresponding biozones in Egypt and other parts of the world. These are arranged from the top to base as Zone NN12, Zone NN11, Zone NN10, Zone NN8, Zone NN7, Zone NN6 Zone NN5, NN4, Zone NN3, Zone NN2 Zone NP25 and Zone NP24. In the present study (Boughaz-1 Well), the Late Miocene unconformably overlies the Middle Miocene. This unconformity surface is recognized by the missing of calcareous nannofossil zones NN7 to NN9. While, in North Sinai (Malha-1 Well), the Early/Middle Miocene boundary cannot be recognized, where the Middle Miocene unconformably overlies the topmost Oligocene, and it is defined by the missing calcareous nannofossil zones NN1 to NN4.</description>
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