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Geodynamic importance of the strike-slip faults at the eastern part of the Anatolian Scholle: Inferences from the uplift and slip rate of the Malatya Fault (Malatya-Ovacik Fault Zone, eastern Turkey)

Sancar, Taylan; Zabci, Cengiz; Akcar, Naki; Karabacak, Volkan; Yesilyurt, Serdar; Yazici, Muge; Akyuz, H. Serdar; Onal, Ayten Oztufekci; Ivy-Ochs, Susan; Christl, Marcus; Vockenhuber, Christof


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  <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/4483</identifier>
  <creators>
    <creator>
      <creatorName>Sancar, Taylan</creatorName>
      <givenName>Taylan</givenName>
      <familyName>Sancar</familyName>
    </creator>
    <creator>
      <creatorName>Zabci, Cengiz</creatorName>
      <givenName>Cengiz</givenName>
      <familyName>Zabci</familyName>
      <affiliation>Istanbul Tech Univ, Jeoloji Muhendisligi Bolumu, Maden Fak, TR-34469 Istanbul, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Akcar, Naki</creatorName>
      <givenName>Naki</givenName>
      <familyName>Akcar</familyName>
      <affiliation>Univ Bern, Inst Geol Sci, Baltzerstr 1 3, CH-3012 Bern, Switzerland</affiliation>
    </creator>
    <creator>
      <creatorName>Karabacak, Volkan</creatorName>
      <givenName>Volkan</givenName>
      <familyName>Karabacak</familyName>
      <affiliation>Eskisehir Osmangazi Univ, Muhendisl Minzarhk Fak, Jeoloji Muhendisligi Bolumu, Eskisehir, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Yesilyurt, Serdar</creatorName>
      <givenName>Serdar</givenName>
      <familyName>Yesilyurt</familyName>
      <affiliation>Univ Bern, Inst Geol Sci, Baltzerstr 1 3, CH-3012 Bern, Switzerland</affiliation>
    </creator>
    <creator>
      <creatorName>Yazici, Muge</creatorName>
      <givenName>Muge</givenName>
      <familyName>Yazici</familyName>
      <affiliation>Istanbul Tech Univ, Jeoloji Muhendisligi Bolumu, Maden Fak, TR-34469 Istanbul, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Akyuz, H. Serdar</creatorName>
      <givenName>H. Serdar</givenName>
      <familyName>Akyuz</familyName>
      <affiliation>Istanbul Tech Univ, Jeoloji Muhendisligi Bolumu, Maden Fak, TR-34469 Istanbul, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Onal, Ayten Oztufekci</creatorName>
      <givenName>Ayten Oztufekci</givenName>
      <familyName>Onal</familyName>
      <affiliation>Munzur Univ, Rare Earth Elements Applicat &amp; Res Ctr, TR-62000 Tunceli, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Ivy-Ochs, Susan</creatorName>
      <givenName>Susan</givenName>
      <familyName>Ivy-Ochs</familyName>
      <affiliation>Swiss Fed Inst Technol, Lab Ion Beam Phys, CH-8093 Zurich, Switzerland</affiliation>
    </creator>
    <creator>
      <creatorName>Christl, Marcus</creatorName>
      <givenName>Marcus</givenName>
      <familyName>Christl</familyName>
      <affiliation>Swiss Fed Inst Technol, Lab Ion Beam Phys, CH-8093 Zurich, Switzerland</affiliation>
    </creator>
    <creator>
      <creatorName>Vockenhuber, Christof</creatorName>
      <givenName>Christof</givenName>
      <familyName>Vockenhuber</familyName>
      <affiliation>Swiss Fed Inst Technol, Lab Ion Beam Phys, CH-8093 Zurich, Switzerland</affiliation>
    </creator>
  </creators>
  <titles>
    <title>Geodynamic Importance Of The Strike-Slip Faults At The Eastern Part Of The Anatolian Scholle: Inferences From The Uplift And Slip Rate Of The Malatya Fault (Malatya-Ovacik Fault Zone, Eastern Turkey)</title>
  </titles>
  <publisher>Aperta</publisher>
  <publicationYear>2020</publicationYear>
  <dates>
    <date dateType="Issued">2020-01-01</date>
  </dates>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/4483</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1016/j.jseaes.2019.104091</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">Controversy remains over when present-day configuration of the Anatolia boundary faults came into existence, and the issue of what are the driving forces of the Anatolian westward motion. The NW-striking dextral and NE-striking sinistral second-order strike-slip faults at the eastern part of the Anatolian Scholle play a crucial role within these long-lasting discussions, and the NE-striking sinistral Malatya-Ovacik Fault Zone (MOFZ) is particularly important in this ongoing debate. Although the MOFZ is defined as one of the intra-plate structures, it has been proposed that it was an inter-plate fault between the Anatolia and Arabian plates from the latest Miocene to mid-Pliocene and that it has been inactive during the last ca. 3.5 Ma. This study provides results from the first morphochronology-based uplift and slip rate estimates on the Malatya Fault within the southern section of the MOFZ. The cosmogenic isochron burial and cosmogenic depth burial of ages from the sinistrally offset Tohma River remnant terraces enabled us to calculate 1.0 +/- 0.01 and 1.12 +/- 0.01 mm/yr minimum and maximum horizontal slip rates, respectively, for the last 1.4 +/- 0.1 Ma. Furthermore, we conclude that the 96 +/- 11 m/Ma mean uplift has been driven by the Malatya Fault. Integrated interpretation of the findings of this study and available data on both the MOFZ and other strike-slip faults at the eastern part of the Anatolian Scholle support the hypothesis that they are plate-boundary related active deformation belts that originated from paleotectonic structures during the tectonic escape of the Anatolian Scholle.</description>
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