1 Ocak 2013 Dergi makalesi Açık Erişim

Mahmoud, Yasser; Masson, Frederic; Meghraoui, Mustapha; Cakir, Ziyadin; Alchalbi, Abdulmutaleb; Yavasoglu, Hakan; Yonlu, Onder; Daoud, Mohamed; Ergintav, Semih; Inan, Sedat

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  <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/91503</identifier>
  <creators>
    <creator>
      <creatorName>Mahmoud, Yasser</creatorName>
      <givenName>Yasser</givenName>
      <familyName>Mahmoud</familyName>
      <affiliation>Univ Strasbourg, CNRS, IPGS, Strasbourg, France</affiliation>
    </creator>
    <creator>
      <creatorName>Masson, Frederic</creatorName>
      <givenName>Frederic</givenName>
      <familyName>Masson</familyName>
      <affiliation>Univ Strasbourg, CNRS, IPGS, Strasbourg, France</affiliation>
    </creator>
    <creator>
      <creatorName>Meghraoui, Mustapha</creatorName>
      <givenName>Mustapha</givenName>
      <familyName>Meghraoui</familyName>
      <affiliation>Univ Strasbourg, CNRS, IPGS, Strasbourg, France</affiliation>
    </creator>
    <creator>
      <creatorName>Cakir, Ziyadin</creatorName>
      <givenName>Ziyadin</givenName>
      <familyName>Cakir</familyName>
      <affiliation>Istanbul Tech Univ, Dept Geol, Istanbul, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Alchalbi, Abdulmutaleb</creatorName>
      <givenName>Abdulmutaleb</givenName>
      <familyName>Alchalbi</familyName>
      <affiliation>NEC Syrian Natl Earthquake Ctr, Damascus, Syria</affiliation>
    </creator>
    <creator>
      <creatorName>Yavasoglu, Hakan</creatorName>
      <givenName>Hakan</givenName>
      <familyName>Yavasoglu</familyName>
      <affiliation>Istanbul Tech Univ, Dept Geomat, Istanbul, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Yonlu, Onder</creatorName>
      <givenName>Onder</givenName>
      <familyName>Yonlu</familyName>
      <affiliation>Eskisehir Osmangazi Univ, Dept Geol, Eskisehir, France</affiliation>
    </creator>
    <creator>
      <creatorName>Daoud, Mohamed</creatorName>
      <givenName>Mohamed</givenName>
      <familyName>Daoud</familyName>
      <affiliation>NEC Syrian Natl Earthquake Ctr, Damascus, Syria</affiliation>
    </creator>
    <creator>
      <creatorName>Ergintav, Semih</creatorName>
      <givenName>Semih</givenName>
      <familyName>Ergintav</familyName>
      <affiliation>Marmara Res Ctr, TUBITAK, Gebze, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Inan, Sedat</creatorName>
      <givenName>Sedat</givenName>
      <familyName>Inan</familyName>
      <affiliation>Marmara Res Ctr, TUBITAK, Gebze, Turkey</affiliation>
    </creator>
  </creators>
  <titles>
    <title>Kinematic Study At The Junction Of The East Anatolian Fault And The Dead Sea Fault From Gps Measurements</title>
  </titles>
  <publisher>Aperta</publisher>
  <publicationYear>2013</publicationYear>
  <dates>
    <date dateType="Issued">2013-01-01</date>
  </dates>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/91503</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1016/j.jog.2012.05.006</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 Hatay Triple Junction (HTJ) is a tectonically complex area located at the intersection between the left-lateral East Anatolian fault (EAF), the Cyprus subduction arc and the left-lateral Dead Sea fault (DSF) which is a transform boundary between the Arabian and Sinai plates as they converge toward Eurasia. Previous GPS studies indicate a left-lateral strike-slip rate across the DSF varying from 5 mm/yr (along the southern part) to 2 mm/yr (along the northern part) (Alchalbi et al., 2010; Gomez et al., 2007; Le Beon et al., 2008; Mahmoud et al., 2005; Al-Tarazi et al., 2011). In contrast, the EAF has a roughly constant velocity along strike estimated at 9.7 + 0.9 mm/yr (Reilinger et al., 2006). The HTJ contains several well-identified active fault segments (DSF, EAF, Osmaniye fault, Karasu fault, Latakia fault, Jisr-al-shuggur fault, Idleb fault and Afrin fault) (Meghraoui et al., 2011), the fault-slip rates for which are poorly constrained.</description>
  </descriptions>
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