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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{
  "@context": "https://schema.org/", 
  "@id": 91503, 
  "@type": "ScholarlyArticle", 
  "creator": [
    {
      "@type": "Person", 
      "affiliation": "Univ Strasbourg, CNRS, IPGS, Strasbourg, France", 
      "name": "Mahmoud, Yasser"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Univ Strasbourg, CNRS, IPGS, Strasbourg, France", 
      "name": "Masson, Frederic"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Univ Strasbourg, CNRS, IPGS, Strasbourg, France", 
      "name": "Meghraoui, Mustapha"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Istanbul Tech Univ, Dept Geol, Istanbul, Turkey", 
      "name": "Cakir, Ziyadin"
    }, 
    {
      "@type": "Person", 
      "affiliation": "NEC Syrian Natl Earthquake Ctr, Damascus, Syria", 
      "name": "Alchalbi, Abdulmutaleb"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Istanbul Tech Univ, Dept Geomat, Istanbul, Turkey", 
      "name": "Yavasoglu, Hakan"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Eskisehir Osmangazi Univ, Dept Geol, Eskisehir, France", 
      "name": "Yonlu, Onder"
    }, 
    {
      "@type": "Person", 
      "affiliation": "NEC Syrian Natl Earthquake Ctr, Damascus, Syria", 
      "name": "Daoud, Mohamed"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Marmara Res Ctr, TUBITAK, Gebze, Turkey", 
      "name": "Ergintav, Semih"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Marmara Res Ctr, TUBITAK, Gebze, Turkey", 
      "name": "Inan, Sedat"
    }
  ], 
  "datePublished": "2013-01-01", 
  "description": "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.", 
  "headline": "Kinematic study at the junction of the East Anatolian fault and the Dead Sea fault from GPS measurements", 
  "identifier": 91503, 
  "image": "https://aperta.ulakbim.gov.tr/static/img/logo/aperta_logo_with_icon.svg", 
  "license": "http://www.opendefinition.org/licenses/cc-by", 
  "name": "Kinematic study at the junction of the East Anatolian fault and the Dead Sea fault from GPS measurements", 
  "url": "https://aperta.ulakbim.gov.tr/record/91503"
}