1 Ocak 2017 Dergi makalesi Açık Erişim

Italiano, F.; Yuce, G.; Di Bella, M.; Rojay, B.; Sabatino, G.; Tripodo, A.; Martelli, M.; Rizzo, A. L.; Misseri, M.

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{
  "@context": "https://schema.org/", 
  "@id": 46243, 
  "@type": "ScholarlyArticle", 
  "creator": [
    {
      "@type": "Person", 
      "affiliation": "Ist Nazl Geofis & Vulcanol, Sez Palermo, Via Ugo La Malfa 153, I-90146 Palermo, Italy", 
      "name": "Italiano, F."
    }, 
    {
      "@type": "Person", 
      "affiliation": "Hacettepe Univ, Dept Geol Engn, TR-06800 Ankara, Turkey", 
      "name": "Yuce, G."
    }, 
    {
      "@type": "Person", 
      "name": "Di Bella, M."
    }, 
    {
      "@type": "Person", 
      "affiliation": "Middle East Tech Univ, Dept Geol Engn, TR-06531 Ankara, Turkey", 
      "name": "Rojay, B."
    }, 
    {
      "@type": "Person", 
      "affiliation": "Univ Messina, Dept Math & Comp Sci Phys Sci & Earth Sci, Viale G Alcontres 31, I-98166 Messina, Italy", 
      "name": "Sabatino, G."
    }, 
    {
      "@type": "Person", 
      "affiliation": "Univ Messina, Dept Math & Comp Sci Phys Sci & Earth Sci, Viale G Alcontres 31, I-98166 Messina, Italy", 
      "name": "Tripodo, A."
    }, 
    {
      "@type": "Person", 
      "affiliation": "Ist Nazl Geofis & Vulcanol, Sez Palermo, Via Ugo La Malfa 153, I-90146 Palermo, Italy", 
      "name": "Martelli, M."
    }, 
    {
      "@type": "Person", 
      "affiliation": "Ist Nazl Geofis & Vulcanol, Sez Palermo, Via Ugo La Malfa 153, I-90146 Palermo, Italy", 
      "name": "Rizzo, A. L."
    }, 
    {
      "@type": "Person", 
      "affiliation": "Ist Nazl Geofis & Vulcanol, Sez Palermo, Via Ugo La Malfa 153, I-90146 Palermo, Italy", 
      "name": "Misseri, M."
    }
  ], 
  "datePublished": "2017-01-01", 
  "description": "The SE part of Turkey is characterized by a transtensional regime within the complex collision zone between the Anatolian, Arabian and African plates, which is bounded by two main faults, Dead Sea Fault and its splays on east and the Karasu Fault on west. In this tectonic and geodynamic context developed the Amik and further North, Erzin and Toprakkale districts, which are located onshore the Iskenderun Gulf, with the occurrence of a widespread and young alkaline volcanism dated from 1.57 to 0.05 Ma in Amik, and 2.25 to 0.61 Ma in Toprakkale.", 
  "headline": "Noble gases and rock geochemistry of alkaline intraplate volcanics from the Amik and Ceyhan-Osmaniye areas, SE Turkey", 
  "identifier": 46243, 
  "image": "https://aperta.ulakbim.gov.tr/static/img/logo/aperta_logo_with_icon.svg", 
  "license": "http://www.opendefinition.org/licenses/cc-by", 
  "name": "Noble gases and rock geochemistry of alkaline intraplate volcanics from the Amik and Ceyhan-Osmaniye areas, SE Turkey", 
  "url": "https://aperta.ulakbim.gov.tr/record/46243"
}