1 Ocak 2020 Dergi makalesi Açık Erişim

Aydin, Faruk; Saka, Simge Oguz; Sen, Cuneyt; Dokuz, Abdurrahman; Aiglsperger, Thomas; Uysal, Ibrahim; Kandemir, Raif; Karsli, Orhan; San, Bilal; Baser, Rasim

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{
  "@context": "https://schema.org/", 
  "@id": 6139, 
  "@type": "ScholarlyArticle", 
  "creator": [
    {
      "@type": "Person", 
      "affiliation": "Karadeniz Tech Univ, Dept Geol Engn, Trabzon, Turkey", 
      "name": "Aydin, Faruk"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Karadeniz Tech Univ, Dept Geol Engn, Trabzon, Turkey", 
      "name": "Saka, Simge Oguz"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Karadeniz Tech Univ, Dept Geol Engn, Trabzon, Turkey", 
      "name": "Sen, Cuneyt"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Gumushane Univ, Dept Geol Engn, Gumushane, Turkey", 
      "name": "Dokuz, Abdurrahman"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Lulea Univ Technol, Dept Civil Engn & Nat Resources, Div Geosci & Environm Engn, Lulea, Sweden", 
      "name": "Aiglsperger, Thomas"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Karadeniz Tech Univ, Dept Geol Engn, Trabzon, Turkey", 
      "name": "Uysal, Ibrahim"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Recep Tayyip Erdogan Univ, Dept Geol Engn, Rize, Turkey", 
      "name": "Kandemir, Raif"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Recep Tayyip Erdogan Univ, Dept Geol Engn, Rize, Turkey", 
      "name": "Karsli, Orhan"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Dokuz Eylul Univ, Dept Geol Engn, Izmir, Turkey", 
      "name": "San, Bilal"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Karadeniz Tech Univ, Dept Geol Engn, Trabzon, Turkey", 
      "name": "Baser, Rasim"
    }
  ], 
  "datePublished": "2020-01-01", 
  "description": "The Late Cretaceous Artvin volcanic rocks (LCAVs) from the eastern Sakarya zone (ESZ) of NE Turkey are composed of mafic/basaltic (S1-catak and S2-caglayan) and felsic/acidic (S1-Kizilkaya and S2-Tirebolu) rock types that occurred in two successive stages: (i) first stage (S1: Turonian-Early Santonian) and (ii) second stage (S2: Late Santonian-Campanian). Clinopyroxene thermobarometric results point that the S2-caglayan basaltic rocks have crystallised at higher temperatures and under deeper crustal conditions than those of the S1-catak basaltic rocks.", 
  "headline": "Temporal, geochemical and geodynamic evolution of the Late Cretaceous subduction zone volcanism in the eastern Sakarya Zone, NE Turkey: Implications for mantle-crust interaction in an arc setting", 
  "identifier": 6139, 
  "image": "https://aperta.ulakbim.gov.tr/static/img/logo/aperta_logo_with_icon.svg", 
  "license": "http://www.opendefinition.org/licenses/cc-by", 
  "name": "Temporal, geochemical and geodynamic evolution of the Late Cretaceous subduction zone volcanism in the eastern Sakarya Zone, NE Turkey: Implications for mantle-crust interaction in an arc setting", 
  "url": "https://aperta.ulakbim.gov.tr/record/6139"
}