1 Ocak 2016 Dergi makalesi Açık Erişim

Cortuk, Rahmi Melih; Celik, Omer Faruk; Ozkan, Mutlu; Sherlock, Sarah C.; Marzoli, Andrea; Altintas, Ismail Emir; Topuz, Gultekin

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{
  "@context": "https://schema.org/", 
  "@id": 53135, 
  "@type": "ScholarlyArticle", 
  "creator": [
    {
      "@type": "Person", 
      "affiliation": "Kocaeli Univ, Muhendislik Fak, Jeoloji Muhendislii Bolumu, TR-41380 Kocaeli, Turkey", 
      "name": "Cortuk, Rahmi Melih"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Kocaeli Univ, Muhendislik Fak, Jeoloji Muhendislii Bolumu, TR-41380 Kocaeli, Turkey", 
      "name": "Celik, Omer Faruk"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Kocaeli Univ, Muhendislik Fak, Jeoloji Muhendislii Bolumu, TR-41380 Kocaeli, Turkey", 
      "name": "Ozkan, Mutlu"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Open Univ, CEPSAR, Milton Keynes, Bucks, England", 
      "name": "Sherlock, Sarah C."
    }, 
    {
      "@type": "Person", 
      "name": "Marzoli, Andrea"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Kocaeli Univ, Muhendislik Fak, Jeoloji Muhendislii Bolumu, TR-41380 Kocaeli, Turkey", 
      "name": "Altintas, Ismail Emir"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Istanbul Tech Univ, Avrasya Yer Bilimleri Enstitusu, Istanbul, Turkey", 
      "name": "Topuz, Gultekin"
    }
  ], 
  "datePublished": "2016-01-01", 
  "description": "The Late Cretaceous accretionary complex of the zmir-Ankara-Erzincan suture zone, near Artova, is composed mainly of peridotites (variably serpentinized), amphibolite, garnet-micaschist, calc-schist, marble, basalt, sandstones, neritic limestones. The metamorphic rocks were interpreted as the metamorphic sole rocks occurring at the base of mantle tectonites, because: (i) amphibolites were observed together with the serpentinized peridotites suggesting their occurrences in the oceanic environment; (ii) foliation in amphibolites and serpentinized peridotites run subparallel to each other; (iii) all these metamorphic rocks and serpentinized peridotites are cross-cut by the unmetamorphosed dolerite dikes with island arc tholeiite-like chemistry. Geochemical characteristics of the amphibolites display enriched mid-ocean ridge basalt (E-MORB)- and ocean island basalt (OIB)-like signatures. The dolerite dikes, on the other hand, yield an island arc tholeiite-like composition. Geothermobarometric investigations of the metamorphic sole rocks suggest that the metamorphic temperature was similar to 650 +/- 30 degrees C and the pressure condition was less than 0.5GPa. Dating of hornblende grains from amphibolite yielded age values ranging from 139 +/- 11 to 157 +/- 3.6Ma (2 sigma). The oldest weighted average age value is regarded as approximating the timing of the intra-oceanic subduction. These cooling ages were interpreted to be the intra-oceanic subduction/thrusting time of the zmir-Ankara-Erzincan oceanic domain.", 
  "headline": "Origin and geodynamic environments of the metamorphic sole rocks from the zmir-Ankara-Erzincan suture zone (Tokat, northern Turkey)", 
  "identifier": 53135, 
  "image": "https://aperta.ulakbim.gov.tr/static/img/logo/aperta_logo_with_icon.svg", 
  "license": "http://www.opendefinition.org/licenses/cc-by", 
  "name": "Origin and geodynamic environments of the metamorphic sole rocks from the zmir-Ankara-Erzincan suture zone (Tokat, northern Turkey)", 
  "url": "https://aperta.ulakbim.gov.tr/record/53135"
}