1 Ocak 2013 Dergi makalesi Açık Erişim

Over, Semir; Yilmaz, Huseyin; Pinar, Ali; Ozden, Suha; Unlugenc, Ulvi Can; Kamaci, Zuheyr

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{
  "@context": "https://schema.org/", 
  "@id": 14783, 
  "@type": "ScholarlyArticle", 
  "creator": [
    {
      "@type": "Person", 
      "affiliation": "Mustafa Kemal Univ, Dept Geophys Engn, TR-31040 Antakya, Turkey", 
      "name": "Over, Semir"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Cumhuriyet Univ, Dept Geophys Engn, TR-58140 Sivas, Turkey", 
      "name": "Yilmaz, Huseyin"
    }, 
    {
      "@type": "Person", 
      "name": "Pinar, Ali"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Canakkale Onsekiz Mart Univ, Dept Geol Engn, TR-17020 Canakkale, Turkey", 
      "name": "Ozden, Suha"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Cukurova Univ, Dept Geol Engn, TR-01330 Adana, Turkey", 
      "name": "Unlugenc, Ulvi Can"
    }, 
    {
      "@type": "Person", 
      "affiliation": "Suleyman Demirel Univ, Dept Geophys Engn, TR-32260 Isparta, Turkey", 
      "name": "Kamaci, Zuheyr"
    }
  ], 
  "datePublished": "2013-01-01", 
  "description": "This study defines the Plio-Quaternary to present day stress regime in the Burdur Basin, located at the northeastern end of the Fethiye-Burdur Fault Zone in SW Turkey. This fault length, which is considered the landward continuation of the Pliny-Strabo trench, is an important feature in SW Turkey. The inversion slip vectors measured on fault planes indicate a consistent normal faulting stress regime during Plio-Quaternary time, continuing into recent times as indicated by earthquake focal mechanism inversions. Both states have consistent NW-SE trending horizontal minimum stress axes (sigma(3)). The orientation of fault sets is predominantly around the NE-SW direction in the major Fethiye-Burdur Fault Zone, making the extension NW-SE. The mean stress ratio is 0.74 indicating a triaxial stress state, which is clearly different from radial extension. The NW-SE extension is probably responsible for the formation of the Burdur Basin during Plio-Quaternary time. This extension, which is probably caused by slab-pull force due to the subduction process along the Cyprus arc, produces a dominant normal motion along the FBFZ. (C) 2013 Elsevier B.V. All rights reserved.", 
  "headline": "Plio-Quaternary Stress State in the Burdur Basin, SW-Turkey", 
  "identifier": 14783, 
  "image": "https://aperta.ulakbim.gov.tr/static/img/logo/aperta_logo_with_icon.svg", 
  "license": "http://www.opendefinition.org/licenses/cc-by", 
  "name": "Plio-Quaternary Stress State in the Burdur Basin, SW-Turkey", 
  "url": "https://aperta.ulakbim.gov.tr/record/14783"
}