1 Ocak 2015 Dergi makalesi Açık Erişim

Seyitoglu, Gurol; Ecevitoglu, G. Berkan; Kaypak, Bulent; Guney, Yucel; Tun, Muammer; Esat, Korhan; Avdan, Ugur; Temel, Abidin; Cabuk, Alper; Telsiz, Sevgi; Uyar Aldas, G. Gulsev

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    "creators": [
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        "affiliation": "Ankara Univ, Tecton Res Grp, Dept Geol Engn, TR-06100 Ankara, Turkey", 
        "name": "Seyitoglu, Gurol"
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      {
        "affiliation": "Anadolu Univ, Inst Earth & Space Sci, Eskisehir, Turkey", 
        "name": "Ecevitoglu, G. Berkan"
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      {
        "affiliation": "Ankara Univ, Dept Geophys Engn, TR-06100 Ankara, Turkey", 
        "name": "Kaypak, Bulent"
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      {
        "affiliation": "Anadolu Univ, Inst Earth & Space Sci, Eskisehir, Turkey", 
        "name": "Guney, Yucel"
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      {
        "affiliation": "Anadolu Univ, Inst Earth & Space Sci, Eskisehir, Turkey", 
        "name": "Tun, Muammer"
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      {
        "affiliation": "Ankara Univ, Tecton Res Grp, Dept Geol Engn, TR-06100 Ankara, Turkey", 
        "name": "Esat, Korhan"
      }, 
      {
        "affiliation": "Anadolu Univ, Inst Earth & Space Sci, Eskisehir, Turkey", 
        "name": "Avdan, Ugur"
      }, 
      {
        "affiliation": "Hacettepe Univ, Dept Geol Engn, Ankara, Turkey", 
        "name": "Temel, Abidin"
      }, 
      {
        "affiliation": "Anadolu Univ, Inst Earth & Space Sci, Eskisehir, Turkey", 
        "name": "Cabuk, Alper"
      }, 
      {
        "affiliation": "Hacettepe Univ, Dept Geol Engn, Ankara, Turkey", 
        "name": "Telsiz, Sevgi"
      }, 
      {
        "affiliation": "Hacettepe Univ, Dept Min Engn, Ankara, Turkey", 
        "name": "Uyar Aldas, G. Gulsev"
      }
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    "description": "The Eskisehir Fault Zone is one of the major neotectonic structures of Turkey, extending from Inegol (Bursa) to Cihanbeyli (Konya). The fault zone presents a considerable seismic risk for the city of Eskisehir but the exact locations of active segments and the source of the major seismic event, the 1956 earthquake (M = 6.5) that occurred in the instrumental period (from 1900 to 2013), have been debated in recent literature. The structural data obtained from field studies indicate an approximately N60W-trending main strand of the right lateral strike-slip Eskisehir Fault Zone. This trend corresponds to the en echelon bends on the course of the Sarisu River. Using this concurrence, the positions of Bahcehisar and the Cukurhisar-Sultandere segments are proposed and checked by seismic reflection studies. The seismic sections disclosing positive flower structures confirm the hypothesized position of the Cukurhisar-Sultandere segment. The relocation of epicenters and focal mechanism solutions of seismic events in 1956, 1990, 2010, and 2013 indicate that the Cukurhisar-Sultandere segment might be the rupture source of the 1956 event and is a possible potential seismic source for an earthquake that could seriously affect the Eskisehir settlement.", 
    "doi": "10.3906/yer-1406-5", 
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    "journal": {
      "issue": "1", 
      "pages": "1-20", 
      "title": "TURKISH JOURNAL OF EARTH SCIENCES", 
      "volume": "24"
    }, 
    "license": {
      "id": "cc-by"
    }, 
    "publication_date": "2015-01-01", 
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    "resource_type": {
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      "title": "Dergi makalesi", 
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    "title": "Determining the main strand of the Eskisehir strike-slip fault zone using subsidiary structures and seismicity: a hypothesis tested by seismic reflection studies"
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