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
{
"@context": "https://schema.org/",
"@id": 77955,
"@type": "ScholarlyArticle",
"creator": [
{
"@type": "Person",
"affiliation": "Ankara Univ, Tecton Res Grp, Dept Geol Engn, TR-06100 Ankara, Turkey",
"name": "Seyitoglu, Gurol"
},
{
"@type": "Person",
"affiliation": "Anadolu Univ, Inst Earth & Space Sci, Eskisehir, Turkey",
"name": "Ecevitoglu, G. Berkan"
},
{
"@type": "Person",
"affiliation": "Ankara Univ, Dept Geophys Engn, TR-06100 Ankara, Turkey",
"name": "Kaypak, Bulent"
},
{
"@type": "Person",
"affiliation": "Anadolu Univ, Inst Earth & Space Sci, Eskisehir, Turkey",
"name": "Guney, Yucel"
},
{
"@type": "Person",
"affiliation": "Anadolu Univ, Inst Earth & Space Sci, Eskisehir, Turkey",
"name": "Tun, Muammer"
},
{
"@type": "Person",
"affiliation": "Ankara Univ, Tecton Res Grp, Dept Geol Engn, TR-06100 Ankara, Turkey",
"name": "Esat, Korhan"
},
{
"@type": "Person",
"affiliation": "Anadolu Univ, Inst Earth & Space Sci, Eskisehir, Turkey",
"name": "Avdan, Ugur"
},
{
"@type": "Person",
"affiliation": "Hacettepe Univ, Dept Geol Engn, Ankara, Turkey",
"name": "Temel, Abidin"
},
{
"@type": "Person",
"affiliation": "Anadolu Univ, Inst Earth & Space Sci, Eskisehir, Turkey",
"name": "Cabuk, Alper"
},
{
"@type": "Person",
"affiliation": "Hacettepe Univ, Dept Geol Engn, Ankara, Turkey",
"name": "Telsiz, Sevgi"
},
{
"@type": "Person",
"affiliation": "Hacettepe Univ, Dept Min Engn, Ankara, Turkey",
"name": "Uyar Aldas, G. Gulsev"
}
],
"datePublished": "2015-01-01",
"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.",
"headline": "Determining the main strand of the Eskisehir strike-slip fault zone using subsidiary structures and seismicity: a hypothesis tested by seismic reflection studies",
"identifier": 77955,
"image": "https://aperta.ulakbim.gov.tr/static/img/logo/aperta_logo_with_icon.svg",
"license": "http://www.opendefinition.org/licenses/cc-by",
"name": "Determining the main strand of the Eskisehir strike-slip fault zone using subsidiary structures and seismicity: a hypothesis tested by seismic reflection studies",
"url": "https://aperta.ulakbim.gov.tr/record/77955"
}
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