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

Dublin Core

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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>Seyitoglu, Gurol</dc:creator>
  <dc:creator>Ecevitoglu, G. Berkan</dc:creator>
  <dc:creator>Kaypak, Bulent</dc:creator>
  <dc:creator>Guney, Yucel</dc:creator>
  <dc:creator>Tun, Muammer</dc:creator>
  <dc:creator>Esat, Korhan</dc:creator>
  <dc:creator>Avdan, Ugur</dc:creator>
  <dc:creator>Temel, Abidin</dc:creator>
  <dc:creator>Cabuk, Alper</dc:creator>
  <dc:creator>Telsiz, Sevgi</dc:creator>
  <dc:creator>Uyar Aldas, G. Gulsev</dc:creator>
  <dc:date>2015-01-01</dc:date>
  <dc: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.</dc:description>
  <dc:identifier>https://aperta.ulakbim.gov.trrecord/77955</dc:identifier>
  <dc:identifier>oai:zenodo.org:77955</dc:identifier>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>http://www.opendefinition.org/licenses/cc-by</dc:rights>
  <dc:source>TURKISH JOURNAL OF EARTH SCIENCES 24(1) 1-20</dc:source>
  <dc:title>Determining the main strand of the Eskisehir strike-slip fault zone using subsidiary structures and seismicity: a hypothesis tested by seismic reflection studies</dc:title>
  <dc:type>info:eu-repo/semantics/article</dc:type>
  <dc:type>publication-article</dc:type>
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