1 Ocak 2013 Dergi makalesi Açık Erişim

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

Dublin Core

<?xml version='1.0' encoding='utf-8'?>
<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>Over, Semir</dc:creator>
  <dc:creator>Yilmaz, Huseyin</dc:creator>
  <dc:creator>Pinar, Ali</dc:creator>
  <dc:creator>Ozden, Suha</dc:creator>
  <dc:creator>Unlugenc, Ulvi Can</dc:creator>
  <dc:creator>Kamaci, Zuheyr</dc:creator>
  <dc:date>2013-01-01</dc:date>
  <dc: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.</dc:description>
  <dc:identifier>https://aperta.ulakbim.gov.trrecord/14783</dc:identifier>
  <dc:identifier>oai:zenodo.org:14783</dc:identifier>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>http://www.opendefinition.org/licenses/cc-by</dc:rights>
  <dc:source>TECTONOPHYSICS 588 56-68</dc:source>
  <dc:title>Plio-Quaternary Stress State in the Burdur Basin, SW-Turkey</dc:title>
  <dc:type>info:eu-repo/semantics/article</dc:type>
  <dc:type>publication-article</dc:type>
</oai_dc:dc>