Plio-Quaternary Stress State in the Burdur Basin, SW-Turkey

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dc.authoridPINAR, Ali/0000-0002-2641-7344
dc.contributor.authorOver, Semir
dc.contributor.authorYilmaz, Huseyin
dc.contributor.authorPinar, Ali
dc.contributor.authorÖzden, Süha
dc.contributor.authorUnlugenc, Ulvi Can
dc.contributor.authorKamaci, Zuheyr
dc.date.accessioned2025-01-27T20:47:40Z
dc.date.available2025-01-27T20:47:40Z
dc.date.issued2013
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description.abstractThis 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.sponsorshipTUBITAK-CAYDAG [107Y321]
dc.description.sponsorshipThis work was financially supported by TUBITAK-CAYDAG (Project no: 107Y321). The authors would like to thank Catherine Yigit for assistance with English exposition that improved recent version of the text. The authors are also grateful to the anonymous reviewers for their valuable comments and suggestions that greatly improved the quality of the manuscript.
dc.identifier.doi10.1016/j.tecto.2012.12.009
dc.identifier.endpage68
dc.identifier.issn0040-1951
dc.identifier.issn1879-3266
dc.identifier.scopus2-s2.0-84874526480
dc.identifier.scopusqualityQ1
dc.identifier.startpage56
dc.identifier.urihttps://doi.org/10.1016/j.tecto.2012.12.009
dc.identifier.urihttps://hdl.handle.net/20.500.12428/25005
dc.identifier.volume588
dc.identifier.wosWOS:000319310700005
dc.identifier.wosqualityQ1
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherElsevier
dc.relation.ispartofTectonophysics
dc.relation.publicationcategoryinfo:eu-repo/semantics/openAccess
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20250125
dc.subjectInversion
dc.subjectStress state
dc.subjectExtension
dc.subjectBurdur Basin
dc.subjectHellenic/Cyprus arcs
dc.subjectSW Turkey
dc.titlePlio-Quaternary Stress State in the Burdur Basin, SW-Turkey
dc.typeArticle

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