Dergi makalesi Açık Erişim
Over, Semir; Yilmaz, Huseyin; Pinar, Ali; Ozden, Suha; Unlugenc, Ulvi Can; Kamaci, Zuheyr
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"affiliation": "Mustafa Kemal Univ, Dept Geophys Engn, TR-31040 Antakya, Turkey",
"name": "Over, Semir"
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{
"affiliation": "Cumhuriyet Univ, Dept Geophys Engn, TR-58140 Sivas, Turkey",
"name": "Yilmaz, Huseyin"
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{
"name": "Pinar, Ali"
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{
"affiliation": "Canakkale Onsekiz Mart Univ, Dept Geol Engn, TR-17020 Canakkale, Turkey",
"name": "Ozden, Suha"
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{
"affiliation": "Cukurova Univ, Dept Geol Engn, TR-01330 Adana, Turkey",
"name": "Unlugenc, Ulvi Can"
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{
"affiliation": "Suleyman Demirel Univ, Dept Geophys Engn, TR-32260 Isparta, Turkey",
"name": "Kamaci, Zuheyr"
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"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.",
"doi": "10.1016/j.tecto.2012.12.009",
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"pages": "56-68",
"title": "TECTONOPHYSICS",
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"title": "Plio-Quaternary Stress State in the Burdur Basin, SW-Turkey"
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