| dc.creator |
YILMAZ, HÜSEYİN |
|
| dc.creator |
Pinar, Ali |
|
| dc.creator |
ÖZDEN, SÜHA |
|
| dc.creator |
ÜNLÜGENÇ, ÜLVİ CAN |
|
| dc.creator |
KAMACI, Züheyr |
|
| dc.creator |
Over, Semir |
|
| dc.date |
2013-03-10T22:00:00Z |
|
| dc.date.accessioned |
2020-10-06T09:24:51Z |
|
| dc.date.available |
2020-10-06T09:24:51Z |
|
| dc.identifier |
0ea080b2-bfb5-465b-afcb-fe00bee3bbeb |
|
| dc.identifier |
10.1016/j.tecto.2012.12.009 |
|
| dc.identifier |
https://avesis.sdu.edu.tr/publication/details/0ea080b2-bfb5-465b-afcb-fe00bee3bbeb/oai |
|
| dc.identifier.uri |
http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/53329 |
|
| 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.language |
eng |
|
| dc.rights |
info:eu-repo/semantics/closedAccess |
|
| dc.title |
Plio-Quaternary Stress State in the Burdur Basin, SW-Turkey |
|
| dc.type |
info:eu-repo/semantics/article |
|