Aksu-Dinar Fault System: Its bearing on the evolution of the Isparta Angle (SW Turkey)

Date

2017-04-28

Author

Kaymakcı, Nuretdin
Özacar, Atilla Arda
Gülyüz, Erhan
Hınsbergen, Douwe
Uzel, Bora
Mcphee, Peter
Sözbilir, Hasan

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https://hdl.handle.net/11511/71616

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Aksu-Dinar Fault System: Its Bearing on the Evolution of the Isparta Angle (SW Turkey) Kaymakcı, Nuretdin; Özacar, Atilla Arda; Gülyüz, Erhan; Van Hinsbergen, Douwe (null; 2017-04-28) The Isparta Angle is a triangular structure in SW Turkey with NE-SW trending western and NW-SE trending eastern flanks. Aksu Fault is located within the core of this structure and have been taken-up large E-W shortening and sinistral translation since the Late Miocene. It is an inherited structure which emplaced Antalya nappes over the Beydaǧları Platform during the late Eocene to Late Miocene and was reactivated by the Pliocene as a high angle reverse fault to accommodate the counter-clockwise rotation of ...
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Citation Formats

N. Kaymakcı et al., “Aksu-Dinar Fault System: Its bearing on the evolution of the Isparta Angle (SW Turkey),” 2017, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/71616.