Reply to the comment by M.C. Alçiçek on “The Fethiye–Burdur Fault Zone: A component of upper plate extension of the subduction transform edge propagator fault linking Hellenic and Cyprus Arcs, Eastern Mediterranean,” Tectonophysics, 635, 80–99, by J. Hall, A.E. Aksu, İ. Elitez, C. Yaltirak and G. Çifçi

•This confirms our previous suggestions that the Fethiye-Burdur Fault Zone is a 75-90km-wide, left-lateral, fault zone.•This is based on GPS vectors, earthquake first motions, magnetotelluric data and detailed mapping including fault kinematics.

Saved in:
Bibliographic Details
Published inTectonophysics Vol. 664; pp. 5 - 13
Main Authors Elitez, I., Yaltırak, C., Hall, J., Aksu, A.E., Çifçi, G.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 28.11.2015
Subjects
Eastern Mediterranean
Fethiye–Burdur Fault Zone
Pliocene–Quaternary tectonics
Rhodes Basin
STEP fault
STEP fault
Pliocene–Quaternary tectonics
Eastern Mediterranean
Rhodes Basin
Fethiye–Burdur Fault Zone
Online AccessGet full text

Cover

More Information
Summary:•This confirms our previous suggestions that the Fethiye-Burdur Fault Zone is a 75-90km-wide, left-lateral, fault zone.•This is based on GPS vectors, earthquake first motions, magnetotelluric data and detailed mapping including fault kinematics.
ISSN:0040-1951
1879-3266
DOI:10.1016/j.tecto.2015.04.002