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

Autor:	Jeremy Hall, Günay Çifçi, İrem Elitez, Cenk Yaltırak, A.E. Aksu
Rok vydání:	2015
Předmět:	geography geography.geographical_feature_category 010504 meteorology & atmospheric sciences Subduction Propagator Fault (geology) 010502 geochemistry & geophysics Strike-slip tectonics 01 natural sciences Eastern mediterranean Geophysics Tectonophysics Seismology Geology 0105 earth and related environmental sciences Earth-Surface Processes
Zdroj:	Tectonophysics. 664:5-13
ISSN:	0040-1951
DOI:	10.1016/j.tecto.2015.04.002
Popis:	• This confirms our previous suggestions that the Fethiye-Burdur Fault Zone is a 75-90 km-wide, left-lateral, fault zone.
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_dedup___::af67f822df42f204bfe5ffdce588c87b https://doi.org/10.1016/j.tecto.2015.04.002 Zobrazit plný text záznamu Full Text from ScienceDirect