Büyük Menderes Graben

The Büyük Menderes Graben is an active rift basin in western Turkey, part of the Western Anatolian Extension Zone.^[1] It is about 140 km long and 2.5–14 km wide with a west–east trend.^[2] It was formed during the early Miocene and remains active, as shown by historical earthquakes, the largest of which was the M7.5 1653 East Smyrna earthquake.^[1] It forms a rift valley, through which the Büyük Menderes River drains into the Aegean Sea.

References[]

^ ^a ^b Bayrak Y. & Bayrak E. (2012). "An Evaluation of Earthquake Hazard Potential for Different Regions in Western Anatolia Using the Historical and Instrumental Earthquake Data". Pure and Applied Geophysics. 169 (10): 1859–1873. doi:10.1007/s00024-011-0439-3.
^ Gürer Ö.; Sarica-Filoreau N.; Özburan M.; Sangu E.; Dogan B. (2009). "Progressive development of the Büyük Menderes Graben based on new data, western Turkey" (PDF). Geological Magazine. 146 (5): 652–673. doi:10.1017/S0016756809006359.

This Turkey location article is a stub. You can help Wikipedia by .

[Bayrak&Bayrak-1] Bayrak Y. & Bayrak E. (2012). "An Evaluation of Earthquake Hazard Potential for Different Regions in Western Anatolia Using the Historical and Instrumental Earthquake Data". Pure and Applied Geophysics. 169 (10): 1859–1873. doi:10.1007/s00024-011-0439-3.

[Gürer-2] Gürer Ö.; Sarica-Filoreau N.; Özburan M.; Sangu E.; Dogan B. (2009). "Progressive development of the Büyük Menderes Graben based on new data, western Turkey" (PDF). Geological Magazine. 146 (5): 652–673. doi:10.1017/S0016756809006359.

[1]

[2]