P-Alıcı Fonksiyonları ve Rayleigh Dalgası Grup Hızları’nın Birleşik Ters Çözümü’nden Doğu Anadolu Fay Zonu’nun Kabuk ve Üst Manto Hız Yapısı

The Eastern Anatolian Fault Zone (EAFZ) is an active plate boundary where intense seismicity has occurred from past to present. This activity related the geodynamic structure of region. Because Arabian northward motion and Eurasian southward motion, attempted escape westward with anticlockwise rotation, caused development important tectonic structures. Concerning these motions, S-wave velocity EAFZ intersecting North (NAFZ) in northeast Dead Sea (DSFZ) southwest interpreting tectonics present study conducted on joint inversion P-wave receiver functions Rayleigh wave group velocities techniques using data collected eight broadband stations along EAFZ. P-receiver are analyzed approximately eighty teleseismic events for each station, recorded by three-component seismometers. On other hand, dispersion curves calculations twenty-one regional earthquakes used, which have focal depth less than 50 km bigger moment magnitude Mw=5.0. analyses obtained two jointly inverted determine 1-D crust uppermost mantle station. results indicate that models show low-velocity layers identified within 4-12 upper crust. Besides, Conrad discontinuity determined as ~22 seismic stations. Furthermore, crust-mantle ~44 Consequently, this yields crustal compatible studied