Navid Shad Manaman - Institute of Geophysics, University of Tehran, Tehran, ۱۴۱۵۵-۶۴۶۶, Iran
Hossein Shomali - Department of Earth Sciences, Uppsala University, Uppsala, ۷۵۲ ۳۶, Sweden

the continental -continental collision of arabian -eurasian plates has resulted complex and different types of subduction zones within iranian plateau. In this study we use surface wave tomography method to image s-velocity structure of upper mantle and moho depth variations across the iranian plateau. our results show that there is a clear evidence for subducting of arabian plate beneath central iran across the zagros collisional zone in south west iran.

waveform tomography , upper mantle , surface waves subduction zones