سال انتشار: ۱۳۹۰

محل انتشار: ششمین کنفرانس بین المللی زلزله شناسی و مهندسی زلزله

تعداد صفحات: ۷

نویسنده(ها):

Navid Shad Manaman – Institute of Geophysics, University of Tehran, Tehran, 14155-6466, Iran
Hossein Shomali – Department of Earth Sciences, Uppsala University, Uppsala, 752 36, Sweden

چکیده:

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.