سال انتشار: ۱۳۸۶
محل انتشار: دومین همایش مقابله با سوانح طبیعی
تعداد صفحات: ۸
Samira Ameri – M.sc Student of Institute of Geophysics of the University of Tehran
Somayeh Ahmadzadeh – M.sc Student of Institute of Geophysics of the University of Tehran
thrusts in the fault footwall, implies that the Mosha Fault is an inverted normalfault which has been reactivated since the late Tertiary. In the study area, the reverse fault mechanism was associated with the rapid uplift and igneous activity in the central Alborz Range during the late Tertiary.