Figures of the Article

• Distribution of the faults and the earthquakes after 1900 with magnitudes greater than 5 in the investigation region (IIEES)
• Annual rate of occurrence estimated by Kijko (2000) method for Tehran and its vicinity
• Comparison of the resulted hazard curves for PGA using in-house MATLAB code and SEISRISKIII software, while the Mosha fault is considered as the only source of seismicity
• Comparison of a 2475-year return period response spectrum resulted in this study with response spectrum presented in Gholipour et al. (2008) final PSHA reports for Tehran
• Response spectrum for the bedrock of considered site in a 10000-year return period
• Deaggregation of hazard for the site of interest in Tehran in a 10000-year return period for different vibration periods, T
• Variation of controlling magnitude with period for the site of interest in a 10000-year return period
• Variation of controlling distance with period for the site of interest in a 10000-year return period
• Variation of values for X with magnitude for the site of interest at the worst scenario for the location of hypocenter
• Maximum probability of pulse occurrence at the site of interest in Tehran for earthquakes with different magnitudes on North Tehran fault
• Hazard curves for the site of interest in Tehran in a 10000-year return period for different vibration periods, (a) T=0.1 s (b) T=1 s (c) T=2 s (d) T=4 s
• Response spectrum for the site of interest in Tehran in a 2475-year return period with and without considering rupture directivity effects
• Response spectrum for the site of interest in Tehran in a 10000-year return period with and without considering rupture directivity effects