Sharif Digital Repository

Due to the inelasticity of the ground and geometric expansion, seismic waves are reduced by moving away from the center of wave propagation, which is called the attenuation of seismic waves. Therefore, the ground motions that occur at the site of the structures are different from the ground motions that are emitted from the source. The upcoming study investigates the attenuation of seismic waves in the geographical area of Iran based on the accelerogram data of Iran. Considering the consecutive occurrence of moderate to large earthquakes in Iran, the development of Iran's accelerography network, and the need to update the attenuation relationships by considering the parameters effective in...