Mid-Period Rayleigh Wave Attenuation Model for Asia

We present an attenuation model for mid-period Rayleigh waves in Central Asia and surrounding regions. This model is defined by maps of attenuation coefficient across the region of study in the period band 14-24 s. The model is constructed to characterize the regional variations in attenuation of seismic waves in the crust, which are related to the tectonic… (More)