Scattering‐to‐Intrinsic Transition Governing Coda Attenuation in the US Continental Crust
Seismic attenuation is a key indicator of crustal heterogeneity and energy dissipation, yet the physical mechanism of coda‐wave attenuation remains unclear due to the combined influence of scattering and intrinsic absorption. In this study, we analyze multi‐frequency S‐wave coda attenuation using the seismic recordings...