“…However, compared with the shear characteristics, the compression behavior of a filled fracture is not well understood, even though such knowledge would be of great importance when investigating the response of a filled fracture in seismic events, such as the propagation of the seismic stress wave and the dynamic weakening of a gouge‐filled fault (Li et al, ; Ma et al, ; Melosh, , ; Rokhlin & Wang, ; Xia et al, ; Zhu et al, ). As shown in Figure , when a naturally triggered or man‐made stress wave propagates through a rock mass, it always encounters multiscale filled fractures and its frequency, phase, energy, and propagation velocity are obviously changed (Blakeslee et al, ; Hamilton & Mooney, ; Huang, Qi, Williams, et al, ; Huang et al, ; Rietbrock, ). In addition to the shear characteristics, the compression behavior of the filled fracture is also crucial to model the seismic response of the filled fracture.…”