“…Monitoring MS (field scale) or AE (laboratory scale) activity has been successfully used to remotely characterize rock fracturing and slip events (e.g., hydraulic fracturing, shear fracturing/faulting, and reactivation), as well as fluid migration through porous and/or fractured rocks when local pore pressure perturbations impact the in situ stress field. Most recently, numerous studies focused on the interplay between fluids, fractures, and seismicity have been published (e.g., Barbosa et al, ; Brown & Ge, ; Cueto‐Felgueroso et al, ; De Barros et al, ; Dempsey et al, ; Dempsey & Suckale, ; Diehl et al, ; Fazio et al, ; Goodfellow et al, ; Improta et al, ; Jeanne et al, ; Levandowski et al, ; Noël et al, ; Rivet et al, ; Segall & Lu, ; Zhang et al, ). This highlights the growing interest for such issues in the geoscience community, which is clearly driven by an increased need to better address actual problems encountered during fluid injection/withdrawal operations.…”