“…GPR has been widely used for imaging fracture networks and detecting permeable fractures in various hydrogeological, geotechnical and nuclear waste‐related applications (see Molron et al., 2020; Slob et al., 2010, for an overview). In certain cases, EM waves with wavelengths at the metre‐scale can resolve fractures with sub‐millimetre aperture (i.e., thin‐bed response) due to the high dielectric contrast between the host rock and fracture filling (Dorn et al., 2012; Day‐Lewis et al., 2017; Glover, 2015; Giertzuch et al., 2021). Properties such as fracture size, local orientation (i.e., curvature), position, extent, aperture and filling, play an important role in the wave‐scattering response at the fracture interface, allowing to infer fracture properties from GPR data.…”