The performance of geothermal and petroleum reservoirs, as well as the safety of underground constructions such as nuclear waste repositories, depends on the ability of fractures to either promote or inhibit fluid flow. In addition, the stability of faults and fractures during hydraulic stimulation requires information on how to minimize and mitigate the risks of induced seismicity (Hofmann et al., 2018) or the loss of the hydraulic integrity of the subsurface (Pyrak-Nolte & Nolte, 2016). Coupled hydro-mechanical processes during stress-related deformation of fractures remain notoriously difficult to predict especially in complex fractured rock masses (Rutqvist, 2015). Besides, the evolution of stress over time changes either short-term or at geological time scales and strongly governs the exploration strategies in geothermal reservoirs. Laboratory experiments can be used to develop tools and knowledge about how to characterize fractured rock mass to better predict the hydraulic properties of rocks.