Our understanding of factors that control fluid flow pathways plays a vital role in numerous disciplines including oil, gas, and geothermal exploitation, and š“š“ CO2 sequestration studies (Fox et al., 2015;Jansen, 2011;Lepillier et al., 2019;Li, 2020). Fluid flow pathways are often controlled by permeable and porous material created by geological features such as fractures, joints, and faults (Hanano, 2000). Fracture and fault patterns dictate the flow distribution in reservoirs (Brown et al., 1999) and contribute to the convection of heat within geothermal systems (Hanano, 2000). Therefore, the knowledge of fracture and fault distribution is of great importance in modeling the viability of both natural and engineered geothermal systems (Li, 2020;Miranda et al., 2018).