“…Particularly, fracture‐dominated rocks are highly sensitive to the opening or closure of fractures due to the changes in the normal stress across a fracture or pore‐fluid pressure (Barton et al., 1985; Cook, 1992; Huo & Benson, 2016; Vogler, Amann, et al., 2016; Vogler et al., 2018; Zimmerman et al., 1991; Zimmerman & Bodvarsson, 1996). An increase in effective normal stress tends to increase the contact area between the fracture walls and to decrease the mean mechanical aperture (Pyrak‐Nolte et al., 1987; Tsang, 1984; Vogler, Settgast, et al., 2016; H. Zhang et al., 2019). Larger contact areas between two fracture walls create large so‐called “archipelagic” regions, when under high effective stresses, which are areas filled with several small, closely spaced contact regions (Jaeger et al., 2007; Pyrak‐Nolte et al., 1987).…”