“…The EDZ is generally defined as the zone beyond the excavation boundary where the rock has been considerably disturbed and/or damaged due to the excavation and re-distribution of stresses, see for example, Fairhurst and Damjanac (1996), Martin et al (1997), Martino and Chandler (2004), Tsang et al (2005), Mostkov (1979), Fishman and Lavrov (1996) among others. The disturbance and damage are mainly in the form of creation of new fractures, closure and opening of preexisting fractures (Sato et al, 2000), and disturbance of the in situ stress (Tsang et al, 2005).…”