“…A tensile wing crack grows near the tip of a closed crack or strike-slip fault in a lower angle owing to confining pressure of the ambient structure arising from change in temperature in field observations of structural geology (Myers and Aydin, 2004;Mutlu and Pollard, 2008). In addition, two elastic T-stresses are present at a crack tip for a closed crack in compression, whereas only one an elastic T-stress for an opening crack (Li and Xu, 2007), and the apparent fracture toughness and small-scale yielding zone are strongly affected by these two T-stresses (Li et al, 2009). Up to now, the advance mechanism of a flaw in shear-compression has been expounded based on the concept of fracture mechanics (NematNasser and Horii, 1982;Shen and Stephansson, 1994).…”