“…A similar explanation for the brittle to ductile transition in rock with increasing pressure is given by Paterson, 1970. The results in the low pressure range can be understood on the basis of a crack friction model developed by Dienes, 1983 andDienes, 2005. Other authors have also considered the effect of friction on the mechanical properties of materials (McClintock and Walsh, 1962;Mavko, 1979;Comninou and Dundurs, 1980;TianHu and Weishen, 1993;Egami and Kitaoka, 1996;Kovtunenko, 1998. Dienes, 1983and Zuo and Dienes, 2005 have applied the concept of coulomb friction forces between closed shear crack surfaces as resisting crack growth (Ward and Hadley, 1993).…”