Ce. Renshaw et Dd. Pollard, ARE LARGE DIFFERENTIAL STRESSES REQUIRED FOR STRAIGHT FRACTURE PROPAGATION PATHS, Journal of structural geology, 16(6), 1994, pp. 817-822
Fracture growth geometries in linear elastic materials are sensitive t
o the ratio between the remote differential stress, or T-stress, and t
he fracture driving stress. Two mechanically interacting fractures fol
low straighter paths for greater values of this ratio. We demonstrate
that the degree of curvature that develops between two mechanically in
teracting fractures is also controlled by such factors as sub-critical
fracture growth and fracture surface roughness. Sub-critical fracture
growth limits the development of fracture curvature by decreasing the
fracture driving stress needed for propagation. Fracture surface roug
hness can affect the development of fracture curvature by limiting the
magnitude of the shear displacement discontinuity that can be accommo
dated along the fracture. Thus, propagation paths for two mechanically
interacting fractures can be quite straight even in the presence of s
mall to moderate differential stresses. Consequently, the absence of f
racture curvature does not necessarily imply a high differential stres
s state.