The effect on the transport properties of fractures of a relative shear
displacement u of rough walls with complementary self-affine surfaces
has been studied experimentally and numerically. The shear displacement u induces an anisotropy of the aperture field with a correlation length
scaling as u and significantly larger in the direction perpendicular to u. This reflects the appearance of long range channels perpendicular to u resulting in a higher effective permeability for flow in the direction
perpendicular to the shear. Miscible displacements fronts in such fractures are
observed experimentally to display a self affine geometry of characteristic
exponent directly related to that of the rough wall surfaces. A simple model
based on the channelization of the aperture field allows to reproduces the
front geometry when the mean flow is parallel to the channels created by the
shear displacement