Shear bands are geologic structures widely used as kinematic indicators. Despite the large amount of
studies about these structures, their mechanical development is not yet well known. This work presents an
experimental study of shear band localization and evolution under coaxial deformation. Particular attention
is given to the influence of the obliquity of anisotropy planes on the orientation of shear bands. During
deformation, two conjugate sets of shear bands develop symmetrically for models with layers parallel to
the extension axis, while for oblique orientations one set dominates. Anisotropy planes have a strong
influence on the local stress field around conjugate fracture systems, which deviates from the applied
boundary conditions