Seismic anisotropy exists in many parts of the Earth's crust. Because of the depositional history, sedimentary rocks, especial shales, are often anisotropic, with a vertical axis of symmetry. This is known as vertical transverse isotropy (VTI). Shales are highly anisotropic, resulting from preferential alignment of clay minerals, soft cracks, organic matters, among other reasons. Shales can act as cap rock for hydrocarbon bearing reservoirs and saline aquifers intended for CO 2 sequestration, waste water re-injection; and also as hydrocarbon source rocks and unconventional reservoirs (