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REFERENCES 203
interface between the base Marcellus and Onondaga with the linear slip theory and P‐wave AVOAz data from the
Limestone were inverted for fracture orientations and top or bottom interfaces can be inverted to predict fracture
showed consistent results with FMI log observations. set orientations.
However, the strength of azimuthal anisotropy is not always
a robust indicator of reservoir quality because the relation
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