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Abstract

Anisotropy in subsurface geological models is primarily caused by two factors: Sedimentation in shale/sand layers and fractures. The sedimentation factor is mainly modeled by Vertical Transverse Isotropy, whereas the fractures are modeled by a Horizontal

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/content/papers/10.3997/2214-4609.201400091
2009-06-08
2024-04-25

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