A well-constrained geomechanical model of the Devonian clastic is presented to assess the fracture slip potential due to water injection in the Berkaoui field, Algeria. The studied interval indicates a strike-slip tectonic regime with a mean maximum horizontal stress azimuth of 98°N. A total of 131 natural fractures were interpreted from the acoustic image logs. These fractures have dominantly E-W strike, with true dips ranging between 51°-80° towards north and south. Critically stressed fracture analysis exhibits the onset of shear displacement of optimally oriented steeply dipping fractures occurring at 2.7 MPa of injection-induced pressure build-up. The practical injection threshold was inferred as 7 MPa based on caprock integrity assessment. A total of 10 out of 131 fractures (with dips = 70°) can experience injection-caused slip within the maximum allowable injection limit. The E-W oriented fractures, subparallel to the maximum horizontal stress azimuth, have a higher likelihood of being critically stressed during injection and therefore can contribute to permeability enhancement.
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