Carbonate reservoirs might contain a large number of critical heterogeneities, such as fractures and karstic features, although some the existing heterogeneities cannot be identified due to the lack of seismic resolution. Our main objective is to evaluate which fracture scales need to be included in the fluid flow simulation models and, in particular, how to model subseismic fractures. We also consider the presence of enlarged fractures in the reservoir models due to karstic dissolution. The fracture network used to compose the simulation models is based on the real karstified fracture sets of the Soledade outcrop, Jandaíra Formation (Potiguar Basin, Brazil). This formation is a large and well-preserved karstified carbonate platform of the Turonian-Campanian age related to the South Atlantic opening. Our work is divided into three phases: in Phase 0, we show how to upscale the fracture network of the Soledade outcrop to in-situ deep conditions. As a result, a semi-synthetic simulation model is composed from the Soledade Outcrop data and of a Brazilian Pre-Salt carbonate reservoir. In Phase 1, we evaluated the impact of the fracture scales and fracture enlargement due to karstic dissolution on the fluid flow behavior of the semi-synthetic reservoir. Finally, in Phase 2, we propose and validate a fluid flow simulation workflow allowing to estimate a statistically equivalent network of subseismic fractures, which might be used on multiple data assimilation methods or in risk analysis of green fields. Results from Phase 1 evidence that subseismic fractures can significantly impact the fluid flow behavior, depending on the producing well location in relation to the fracture network and on the presence of enlarged fractures due to karstic dissolution. On the other hand, the Phase 2 results provide the oil and gas industry with a workflow to better characterize sub-seismic fractures in fluid flow simulation models.
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