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Karoo Basin (1)
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South Africa (6)
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Asia
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Far East
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China
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Tibetan Plateau (2)
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Atlantic Ocean
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Equatorial Atlantic (1)
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North Atlantic
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Amazon Fan (1)
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Northwest Atlantic (1)
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A new model for the growth of normal faults developed above pre-existing structures
Field-based investigation of fault architecture: A case study from the Lenghu fold-and-thrust belt, Qaidam Basin, NE Tibetan Plateau
A revised position for the rotated Falkland Islands microplate
Unraveling the influence of throw and stratigraphy in controlling subseismic fault architecture of fold-thrust belts: An example from the Qaidam Basin, northeast Tibetan Plateau
Palinspastic restoration of an exhumed deepwater system: A workflow to improve paleogeographic reconstructions
Temporal and spatial evolution of deepwater fold thrust belts: Implications for quantifying strain imbalance
Abstract The impact of geometric uncertainty on across-fault flow behaviour at the scale of individual intra-reservoir faults is investigated in this study. A high resolution digital elevation model (DEM) of a faulted outcrop is used to construct an outcrop-scale geocellular grid capturing high-resolution fault geometries (5 m scale). Seismic forward modelling of this grid allows generation of a 3D synthetic seismic cube, which reveals the corresponding seismically resolvable fault geometries (12.5 m scale). Construction of a second geocellular model, based upon the seismically resolvable fault geometries, allows comparison with the original outcrop geometries. Running fluid flow simulations across both models enables us to assess quantitatively the impact of outcrop resolution v. seismic resolution fault geometries upon across-fault flow. The results suggest that seismically resolvable fault geometries significantly underestimate the area of across-fault juxtaposition relative to realistic fault geometries. In turn this leads to overestimates in the sealing ability of faults, and inaccurate calculation of fault plane properties such as transmissibility multipliers (TMs).