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#Basin

Impact of permeability anisotropy misalignment on flow rates

Permeability is the most critical parameter controlling fluid flow in porous media. The general form of permeability is anisotropic but […]

Modelling fluid flow in the Glyde sub-basin

Understanding fluid flow pathways in sedimentary basins is critical for predicting the location of sediment-hosted mineral deposits. Fluid flow pathways […]

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