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Fault zones are mechanical and hydrological heterogeneities in Earth's upper crust, however, the internal properties that cause heterogeneity, their three-dimensional variations, and the fundamental processes that lead to these variations are poorly understood. The hydraulic behaviour of faults at depth plays an important role in the exploration and production of hydrocarbons, as in several other subsurface engineering applications. Faults can act as conduits, barriers and combined conduit-barrier systems to fluid flow, depending on their petrophysical properties, on their internal structure and stress state. The degree to which a fault will impede fluid flow is only as great as its most permeable point. Producing reliable predictions of cross-fault and up-fault fluid flow requires an understanding of the processes that determine areas of the fault surface containing transmissible fault rocks. A field site in Miri, Jalan Mukag outcrop, was selected because it offers excellent 3D outcrops of normal faults in soft siliciclastic sediments, and gives the opportunity to investigate fault architecture both along-strike and down-dip. Weak-seal areas for cross-fault fluid flow along the fault zone exposures are identified combining detailed mapping of the fault zone architecture, analyses of the fault rock facies and geostatistical characterization (variograms) of variation in along-strike fault-core thickness. Processes that express the accumulation of of strain in the fault core (slip surfaces, boudinage and grain-scale mixing) are analysed because of their implications in terms of cross-fault fluid flow. The interaction between these processes in the fault core may or may not lead to complete mesoscale and grain-scale mixing, thus potentially induce changes in the capillary entry pressure of the fault rocks. Deformation mechanisms and geochemical processes that affect the fault zone are identified through petrographic, microstructural and mineralogical analysis,and they are used to infer along-fault fluid flow history and implications for cross-fault fluid flow.