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First EAGE International Conference on Fault and Top Seals - What do we know and where do we go?
- Conference date: 08 Sep 2003 - 11 Sep 2003
- Location: Montpellier, France
- ISBN: 978-90-73781-32-0
- Published: 08 September 2003
1 - 20 of 66 results
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Attempt at Correlation Study between Linear and Relative Permeability Data of Basis Types of Carbonate Rocks, Applying a Neural Network
Authors B. D. Darlak and M. W. WlodarczykThis paper deals with a new application of neural network in the study of relative permeability curves. This problem has particular significance since during these lengthy experiments the number of tested samples is fewer than it should be used to prepare main data base.
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Risking Accumulations and Sealing in Petroleum Systems Modeling - A Bayesian Approach
Authors A. Kauerauf and T. HantschelModeling the accumulation and loss of hydrocarbons in traps is one of the prirnary tasks in Petroleum Systems Modeling. Hydrocarbon column heights and accumulation sizes are in most cases determined by the physical properties of the top seals which can also obviously include faults and facies boundaries. The sealing capacity is usually quantified with capillary pressure values, and hydrocarbon break-through and loss from an accumulation occurs when the density contrast between the hydrocarbons and water times column height exceeds the capillary pressure. Accurate quantitative knowledge of the sealing capillary pressure is therefore required. Unfortunately, experimental values or theories for the derivation of capillary values from interfacial tensions, fluid properties and pore geometry are seldom available with the required degree of accuracy, especially as effective or bulk values are required.
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Is the Top of Overpressure Seal in the Gulf of Mexico a Result of Capillary Sealling?
Authors L. M. Cathles, C. Poyurs, J. Shosa and M. WizevichMost active basins generate and retain near-lithostatic fluid pressures a few kilometers below the sediment surface.
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Secondary Migration in a 2D Visual Laboratory Model
Authors F. Vassenden, Ø. Sylta and C. ZwachReservoirs and cap-rocks undergo burial dwing geological time. Hydrocarbons migrate into and fill traps during periods of active expulsion from source rocks. The supply of oil and gas can be abundant until deep burial stops the supply. Capillary leakage of oil and gas from the trap can then potentially decrease the size of the accumulation. A laboratory study of filling into and leakage out of a trap has been undertaken with a visual 2D laboratory model. The model defined a synthetic cap rock having a finite entry pressure overlying a permeable reservoir rock. The trap was formed by imbedding a pyramid-shaped layer of smaller glass beads in a pack of larger glass beads.
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Identifying and Assessing Seals Using Carbon Isitope Mud Gas Depth Profiles - Examples from the Western Canada Sedimentary Basin
Authors B. J. Tilley and K. MuehlenbachsThe regional integrity of hydrocarbon seals was investigated across the BC/Alberta edge of the Western Canada Sedimentary Basin by looking at the geochemistry of gases from three wells. We analyzed the carbon isotope and compositional geochemistry of hydrocarbon gases liberated by drilling.
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Accurate Assessment of Fill History - A Critical Element when Adressing Seal Potential
Authors M. Lisk, W. Bailey, M. Brincat and A. GartrellAccurate determination of hydrocarbon fill history is critical to the effective validation of predictive trap integrity models. In most instances, such models are validated using the distribution of hydrocarbon discoveries, thereby excluding the majority of the well results that are water wet. Interpreting the fill history of presently water-wet traps is desirable because it enlarges the footprint of investigation and helps produce a more statistically reliable predictive model. A reliance on conventional hydrocarbon shows, which are easily degraded over geological timeframes or during the drilling process and where there is uncertainty in the significance of oil show intensity, often makes reliable determination of the hydrocarbon charge history of water wet traps equivocal.
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Seal Assessment in the Context of Underground CO2 Storage - Challenges and Existing Methods
Authors P. Zweigel and E. G. B. LindebergCapture of C02 from large point sources and subsequent long-term underground storage is at present the most promising option to reduce greenhouse-gas emissions without major sudden changes of our energy system. Two main types of subsurface CO2 reservoirs exist: emptied hydrocarbon fields and (saline) aquifers. In addition, some minor quantities of CO2 can be stored in enhanced oil recovery (EOR) projects. In all these cases, the existente of a tight seal is mandatory, to restrict buoyancy-driven upward migration of the CO2 into the atmosphere.
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Vertical Seal Efficiency of Conventional and Fault-Related Traps in Deepwater Clastic Environment
Authors D. Grauls, J. L. Montenat and M. LescanneIn deep offshore Tertiary basins the hydrocarbons trapped in turbiditic plays are very often found at shallow burial in different structural settings. These traps are also characterized by important 4 way or 3 way-dip closures sometimes exceeding 1000 meters especially in ultra deep imbricate fan system.
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Evaluation of Reservoir Fluid Behaviour, Compartmentalisation and Seal Efficiency through Gas While Drilling Data Analysis (GWDtm)
Authors P. Blanc, B. Barraud, D. Kandel, D. Levaché and G. SegaliniThe acquisition of gas data while drilling for geological-surveillance and safety is an almost universal. practice. Hence, mud logging services provide the earliest available data, along with LWD operations. A method has been developed by Total and Eni in order to use these gas data within the scope of reducing uncertainties in formation evaluation.
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A Methodology for Integrated Seal Assessment and Risking
Authors R. R. Hills, S. D. Mildren, R. Daniel and J. KaldiAn integrated workflow for seal assessment and risking is proposed. The methodology considers six key parameters that can be combined into a single value indicative of overall risk for the presence of a sealed trap.
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Fault Trap Analysis of the Lower Permian Rotliegend Gas Play in the Lauwerszee Trough, NE Netherlands
By F. V. CoronaThe Lauwerszee Trough is a northeast-trending sub-basin located within the Southem Permian Basin, and lies in the onshore area of northeast Netherlands. Referrred to as the "Golden Land" Trend, it is the classical Lower Permian Rotliegend gas play of the Netherlands, consisting here of the prolific, high net-to-gross sandstones of the Slochteren Formation trapped in tilted fault blocks and sourced from the Carboniferous.
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Reservoir Compartmentalisation, Approaches Based on the Fluids - An Examples in the UK North Sea
Authors G. Caillet, A. Noyau, D. Kandel and F. WalgenwitzThis paper is dedicated to an approach based on fluid analyses to investigate the possibility of either a fluid compartmentalisation or a fluid connectivity in complex oil and gas fields. This may have a major impact for the optimisation of the development and production of the fields.
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Prograding' Deltaic Tectonics in Brunei - Implications for Fault Sealing
Authors M. R. P. Tingray, R. R. Hillis, C. K. Morley, R. E. Swarbick and S. J. DrakeThe Baram Delta province of Brunei (northwest Borneo) is a Tertiary delta system built up upon an active margin. Hence, the structures observed in Brunei are the result of a complex interaction between gravity-driven deltaic tectonics and transpressive tectonics associated with the active margin.
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Large Strain Testing of Fault Seals - Laboratory Experiments and Development of Fault Seal Models
Authors F. D. E. Cuisiat, K. Bjørlykke, R. H. Gabrielsen and R. B. FærsethFaults that affect fluid flow in hydrocarbon reservoirs are produced by the deformation of a large variety of sediment types, under different stress conditions.
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Discrete Element Stress Modelling in the Timor Sea and Otway Basin, Australia
Authors S. P. Hunt, P. Boult and C. BronwynRock stress can only be measured at local points in space but determination of the state of stress in large rock masses is affected by heterogeneities, most significantly faults and horizon boundaries. Faults and horizon boundaries can greatly affect the magnitude and orientation of the in-situ rock stress state. The discrete element method is specifically designed to solve fracture problems.
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