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Using Previous HitSeismicNext Hit Information to Predict Pressure Variations and Fluid Migration Pathways to Optimize Previous HitReservoirNext Hit Development Plans

By

Tom Guidish1, Vladimir Pisetski2

(1) Geodata Consulting, Houston, TX (2) Trans Previous HitSeismicNext Hit International Inc, San Francisco,

 Previous HitReservoirNext Hit Geophysics focuses on imaging geometry, inferring lithologic properties of the subsurface, and on the direct identification of hydrocarbons under certain conditions. Other important Previous HitreservoirNext Hit parameters in Previous HitreservoirNext Hit dynamics are stresses and the resulting pressure fields within the Previous HitreservoirNext Hit. These stresses affect the fluid migration pathways, optimized location of hydrocarbons and recovery schemes throughout the life of the Previous HitreservoirNext Hit. We present a technique where Previous HitseismicNext Hit information is used to estimate the changes in stresses and Previous HitreservoirNext Hit pressures within a Previous HitreservoirNext Hit and infer fluid movement and hydrocarbon accumulations zones within the Previous HitreservoirNext Hit.

The Dynamic Fluid Method, or DFM, couples basin stress evolution models, which correspond to subsurface fluid movements, with predictions of Previous HitseismicNext Hit response and specialized processing to emphasize that response. This technique has applicability optimize field development plans, identify redistribution of pressure within the Previous HitreservoirNext Hit due to production, identify missed pay and zones most conducive to recharging.

Our technique allows estimation of pressure variations within a defined Previous HitreservoirTop zone. We can define zones or compartments of abnormal pressures, or areas that are most likely areas of fluid accumulation based on the derived parameters of fluid flow. In essence, the total pressure and its variation in the geological time scale determine the fluid dynamics and make the fluid migrate from the regions of compression into the regions of low pressures (the areas of decompression).

Besides discussion of the methodology of this technique, several case histories of this technique are provided, in both clastic and carbonate reservoirs.