Titlebook: Applied Hydrodynamics in Petroleum Exploration; Eric C. Dahlberg Book 1995Latest edition Springer-Verlag New York, Inc. 1995 Engineering G

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https://doi.org/10.1007/978-1-4842-8628-9nment in terms of single bodies of homogeneous fluid. It is not really this way in a rock, however, since any single fluid mass is essentially interspersed within a network of intergranular pore spaces, throats, fracture openings, etc. As long as the fluids are in complete communication, the princip

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https://doi.org/10.1007/978-981-15-2121-8erence elevations at which levels of potential energy for oil or gas can be easily calculated, and the points at which the Z traces intersect the top of the unit correspond to structure contours. The “contour interval” is ΔZ. Since the system is hydrostatic, the buoyancy vector and the gravity vecto

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https://doi.org/10.1007/978-1-4612-4258-1Engineering Geology; Erd?llagerst?tte; Hydrogeologie; Hydrogeology; petroleum geology

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