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Disequilibrium fluid pressures and groundwater flow in the western Canada sedimentary basin
T. F. Corbet,
C. M. Bethke
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Keyphrases
Low Pressure
100%
Pressure-driven Flow
100%
Pore Volume
100%
Disequilibrium
100%
Groundwater
100%
Groundwater Flow
100%
Fluid Pressure
100%
Western Canadian Sedimentary Basin
100%
Potential Gradient
50%
Numerical Model
50%
Advection
50%
Amount of Heat
50%
Plio-Pleistocene
50%
Deeply Buried
50%
Aquitard
50%
Geothermal Gradient
50%
Regional Groundwater Flow
50%
Pore Fluid
50%
Deep Aquifer
50%
Thermally Conductive
50%
Paleozoic Shales
50%
Basin Topography
50%
Southern Alberta
50%
Earth and Planetary Sciences
Canada
100%
Sedimentary Basin
100%
Groundwater Flow
100%
Fluid Pressure
100%
Confining
50%
Advection
50%
Numerical Model
50%
Alberta
50%
Pliocene
50%
Pleistocene
50%
Aquitard
50%
Geothermal Gradient
50%
Potential Gradient
50%