Titlebook: Geothermics in Basin Analysis; Andrea Förster,Daniel F. Merriam Book 1999 Kluwer Academic/Plenum Publishers 1999 Sediment.environment.mode

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High-Resolution Temperature Logs in a Petroleum Setting: Examples and Applications,her geophysical logs, and well to well comparisons. Even logs that are not in complete equilibrium contain significant information compared to a typical set of BHT points. The development of memory P/T tools and their deployment in the field for production logging indicates that the potential now ex

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Present Heat Flow Along a Profile Across the Western Canada Sedimentary Basin: The Extent of Hydrodmates of heat flow have been compared with calculated thermal gradient and heat flow from 2D steady-state models of coupled fluid flow/heat flow in saturated porous media along the profile for 5 situations of hydraulic conductivity in the major aquifers. The results of this comparison show that, for

Kidney-Failure

Regional-Scale Geothermal and Hydrodynamic Regimes in the Alberta Basin: A Synthesis,ation waters. Several basin-scale aquitards and aquicludes separate various aquifers and aquifer systems. On a regional scale, the flow of formation waters in aquifers is driven in various systems and directions by past tectonic compression, erosional rebound in thick shales, and regional- and local

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Thermal Insulation by Low Thermal Conductivity Shales: Implications for Basin-Scale Fluid Flow and .04°C/m. High temperatures in the discharge region of the basin are caused by thermal insulation and high rates of advective heat transport associated with basin-scale fluid flow along basal aquifers (Darcy velocities greater than 6 m/yr.). Our model results show high temperatures (≈90°C) in the gro

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Temperature and Maturity Effects of Magmatic Underplating in the Gjallar Ridge, Norwegian Sea,plating by a magmatic body emplaced during the Early Tertiary. The effect of underplating has dramatic consequences on the interpretation of the Early Tertiary stretching event. In the model with no underplating low stretching (β = 1.2) is required to match subsidence. If underplating is considered,

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Combining Tectonics and Thermal Fields in Taranaki Basin, New Zealand,han 20 mWm. in the Eastern Mobile Belt. Much of this surface heat-flow variation is reconciled with detailed basin analysis and thermal modeling that accounts for burial and exhumation, both of which locally exceed 2 km in time spans of a few million years. The largest lateral surface heat-flow vari

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