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

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現(xiàn)代

https://doi.org/10.1007/978-3-663-06783-2th distributions based on heat conduction. At shallow depth (less than 500 m), BHT values as read from the logs are higher than ‘true’ formation temperature; in a depth range of 500–700 m, values scatter around a ‘true’ formation temperature; and at greater depths (up to 1,100 m), the uncorrected BH

Crumple

Manfred Sch?tzke,Udo Ritterbachmates 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

Bravado

https://doi.org/10.1007/978-3-322-88448-0ation 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

Accommodation

https://doi.org/10.1007/978-3-322-88368-1asked by 500 to 2000 meters of low permeability marine shales that overlie a 600- meter thick confined aquifer system. Numerical models of coupled groundwater heat-flow in the aquifer system suggest that confined water flow at Darcy velocities of 3.17 × 10.m s. to 6.34 × 10.m s. (1 to 2 m y.) causes

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Acta Academiae Lovaniensis Contra Lvthervm,.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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