黑暗社会
发表于 2025-3-21 19:33:15
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现代
发表于 2025-3-21 21:59:50
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
发表于 2025-3-22 03:07:43
Manfred Schätzke,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
发表于 2025-3-22 06:45:58
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
发表于 2025-3-22 09:02:02
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
推迟
发表于 2025-3-22 15:20:28
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
推迟
发表于 2025-3-22 17:08:20
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轻触
发表于 2025-3-22 23:48:15
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formula
发表于 2025-3-23 04:32:51
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Between
发表于 2025-3-23 06:33:33
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