標(biāo)題: Titlebook: Geothermics in Basin Analysis; Andrea F?rster,Daniel F. Merriam Book 1999 Kluwer Academic/Plenum Publishers 1999 Sediment.environment.mode [打印本頁(yè)] 作者: 黑暗社會(huì) 時(shí)間: 2025-3-21 19:33
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作者: 現(xiàn)代 時(shí)間: 2025-3-21 21:59
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作者: Crumple 時(shí)間: 2025-3-22 03:07
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作者: Bravado 時(shí)間: 2025-3-22 06:45
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作者: Accommodation 時(shí)間: 2025-3-22 09:02
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作者: 推遲 時(shí)間: 2025-3-22 15:20
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作者: 推遲 時(shí)間: 2025-3-22 17:08 作者: 輕觸 時(shí)間: 2025-3-22 23:48 作者: formula 時(shí)間: 2025-3-23 04:32 作者: Between 時(shí)間: 2025-3-23 06:33 作者: dragon 時(shí)間: 2025-3-23 09:54 作者: 連系 時(shí)間: 2025-3-23 15:51
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作者: Dedication 時(shí)間: 2025-3-23 21:08 作者: Ornament 時(shí)間: 2025-3-24 01:27
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作者: Kidney-Failure 時(shí)間: 2025-3-24 04:40
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作者: 獨(dú)特性 時(shí)間: 2025-3-24 09:18 作者: INTER 時(shí)間: 2025-3-24 12:11
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作者: expire 時(shí)間: 2025-3-24 18:17
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,作者: vanquish 時(shí)間: 2025-3-24 19:15
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作者: 是突襲 時(shí)間: 2025-3-25 01:26 作者: 收集 時(shí)間: 2025-3-25 04:21 作者: corpus-callosum 時(shí)間: 2025-3-25 09:38
Effect of Oil and Gas Saturation on Simulation of Temperature History and Maturation,f the lower Cretaceous section is thought to be gas saturated, underneath a water-saturated seal. Another case study comes from northwestern Siberia, where the largest gas accumulations on earth have been discovered..Results show that the thermal effect of gas in pores, as opposed to water, is signi作者: Truculent 時(shí)間: 2025-3-25 13:17
Ergebnisse der ersten Stufe des Neuansatzes,sin analysis are discussed. We point out that wells suitable for equilibrium or near equilibrium temperature logs usually are available, and we describe by examples criteria for the evaluation of the quality of a high- resolution temperature log. Examples of temperature gradient logs from two fields作者: Mosaic 時(shí)間: 2025-3-25 17:49 作者: agitate 時(shí)間: 2025-3-25 23:17
Manfred Sch?tzke,Udo Ritterbachthe western edge of the Canadian Shield has allowed detailed analysis of the 2D temperature distribution, calculation of the thermal gradient, and estimate of heat flow. Temperature data are available typically from only a section of the depth interval making 2D contouring of the temperature field d作者: 性滿(mǎn)足 時(shí)間: 2025-3-26 03:46 作者: 領(lǐng)先 時(shí)間: 2025-3-26 04:19 作者: Ondines-curse 時(shí)間: 2025-3-26 08:54 作者: liposuction 時(shí)間: 2025-3-26 14:34
An Intellectual Against Crusading,s of rifting during basin development. Seismic refraction data indicate the existence of a “l(fā)ow velocity layer” which can be interpreted as magmatic underplating..The aim of this study was to evaluate the effects of a possible magmatic underplating over the Gjallar Ridge. More precisely, we have est作者: Exuberance 時(shí)間: 2025-3-26 20:36 作者: Rodent 時(shí)間: 2025-3-26 23:29
Erasmus and Nicholas of Cusa on Islaments, burial depths, and heat flow. Because of the complexity of the basin’s thermal history, no previous study has resulted in a single model that predicts the observed thermal maturity for the entire stratigraphic section in the basin. Two hypotheses, however, have resulted from previous studies. 作者: 絕食 時(shí)間: 2025-3-27 04:10 作者: 浮雕 時(shí)間: 2025-3-27 06:34 作者: DNR215 時(shí)間: 2025-3-27 10:39 作者: Melanoma 時(shí)間: 2025-3-27 17:36 作者: 偽造者 時(shí)間: 2025-3-27 19:55
Geothermics in Basin Analysis978-1-4615-4751-8Series ISSN 1567-8296 作者: 先鋒派 時(shí)間: 2025-3-28 01:38
1567-8296 lved. Subject matter includes the measuring oftemperature logs and capturing of industrial temperature data andtheir interpretation to delineate subsurface conditions and processes,the importance of porosity and pore filling for modeling thermalfields, the thermal insulation of shales, geothermal an作者: Recess 時(shí)間: 2025-3-28 05:32 作者: STIT 時(shí)間: 2025-3-28 07:19
Book 1999itions and processes,the importance of porosity and pore filling for modeling thermalfields, the thermal insulation of shales, geothermal anomaliesassociated with mud diapirs and basin hydrodynamic regimes,temperatures related to magmatic underplating and plate tectonics.作者: 不可接觸 時(shí)間: 2025-3-28 12:20
1567-8296 rface conditions and processes,the importance of porosity and pore filling for modeling thermalfields, the thermal insulation of shales, geothermal anomaliesassociated with mud diapirs and basin hydrodynamic regimes,temperatures related to magmatic underplating and plate tectonics.978-1-4613-7154-0978-1-4615-4751-8Series ISSN 1567-8296 作者: cogitate 時(shí)間: 2025-3-28 15:28
High-Resolution Temperature Logs in a Petroleum Setting: Examples and Applications,sin analysis are discussed. We point out that wells suitable for equilibrium or near equilibrium temperature logs usually are available, and we describe by examples criteria for the evaluation of the quality of a high- resolution temperature log. Examples of temperature gradient logs from two fields作者: Mammal 時(shí)間: 2025-3-28 20:20 作者: 船員 時(shí)間: 2025-3-29 02:10
Present Heat Flow Along a Profile Across the Western Canada Sedimentary Basin: The Extent of Hydrodthe western edge of the Canadian Shield has allowed detailed analysis of the 2D temperature distribution, calculation of the thermal gradient, and estimate of heat flow. Temperature data are available typically from only a section of the depth interval making 2D contouring of the temperature field d作者: rods366 時(shí)間: 2025-3-29 03:05 作者: Nucleate 時(shí)間: 2025-3-29 09:56 作者: 要素 時(shí)間: 2025-3-29 15:03 作者: 極大痛苦 時(shí)間: 2025-3-29 19:11
Temperature and Maturity Effects of Magmatic Underplating in the Gjallar Ridge, Norwegian Sea,s of rifting during basin development. Seismic refraction data indicate the existence of a “l(fā)ow velocity layer” which can be interpreted as magmatic underplating..The aim of this study was to evaluate the effects of a possible magmatic underplating over the Gjallar Ridge. More precisely, we have est作者: Countermand 時(shí)間: 2025-3-29 23:33 作者: Expiration 時(shí)間: 2025-3-30 02:05 作者: pulmonary-edema 時(shí)間: 2025-3-30 07:03
Rising Mud Diapirs and Their Thermal Anomalies,or having cold to ice-cold frothy mud and water emissions from gryphons and salses despite originating from several kilometers depth (as judged by mineral contents of the waters), and for having inferred heat- flux values which can be an order or magnitude or more higher than those inferred regional作者: Irksome 時(shí)間: 2025-3-30 10:41
