doxazosin
发表于 2025-3-23 09:58:43
6.1.3 Dielectric constitutive relations,rformed by using seismic data, sedimentary strata, sequence stratigraphic concepts, constructing various maps and reservoir tomography. Seismic waves pass through the reservoir rocks and illustrate the large-scale structures. These data are very useful for detailed subsurface correlations at field s
冒号
发表于 2025-3-23 16:16:26
Nonlinear Dielectric Susceptibilitiesually available from all wells and reservoir intervals. Various formulas and parameters are used for calculating porosity, water saturation and lithology from logs. Reservoir heterogeneities may considerably change these formulas and their parameters. Matrix responses, pore types, permeabilities and
WITH
发表于 2025-3-23 19:03:38
Carbonate Reservoir Heterogeneity978-3-030-34773-4Series ISSN 2509-3126 Series E-ISSN 2509-3134
NAIVE
发表于 2025-3-23 23:00:27
Reservoir Heterogeneity: An Introduction,m boreholes. Reservoir heterogeneity means variations of reservoir properties in space and time, and so this concept is the most important factor in reservoir studies. Despite such importance, relatively few works have been focused or documented different aspects of this subject. Evaluating heteroge
Estrogen
发表于 2025-3-24 03:44:43
Microscopic Heterogeneity, carbonate reservoir. At first, available data and methods are discussed to understand the microscopic heterogeneity in carbonates. Then, various methods are introduced to overcome this challenge. All reservoir properties depend on geological attributes, and so facies analysis and diagenetic impacts
玩忽职守
发表于 2025-3-24 10:01:12
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Perennial长期的
发表于 2025-3-24 11:21:35
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散布
发表于 2025-3-24 18:04:25
Petrophysical Evaluations,ually available from all wells and reservoir intervals. Various formulas and parameters are used for calculating porosity, water saturation and lithology from logs. Reservoir heterogeneities may considerably change these formulas and their parameters. Matrix responses, pore types, permeabilities and
团结
发表于 2025-3-24 19:26:18
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档案
发表于 2025-3-25 02:32:20
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