Titlebook: Carbonate Reservoir Characterization; An Integrated Approa F. Jerry Lucia Book 19991st edition Springer-Verlag Berlin Heidelberg 1999 Carbo

招致

疏远天际

Rock-Fabric/Petrophysical Properties from Core Description and Wireline Logs: The One-Dimensional A extrapolate the petrophysical data laterally, as will be discussed in a later chapter. Core samples are normally available from only a few wells, whereas wireline logs are available from most wells. Therefore, most geological as well as petrophysical information must be derived from wireline logs.

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Diagenetic Overprinting and Rock-Fabric Distribution: The Dolomitization/Evaporite-Mineralization End the relationship between the spatial distribution of depositional textures and petrophysical properties. Reservoir studies have made it abundantly clear that the petrophysical properties found in carbonate reservoirs are significantly different from those of Holocene carbonate sediments due to various diagenetic processes.

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Book 19991st editionn carbonate reservoirs, in order to improve performance predictions by means of fluid-flow computer simulations The book focuses on the improvement of geological, petrophysical, and geostatistical methods, describes the basic petrophysical properties, important geology parameters, and rock fabrics f

臭名昭著

Rock-Fabric, Petrophysical Parameters, and Classification,nal space. Studies that relate rock fabric to pore-size distribution, and thus to petrophysical properties, are key to quantification of geologic models in numerical terms for input into computer simulators (Fig. 1).

Mystic

英寸

FECK

Eructation

The Nonlinear Guiding Center Theory, maps) or the porositytimes-oil-saturation (SoPhiH maps) isopached for each layer. The layers commonly lump several petrophysical rock types, and the average petrophysical values do not characterize the flow properties of the reservoir.

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Diagenetic Overprinting and Rock Fabric Distribution: The Cementation, Compaction, and Selective Dihe importance of chronostratigraphic surfaces was emphasized as the fundamental element in constructing a geological framework within which petrophysically-significant depositional textures can be systematically distributed.