Titlebook: Marine Clastic Reservoirs; Examples and Analogu E. G. Rhodes,T. F. Moslow Book 1993 Springer-Verlag New York, Inc. 1993 Bohrkernkorrelation

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Tidal Inlet Reservoirs: Insights from Modern Examplesic barrier island shoreline (Fig. 4.1). Submergence during the Holocene and the presence of reworked Holocene and Pleistocene sediment sources resulted in the formation of barrier-island, tidal-inlet, flood- and ebb-tidal delta, estuarine, and complex backbarrier environments. Hayes (1975), Nummedal

Concrete

The Sedimentologic and Geomorphologic Provinces of the Nile Fan its material from one primary source—the Nile River. The Nile River is 6,800 km long; it drains a basin of 3 million km., and has an average annual water discharge of 86 billion m. (Said, 1981). Prior to construction of the Aswan High Dam in 1964, the Nile discharged approximately 120 million m. of

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Depositional and Structural Controls on the Diagenesis of Lockhart Crossing Reservoir (Wilcox); Gulfggest that cement and porosity distributions should reflect both the geometry of the depositional units and the geometry of faults and folds. First, diagenetic processes are stabilization processes. That is, the reactive components in the sediments interact with the subsurface environment to form mo

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Shelf Sandstones of the Deep Wilcox Trend, Central Texas Gulf Coastdges along the Texas Gulf Coast. The Wilcox produces hydrocarbons along a strip paralleling the coastline from the Mississippi-Alabama state line to the Mexico border. This sequence also yields fresh water, lignite, ceramic clay, and industrial sand, and is a potential geopressured geothermal reserv

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Facies, Reservoirs and Stratigraphic Framework of the Mossoró Member (Latest Cenomanian-Earliest Tur one of the Brazilian marginal basins originated by Africa-South America rifting in the Early Cretaceous. In recent years, the onshore portion has undergone intense exploration, resulting in the discovery of several small oil fields that produce from Lower and middle Cretaceous rocks. The mid-Cretac

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Reservoir Character of Deep Marine Sandstones, Inglewood Field, Los Angeles Basin1). It was discovered in 1924 by the Standard Oil Company of California, and was completed in the Pliocene Vickers zone. Subsequently, seven additional productive zones have been discovered and are producing in the field.

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Scales of Geologic Heterogeneity of a Deep-Water Sand Giant Oil Field, Long Beach Unit, Wilmington Fditional, somewhat qualitative perspective, quantitative reservoir characteristics are poorly understood, and often are not described in a format suitable for reservoir engineering applications. Like other types of sands, heterogeneities of deep-water sand reservoirs can be described at four scales

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ues a highly interdisciplinary approach. It will serve as a valuable reference guide for students, practitioners and researchers interested in media convergence processes. .978-3-642-43821-9978-3-642-36163-0