Titlebook: Carbonate Petroleum Reservoirs; Perry O. Roehl,Philip W. Choquette Book 1985Latest edition Springer-Verlag New York Inc. 1985 Jura.Petroph

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Qiang Lu,Yuanzhang Sun,Shengwei Mei was discovered by the Pure Oil Company in January 1960 from seismic data and stratigraphic analysis of the Pure NW Lisbon No. 1 (B-610) well. Initial production was from Pennsylvanian, Mississippian, and Devonian strata, but only the Mississippian (Leadville) carbonate sequence, by far the major pr

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Local decompositions of control systems,of Billings, Dunn, and McKenzie Counties, T144-145N, R97-98W (Fig. 10-1). Production is from the Mission Canyon Formation (lower Mississippian). The Mission Canyon lies between the Lodgepole Limestone below and the Charles Formation above, and all three combine to form the Madison Group. At this loc

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Local decompositions of control systems,ed in southeastern Illinois approximately 50 miles (80 km) northeast of the structural center of the Illinois Basin, along a major trans-basin structure, the LaSalle Anticline (Fig. 12-1). The principal carbonate reservoirs in North Bridgeport Field occur in the upper part of the Ste. Genevieve Form

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Local decompositions of control systems,Texas (Fig. 13-1A) and southeastern New Mexico. The reservoirs occur in stratigraphic and stratigraphic-structural combination traps, and are predominantly algal and coralgal buildups (“reefs”) and associated carbonate grainstones of shallow-marine origin. A modest literature exists on the sedimento

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ensemble

Local decompositions of control systems,in the Fore-Sudetic area, western Poland (Figs. 15-1, 15-2). The Main Dolomite reservoirs are of stratigraphic-structural type and are principally dolomitized oolitic and oncolitic grainstones and fractured, vuggy, dolomitized mudstones.

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Lumbar-Stenosis

Origin and Diagenesis of Middle Devonian Pinnacle Reefs Encased in Evaporites, “A” and “E” Pools, Rauction is found in Middle Devonian limestone and dolostone reefs, which are encased in evaporites (Figs. 8-2-8-4). The reefs form the Rainbow Member of the Upper Keg River Formation in the Upper Elk Point Subgroup, which is of Givetian Age (Langton and Chin, 1968).