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

floaters

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).

性上癮

Depositional and Reservoir Facies of the Mississippian Leadville Formation, Northwest Lisbon Field, 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

裙帶關(guān)系

Depositional Facies, Diagenesis, and Reservoir Character of Mississippian Cyclic Carbonates in the Mof 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

Jejune

Porosity Development in the Mississippian Pisolitic Limestones of the Mission Canyon Formation, Glenstern part of the Williston Basin (Fig. 11- 1). The field was discovered in February 1958 on a seismically defined structural high, by the Anschutz # 1 Einar Christiansen well, which had initial production of 205 barrels of oil per day with 27° API gravity oil and a gas-oil ratio of about 100:1. Gle

燈絲

Mississippian Oolite and Non-Supratidal Dolomite Reservoirs in the Ste. Genevieve Formation, North Bed 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

foppish

fixed-joint

Geology of Upper Pennsylvanian Carbonate Oil Reservoirs, Happy and Seberger Fields, Northwestern Kaneast of Goodland (Fig. 14-1). Oil and gas in these fields are produced from limestone formations of the Lansing and Kansas City groups (Missourian). Rawlins County is situated at the northeastern end of the Las Animas arch, near the intersection of this low- relief, subsurface structure with the tre

Madrigal

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cavity