Hydrocarbon Reservoir Characterization 1995
DOI: 10.2110/scn.95.34.0129
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Fluid-Flow Characterization of Dolomitized Carbonate-Ramp Reservoirs: San Andres Formation (Permian) of Seminole Field and Algerita Escarpment, Permian Basin, Texas and New Mexico

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Cited by 17 publications
(10 citation statements)
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“…However, evaluation of 3 composite cores after an extensive water-alternating miscible CO 2 injection showed that Klinkenberg-corrected permeability increased by 65% to 6 folds (600%). Porosity increased by 0.5 to 1.0 porosity unit, while the grain density reduced by 0.007 to 0.019 g/cm 3 . This might suggest that appreciable formation alteration occurred due to dissolution of carbonates by the weak carbonic acid formation.…”
Section: Remaining Oil Saturation Vs Permeabilitymentioning
confidence: 91%
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“…However, evaluation of 3 composite cores after an extensive water-alternating miscible CO 2 injection showed that Klinkenberg-corrected permeability increased by 65% to 6 folds (600%). Porosity increased by 0.5 to 1.0 porosity unit, while the grain density reduced by 0.007 to 0.019 g/cm 3 . This might suggest that appreciable formation alteration occurred due to dissolution of carbonates by the weak carbonic acid formation.…”
Section: Remaining Oil Saturation Vs Permeabilitymentioning
confidence: 91%
“…Core data reveal that the lower 750 ft of the San Andres contains skeletal grainstone and packstone and an open-marine fauna. The highstand systems tract is represented by (1) A number of detailed reservoir characterization studies have been undertaken on the Seminole Field as well as the San Andres in general and reported by several authors [3][4][5][6] . Eleven high-frequency cycles (HFCs) have been identified and twelve dolomitic facies ranging from deep subtidal argillaceous mudstone and fusulinid wackestone, to peritidal laminites and microkarst residuum have been described.…”
Section: B) Geologic Setting (Structure and Reservoir)mentioning
confidence: 99%
“…10 presents saturation above the transition zone estimated from resistivity logs, porosity from core plugs, and rock-fabric class determined from thin sections. Data are included from Seminole San Andres (Permian) field of West Texas, 19 South Cowden Grayburg (Permian) field in West Texas, 20 and Ghawar Arab D (Jurassic) field in Saudi Arabia. 21 Seminole and South Cowden fields produce from dolostone and Ghawar field produces from both limestone and dolostone.…”
Section: Comparison With Other Permeability Modelsmentioning
confidence: 99%
“…11). 19,22 This is a dolomite reservoir where the precursor limestone fabrics are preserved in the dolostone. Results from the Jurassic Arab D reservoir in the Haradh area of Ghawar field, Saudi Arabia, clearly identify the class 1 large crystalline dolostone (Fig.…”
Section: (7b) Ln(s W ) = C(l) + D(l)ln(f)mentioning
confidence: 99%
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