Part 4 - Berg - Hughes Center

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Figure 353. (A) Thermal-maturity and migration modeling at the initiation of oil expulsion during the Early Cretaceous in the southern part of the basin based on the geologic model constructed from cross section D-D’. (B) Thermal-maturity and migration modeling at peak dry-gas expulsion during the early Late Cretaceous in the southern part of the basin. See Figure 2 for the location of cross section D-D’. 421
Figure 354. (A) Thermal-maturity and migration modeling at the initiation of oil expulsion during the Early Cretaceous in the southern part of the basin based on the geologic model constructed from cross section J-J’. (B) Thermal-maturity and migration into the Monroe uplift area during the early Eocene from the southern part of the basin. See Figure 2 for location of the cross section J-J’. 422
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time frame spanning from approximat
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the same well, Pennsylvanian plant
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Louann Salt The Louann Salt conform
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Norphlet deposition, in southern Ar
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Haynesville-Buckner Formation Produ
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Caddo, Bossier, Webster, Claiborne,
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Smackover limestone. The Bossier gr
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Lower Cretaceous Coahuila (Hosston,
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system that includes a variety of d
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greater than 90 md, most of the Tra
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contains approximately 13 producing
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Pine Island shale, averaging 250 ft
Page 25 and 26: 10%. Calcite-lined vugs and intergr
Page 27 and 28: Lake Anhydrite was deposited above
Page 29 and 30: Sabine, Franklin, Tensas Shallow wa
Page 31 and 32: Across northern Louisiana in the pr
Page 33 and 34: Taylor Group Producing Parishes Cad
Page 35 and 36: 2,000 to 2,500 ft with net pay of 1
Page 37 and 38: productive in east-central Louisian
Page 39 and 40: North Louisiana Salt Basin. The str
Page 41 and 42: Louisiana Salt Basin. Lower Cretace
Page 43 and 44: Table 2. Oil and gas production for
Page 45 and 46: 1987; Claypool and Mancini, 1989; M
Page 47 and 48: Figure 329. Cross section A-A’. G
Page 49 and 50: generation (Table 4). The following
Page 51 and 52: Table 5. Cotton Valley-Bossier Grou
Page 53 and 54: Table 6. Cotton Valley-Group sample
Page 55 and 56: Table 7. Wells used to construct th
Page 57 and 58: Figure 336. Electric logs for wells
Page 59 and 60: Figure 338. Thin section micrograph
Page 61 and 62: Figure 340. Amoco CZ 5-7 well elect
Page 63 and 64: Table 9. Total organic carbon, rock
Page 65 and 66: Figure 343. HI versus OI diagram. T
Page 67 and 68: Figure 345. Rock-Eval pyrolysis ana
Page 69 and 70: Figure 347. Visual kerogen analyses
Page 71 and 72: gas with some oil, not only within
Page 73 and 74: Figure 350. Burial history profile
Page 75: Figure 352. Hydrocarbon expulsion p
Page 79 and 80: Figure 356. Cross section A-A’ sh
Page 81 and 82: Figure 360. Cross section J-J’ sh
Page 83 and 84: Figure 364. Seismic cross section B
Page 85 and 86: of secondary, non-associated thermo
Page 87 and 88: RESULTS AND DISCUSSION Geologic His
Page 89 and 90: peripheral fault trend and numerous
Page 91 and 92: oundary between thick transitional
Page 93 and 94: Cretaceous reservoirs have shown th
Page 95 and 96: from the southern part of the basin
Page 97 and 98: Reservoir Assessment Comparison of
Page 99 and 100: For example, Upper Cretaceous sands
Page 101 and 102: The Upper Jurassic to Lower Cretace
Page 103 and 104: Bishop, W.F., 1968, Petrology of up
Page 105 and 106: Dawson, W.C., and Callender, C.A.,
Page 107 and 108: Fisher, W.L., and McGowen, J.H., 19
Page 109 and 110: Hermann, L.A., J.A. Lott, and R.E.
Page 111 and 112: Mancini, E.A., M. Badali, T.M. Puck
Page 113 and 114: McCulloh, R.P., and Eversull, L.G.,
Page 115 and 116: Source Rock Potential of Carbonate
Page 117 and 118: Salvador, A., 1991b, Triassic-Juras
Page 119 and 120: Tolson, J.S., C.W. Copeland, and B.
Page 121: Zimmerman, R.K., 1999a, A potential
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