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Relative Stratigraphic Position (ft)* 15000 10000 5000 0 -5000 -10000 1 2 3 4 5 6 7 8 9 10 * Mean Vitrinite Reflectance (% R o )* Estimated Woodford-Chattanooga top Estimated Arbuckle top Latimer County, OK Sebastian County, OK Yell County, AR Logan County, AR Faulkner County, AR White County, AR Stratigraphic position relative to top of basal Atokan (Spiro/Orr) sandstone Figure 4. Depth vs. vitrinite reflectance profile for wells in Arkansas and Oklahoma. These profiles use the Spiro sandstone as a stratigraphic datum and indicate that thermal maturity of eastern Arkansas wells does not follow the inferred west-to-east increase in maturity across the basin. After Horn and Curtis (1996) and Houseknecht et al. (1992).
GEOLOGIC SETTING The Black Warrior basin of Alabama and Mississippi is a foreland basin located in the major structural reentrant between the Appalachian fold-and-thrust belt to the southeast and the Ouachita fold-and-thrust belt to the southwest. Figure 1 shows the basin location and its major structural features. The northern margin of the basin is bounded by the Nashville dome. The basin is shaped like a kite with its tail facing south, and has a surface area of about 35,000 square miles. North to south, the basin extends about 190 miles, and the east-west width is about 220 miles. The overall sedimentary section in the province includes rocks of Paleozoic, Mesozoic and Cenozoic age that range in thickness from about 7,000 ft along the northern margin to about 31,000 ft in the depocenter located in eastern Mississippi (Ryder, 1994). The geotectonic history of the basin includes 5 stages: 1) Late Precambrian-Early Cambrian rift with associated deposition of coarse clastics. 2) Middle Cambrian-Mississippian period of stable shelf deposition (7000 ft of shallow water carbonates) occurring on a passive continental margin. 3) Late Mississippian (Chester) transitional episode; early stages of continental collision, marine deltaic sedimentation and several major regressive-transgressive cycles. 4) Early-Late (?) Pennsylvanian time of maximum basin subsidence and synorogenic deposition related to maturation of the Appalachian-Ouachita thrust belts. Following a brief period of barrier bar development, thick clastic wedges prograded from source areas along the south margin. Abundant coal bed development in north-central portion of the basin. 5) Permian-Cretaceous erosion/non-deposition ending with Late Cretaceous marine incursion and deposition into Early Tertiary shallow marine sediments (Mississippi Embayment). Figure 2 shows a regional cross section of Mississippian strata across northwestern Alabama. The Black Warrior basin was first downwarped in the Late Mississippian-Early Pennsylvanian and then subsequently filled by Pennsylvanian shallow marine and terrestrial clastic material shed from rising highlands along its southern margin. No Permian or early Mesozoic deposits exist in the basin. Indications are that the Black Warrior was uplifted above sea level in Latest Pennsylvanian-Early Mesozoic time (Petroleum Information Corp, 1986). Continental break-up during the Mesozoic resulted in the basin becoming downwarped to the southwest and eventually covered by the Mississippi Embayment marine transgressive episode (Mancini et al., 1983). Most of the basin and its thrust faulted margins are concealed beneath Tertiary and Cretaceous rocks of the Gulf coastal plain and the Mississippi embayment. 1
Page 1 and 2: Central Alaska Colville/ North Slop
Page 3 and 4: TABLE OF CONTENTS Scope of Assessme
Page 5 and 6: SCOPE OF THE ASSESSMENT The scope o
Page 7 and 8: BASIN-CENTERED/CONTINUOUS-TYPE ACCU
Page 9 and 10: LIST OF POTENTIAL BASIN-CENTERED GA
Page 11 and 12: Accumulation Region Province Notes
Page 13 and 14: ACKNOWLEDGEMENTS Various individual
Page 15 and 16: Province, Play and Accumulation Nam
Page 17 and 18: AMARILLO UPLIFT Oklahoma Texas 100
Page 19 and 20: Depth (feet) 0 5,000 10,000 15,000
Page 21 and 22: GEOLOGIC SETTING The Appalachian ba
Page 23 and 24: EVIDENCE FOR BASIN-CENTERED GAS Whi
Page 25 and 26: Production and Drilling Characteris
Page 27 and 28: N Kentucky Ohio Sandstone reservoir
Page 29 and 30: GEOLOGIC SETTING The Arkoma Basin f
Page 33 and 34: 35° 34° Atoka 96° 95° 94° 93°
Page 35: System Pennsylvanian Mississippian
Page 41 and 42: e.Basin maturity mature f.Sediment
Page 43 and 44: A A' Clastic rocks Carbonate rocks
Page 45 and 46: GEOLOGIC SETTING The interior basin
Page 47 and 48: EVIDENCE FOR BASIN-CENTERED GAS In
Page 51 and 52: System Tertiary Sandstone, mudstone
Page 53 and 54: GEOLOGIC SETTING The Late Proterozo
Page 58 and 59: GEOLOGIC SETTING The Columbia Basin
Page 62 and 63: 47° 46° 121° 120° 119° BN 23-3
Page 64 and 65: GEOLOGIC SETTING The Cook Inlet bas
Page 68 and 69: 62° 60° 58° Bruin Bay Fault Aleu
Page 70 and 71: Sea Level Depth (in feet) 1 2 3 4 5
Page 72 and 73: GEOLOGIC SETTING The Denver basin i
Page 76 and 77: 42° 41° 40° 39° | | | | | | 105
Page 78 and 79: Era Cenozoic Mesozoic Paleozoic Ter
Page 80 and 81: Depth (ft) 0 1,000 2,000 3,000 4,00
Page 82 and 83: GEOLOGIC SETTING The Great Basin is
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d.Overmaturity Overmature source ro
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Penn Mississippian Devonian Sil Ord
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120° 118° 116° 114° 0 20 North
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EVIDENCE FOR BASIN-CENTERED GAS The
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Production and Drilling Characteris
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Stage Danian Tertiary Maastrichtian
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GEOLOGIC SETTING The Eagle Ford For
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System Series Stage Central Texas C
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GEOLOGIC SETTING The Lower Cretaceo
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Province, Play and Accumulation Nam
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97° 34° 33° 32° 31° 30° 29°
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System Cretaceous Jurassic Upper Se
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Economic Characteristics: Field Nam
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Aproximate Depth (ft) 0 10,000 20,0
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Depth (ft) 0 1,000 2,000 3,000 4,00
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Page 122 and 123:
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Sea Level Depth in Miles 10 20 A A'
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GEOLOGIC SETTING The Michigan Basin
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Economic Characteristics: b. Cumula
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Era System Sequence West East Mesoz
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GEOLOGIC SETTING The Mid-Continent
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49° 45° 40° North Dakota South D
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Depth (feet) 0 1000 2000 3000 4000
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EVIDENCE FOR BASIN-CENTERED GAS Sev
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Elevation in Feet 10,000 Sea Level
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T36S T37S T38S T39S T40S T41S T48N
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EVIDENCE FOR BASIN CENTERED-GAS The
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System Pennsylvanian Series Formati
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A A' Hermosa Formation Upper Member
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Elevation (ft. msl) Elevation (ft.
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Page 160 and 161:
Page 162 and 163:
System Tertiary Cretaceous Jurassic
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B W T K K K & J Amoco State of Colo
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EVIDENCE FOR BASIN-CENTERED GAS Nei
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New Mexico Texas Huapache Flexure V
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34° 33° 32° New Mexico Texas 0.4
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Page 176 and 177:
R 71 W R 69 W R 67 W R 65 W R 63 W
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R 71 W R 69 W R 67 W R 65 W R 63 W
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R69W R68W R67W R66W R65W Huerfano C
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Page 184 and 185:
SA W Mt LA 108° Colorado Plateau U
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Feet 10,000 5,000 Sea Level -5,000
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GEOLOGIC SETTING The present day Sa
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Map Area Coast Ranges 38° 123° Sa
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Depth in Feet 0 5000 10000 15000 20
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EVIDENCE FOR BASIN-CENTERED GAS Acc
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Depth in Kilometers 0 10 20 A A' Th
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Depth in Feet 0 2,000 4,000 6,000 8
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HYDROCARBON POTENTIAL In central Ut
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Cenozoic Mesozoic Tertiary Cretaceo
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40° 39° ⊥ ⊥ ⊥ Duchesne Carb
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Several formations within the basin
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System Quaternary Tertiary Cretaceo
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GEOLOGIC SETTING The Snake River Do
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U D A 13000 10000 12000 15000 A' 14
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Series Depth Lith. Description Thic
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GEOLOGIC SETTING As one of the larg
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Kootenai Fm Morrison Fm Swift Sands
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50° 00' 49° 00' 1 R o = 1.5% 7 2
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HYDROCARBON PRODUCTION There is no
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Page 238 and 239:
N Geologic Map Structure Map Therma
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GEOLOGIC SETTING The Wasatch Platea
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T. 12 S. T. 13 S. T. 14 S. T. 15 S.
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Cenozoic Mesozoic Tertiary Cretaceo
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EVIDENCE FOR BASIN-CENTERED GAS In
Page 250 and 251:
Page 252 and 253:
Years Ma (millions ago) 0 10 20 30
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GEOLOGIC SETTING The western Colvil
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Russia USA Herald Arch Chukchi Plat
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Elevation in feet 5000 0 5000 10000
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Elevation in Miles Elevation in Mil
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-3550 Axis of Well -8476 Depth to t
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Axis of AKK AKK 0.57 psi/ft 11080'
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Beirei, M.A., 1987, Hydrocarbon mat
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Corbett, K.P., Friedman, M., and Sp
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Fuis, G.S., and Zucca, J.J., 1984,
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Imperato, D.P., Nilsen, T.H., and M
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Lingley, W.S., Jr., 1995, Petroleum
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Neuhauser, K.R., 1988, Sevier-age r
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Royse, F., 1996, Detachment fold tr
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Tennyson, M.E., 1995, Eastern Washi
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SELECTED BIBLIOGRAPHY Allison, M.L.
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Meylan, M.A., 1997, Controls on the
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1 POTENTIAL FOR A BASIN-CENTERED GA
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BOREHOLE TEMPERATURE DATA Previous
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depth of about 8,350 ft. (2,545 m).
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7 Region: The Geological Society of
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CENOZOIC MESOZOIC PALEOZOIC ERA AGE
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Km 2.5 0 -2.5 -5.0 -7.5 -10.0 WEST
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N37° SAGUACHE ALAMOSA R 72 W R 70
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Lucero Uplift B Ladron Mtns Nacimen
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Lucero Uplift B Ladron Mtns Nacimen
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Depth (feet) 25000 20000 15000 1000
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Depth Subsurface (feet) 0 2000 4000
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Rate of Oil Generation (mg/g TOC*my
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NUMBER OF WILDCATS 10 9 8 7 6 5 4 3
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ABSTRACT IS THERE A BASIN-CENTER GA
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The Woodford Shale has been studied
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An online database of pressure meas
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Deep resistivities measured from du
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MANY DEEP FORMATION TESTS PRODUCED
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Perhaps the source rocks were too l
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REFERENCES Al-Shaieb, Z., Alberta,
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Oklahoma State University, Departme
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NEW MEXICO 0 -5,000' 25 50 MILES 0
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PERMIAN (PART) PENNSYLVANIAN MISSIS
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DEPTH, IN THOUSANDS OF FEET 0 0 5 1
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Well Name FIELD Sec. Twp. Rg. Forma
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Well Name No. FIELD Sec. Twp. Rg. F
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Well Name No. FIELD Sec. Twp. Rg. F
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drilling, but best available data s
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Cotton Valley lithofacies and assoc
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DIAGENESIS OF COTTON VALLEY SANDSTO
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SOURCE ROCKS Relatively scant infor
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In the 1970s, production from low-p
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(1984) and Dutton and others (1993)
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As described above, Cotton Valley s
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Gas-Water Contacts Perhaps the most
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on the right side of Figure 16, min
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20 sandstone trend is not indicativ
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REFERENCES Almon, W.R., 1979, A geo
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3 Meehan, D.N., and B.F. Pennington
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5 Wescott, W.A., 1983, Diagenesis o
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Table 1. Comparison of two producti
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Field FERC Trap Disc CV Disc Date:
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34° N 32° N 30° N APPROX UPDIP L
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DALLAS ELLIS COLLIN ROCK- WALL OKLA
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A SOUTH 1 WINN LIMESTONE 2 3 4 5 6
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OKLAHOMA TEXAS LONE OAK DELTA COTTO
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OK Dallas TX AR DETAIL AREA CALHOUN
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OK AR Dallas TX Porosity DETAIL ARE
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OK AR Dallas TX DETAIL AREA LA MS G
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1477 1000 600 432 500 549 800 178,0
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IS THERE A BASIN-CENTER GAS ACCUMUL
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WELL HISTORIES AND FORMATION TEST D
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CONCLUSIONS Pressures, temperatures
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LAKE MICHIGAN 1000 500 0 Miles 100
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SYSTEM ORDOVICIAN S CAMBRIAN U M L
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LAKE MICHIGAN Burdell Leroy Reed Ci
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FIELD NAME Sec. T. R. County Format
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The Standard Oil Company drilled an
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13,372-13,388 ft increased gas prod
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CONCLUSIONS The Pasco basin has man
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Lingley, W.S. Jr. And Walsh, T.J.,
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A Scale: C DAN ELLENSBURG YAKIMA 6
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PERIOD/ EPOCH PLEISTOCENE PLIOCENE
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DEPTH, IN THOUSANDS OF FEET SOUTH N
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1 POTENTIAL FOR A BASIN-CENTERED GA
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workers such as Jiao and Surdam (19
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DISCUSSION It has long been suspect
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7 Johnson, R. C., Crovelli, R. A.,
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9 Tschudy, R. H., Pillmore, C. I.,
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TERTIARY MESOZOIC AGE PALEOCENE UPP
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West East 40 Feet 1,000 Feet Coal S
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DOES THE FORBES FORMATION IN THE SA
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The Forbes Fm contains thick marine
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CAUSE OF OVERPRESSURE Previous auth
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Forbes gas is mostly methane, with
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CONCLUSIONS Well data, drill stem t
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Horan, E.P., 1992, Pressure-Tempera
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Williams, T.A., Graham, S.A., and C
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40° 00' 39° 30' 39° 00' A 122°
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SYSTEM SERIES QUATER. TERTIARY CRET
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Depth, in thousands of feet SEA LEV
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Depth, in thousands of feet 0 - 5 -
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7N 6N 5N 4N 3N 2N 1N 1S C KIRBY KIR
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Table 2. Mud weights (lb/cubic ft),
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Table 3. Mud weights (lb/cubic ft),
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within the upper 500 feet of the Tr
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As shown in figure 2, the Travis Pe
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Across the Travis Peak hydrocarbon-
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High-Sinuosity Fluvial System High-
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Porosity Porosity and permeability
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BURIAL AND THERMAL HISTORY Vitrinit
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HYDROCARBON-WATER CONTACTS Based on
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in Figures 13 and 14. Multiple valu
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Travis Peak sandstones where it was
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depleting and giving way to water p
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22 Peak in northeast Texas, limited
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2 Herald, F.A., ed., 1951, Occurren
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4 Shreveport Geological Society, 19
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Field County State Discovery Trap D
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Hill Falls OK DETAIL AREA TX Ellis
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Amite St Helena Hinds Copiah Lincol
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34° N 32° N 30° N ANCESTRAL RED
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Depth, in Feet 0 1000 2000 3000 400
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Depth (feet) 5000 6000 7000 8000 90
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TEXAS LOUISIANA Miller Cass Lafayet
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Cass Marion Harrison TEXAS LOUISIAN
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TEXAS LOUISIANA Miller Cass Lafayet
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The following talk was presented at
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Basin or Area Evaluation of Area fo
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Basin or Area Evaluation of Area fo
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