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Economic Characteristics: a. High inert gas content in Ohio, average Clinton-Medina Nitrogen content is 5.1%, Carbon Dioxide content is 0.1% (Hugman et al., 1993). In the Rome Trough and adjacent areas, very high inerts in natural gas have been reported from pre-Knox rocks, sometimes rendering the gas non-combustible (up to 78% Nitrogen) b. Recovery Low. Continuous-type accumulations are characterized by low individual well-production rates and small well-drainage area. Directional/horizontal wells are being drilled to reduce the number of well sites. c. Pipeline infrastructure very good There are numerous gas lines in the basin. d. Overmaturity none e. Basin maturity mature f. Sediment consolidation consolidation/porosity reduction occurs with depth of burial g. Porosity/completion problems tight sands. Improved hydraulic fracturing techniques in recent years resulted in higher gas recoveries. h. Permeability pre-Knox=1.0 md (Innerkip field, Oxford Co., Ontario) i. Porosity pre-Knox=3.5 to 22% (Innerkip field, Ontario)
N Kentucky Ohio Sandstone reservoir for gas Sandstone reservoir for oil Oil and gas field Basin-centerd gas accumulation Ontario Lake Erie West Virginia Lake Ontario Approximate updip limit of basincentered gas accumulation Approximate updip limit of Tuscarora Sandstone Pennsylvania Well location with show of gas or oil New York 0 50 mi Figure 1. Map showing regional hydrocarbon accumulation in Lower Silurian sandstone reservoirs of the Appalachian basin. Oil and gas shows seen in wells are from pre-Knox units. After Harris and Baranoski (1996), and Ryder (1998).
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: Production and Drilling Characteris
Page 29 and 30: GEOLOGIC SETTING The Arkoma Basin f
Page 33 and 34: 35° 34° Atoka 96° 95° 94° 93°
Page 35 and 36: System Pennsylvanian Mississippian
Page 37 and 38: GEOLOGIC SETTING The Black Warrior
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 49 and 50: Production and Drilling Characteris
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
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Era Cenozoic Mesozoic Paleozoic Ter
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Depth (ft) 0 1,000 2,000 3,000 4,00
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GEOLOGIC SETTING The Great Basin is
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Province, Play and Accumulation Nam
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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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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:
Page 124 and 125:
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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Page 144 and 145:
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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Page 208 and 209:
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
Page 236 and 237:
Page 238 and 239:
N Geologic Map Structure Map Therma
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GEOLOGIC SETTING The Wasatch Platea
Page 242 and 243:
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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:
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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
Page 278 and 279:
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.
Page 286 and 287:
Meylan, M.A., 1997, Controls on the
Page 288 and 289:
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).
Page 294 and 295:
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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