Final Report - National Energy Technology Laboratory - U.S. ...

More documents

Recommendations

Info

Depth (ft) 0 5,000 10,000 15,000 20,000 25,000 0.465 psi/ft VIRGILIAN , , , MISSOURIAN 0 5,000 10,000 DESMOINESIAN "SKINNER" LEVEL 2 Pressure (psi) DESMOINESIAN "RED FORK" WOODFORD SHALE UPPER MORROWAN ORDOVICIAN-DEVONIAN "HUNTON" 15,000 20,000 Figure 4. Graphical representation of a pressure-depth profile lillustrating the relationship among Levels 1, 2, and 3. Note that Level 2 compartments are essentially clusters of isolated Level 3 compartments. This pressure-depth profile represents the Reydon-Cheyenne area in western Oklahoma. After Al-Shaieb et al. (1997).
GEOLOGIC SETTING The Appalachian basin extends southwestward from the Adirondack Mountains in New York to central Alabama. Figure 1 includes the area’s location . Structural boundaries include the Cincinnati arch in western Ohio, the Allegheny Front to the east, and the Blue Ridge of West Virginia. The basin is about 900 miles long and 300 miles wide and includes at least 100 million surface acres (Roth, 1964). The Appalachian basin originated as a sedimentary trough on the Precambrian surface that was later covered by Cambrian seas. Deposition of great masses of marine and continental sediments occurred throughout the Paleozoic Era. Carbonate and siliclastic tongues extended basinward from opposite margins synchronously in response to sea level drops. The interplay of eustatic sea-level drop and local tectonic uplift resulted in stratigraphic sequences bounded by widespread unconformities (Brett et al., 1990). Figure 2 shows correlation of the stratigraphy across the basin. Three major orogenic events affected the basin: the Taconic Orogeny (Late Ordovician), the Acadian Orogeny (Late Devonian), and the Allegheny Orogeny (Late Permian). 1 The geotectonic history of the basin includes the following stages: 1) Precambrian: metamorphic and igneous rocks of the Grenville deformation form a basement under the Appalachian Foreland. 2) Early and Middle Cambrian: offset of the basement surface associated with the formation of the Iapetus Ocean during Late Precambrian and Early Cambrian (Schumaker, 1996). 3) Upper Cambrian-Middle Ordovician: relative crustal stability and the formation of a broad carbonate shelf. In the Middle Ordovician, a Foreland basin develops from compression of the passive, carbonate-dominated continental margin during collision with an island arc system (Taconic Orogeny). Thick turbidite sequences record the early phases of the orogeny. 4) Late Ordovician (Ashgillian): waning of the main Taconic pulse, and deposition of the Bald Eagle-Oswego sandstone wedge and the Juniata-Queenston red bed sequences. 5) Late Ordovician to Early Silurian: tectonic rejuvenation of the Taconic Front. In New York State, evidence for a late Taconic pulse lies in the regionally extensive, low-angle unconformity at the Ordovician-Silurian boundary (Cherokee Unconformity). 6) Early Silurian (Cherokee Unconformity) and Late Silurian (Salinic Unconformity): eastward subsidence of the Appalachian Foreland Basin, which coincides with tectonic quiescence and thrust-load relaxation. A thick Early Silurian clastic wedge results from this subsidence. Westward migration in the foreland basin occurred during the Middle Silurian, depositing finer-grained strata; increased tectonism and onset of the Salinic Disturbance may have caused this migration. A small-scale unconformity at the Siluro-Devonian boundary may represent the latest Silurian tectonic activity (Brett et al., 1990). 7) Devonian-Late Permian: The Acadian (Devonian) and Allegheny orogenies (Late Permian) correlate to the collision of the North American plate with other continental plates, eventually creating Pangaea at the end of the Paleozoic (Schumaker, 1996). During the Allegheny (Appalachian) Orogeny, tremendous thrust pulses from the east and southeast intensely folded and faulted the rocks in the eastern area. The deformation becomes gradually less intense westward. The Ridge and Valley province shows the greatest folding of rocks. The Allegheny Orogeny primarily determined the present day geologic pattern dividing the area into two main parts–the Plateau province, and the Ridge and Valley province (Roth, 1964).
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: Depth (feet) 0 5,000 10,000 15,000
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 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 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 74 and 75:
Province, Play and Accumulation Nam
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
Page 84 and 85:
Page 86 and 87:
d.Overmaturity Overmature source ro
Page 88 and 89:
Penn Mississippian Devonian Sil Ord
Page 90 and 91:
120° 118° 116° 114° 0 20 North
Page 92 and 93:
EVIDENCE FOR BASIN-CENTERED GAS The
Page 94 and 95:
Production and Drilling Characteris
Page 96 and 97:
Stage Danian Tertiary Maastrichtian
Page 98 and 99:
GEOLOGIC SETTING The Eagle Ford For
Page 100 and 101:
Page 102 and 103:
System Series Stage Central Texas C
Page 104 and 105:
GEOLOGIC SETTING The Lower Cretaceo
Page 106 and 107:
Page 108 and 109:
97° 34° 33° 32° 31° 30° 29°
Page 110 and 111:
System Cretaceous Jurassic Upper Se
Page 112 and 113:
Page 114 and 115:
Economic Characteristics: Field Nam
Page 116 and 117:
Aproximate Depth (ft) 0 10,000 20,0
Page 118 and 119:
Depth (ft) 0 1,000 2,000 3,000 4,00
Page 120 and 121:
Page 122 and 123:
Page 124 and 125:
Sea Level Depth in Miles 10 20 A A'
Page 126 and 127:
GEOLOGIC SETTING The Michigan Basin
Page 128 and 129:
Economic Characteristics: b. Cumula
Page 130 and 131:
Era System Sequence West East Mesoz
Page 132 and 133:
GEOLOGIC SETTING The Mid-Continent
Page 134 and 135:
Page 136 and 137:
49° 45° 40° North Dakota South D
Page 138 and 139:
Depth (feet) 0 1000 2000 3000 4000
Page 140 and 141:
EVIDENCE FOR BASIN-CENTERED GAS Sev
Page 142 and 143:
Page 144 and 145:
Elevation in Feet 10,000 Sea Level
Page 146 and 147:
T36S T37S T38S T39S T40S T41S T48N
Page 148 and 149:
EVIDENCE FOR BASIN CENTERED-GAS The
Page 150 and 151:
Page 152 and 153:
System Pennsylvanian Series Formati
Page 154 and 155:
A A' Hermosa Formation Upper Member
Page 156 and 157:
Elevation (ft. msl) Elevation (ft.
Page 158 and 159:
Page 160 and 161:
Page 162 and 163:
System Tertiary Cretaceous Jurassic
Page 164 and 165:
B W T K K K & J Amoco State of Colo
Page 166 and 167:
EVIDENCE FOR BASIN-CENTERED GAS Nei
Page 168 and 169:
Page 170 and 171:
New Mexico Texas Huapache Flexure V
Page 172 and 173:
34° 33° 32° New Mexico Texas 0.4
Page 174 and 175:
Page 176 and 177:
R 71 W R 69 W R 67 W R 65 W R 63 W
Page 178 and 179:
R 71 W R 69 W R 67 W R 65 W R 63 W
Page 180 and 181:
R69W R68W R67W R66W R65W Huerfano C
Page 182 and 183:
Page 184 and 185:
SA W Mt LA 108° Colorado Plateau U
Page 186 and 187:
Feet 10,000 5,000 Sea Level -5,000
Page 188 and 189:
GEOLOGIC SETTING The present day Sa
Page 190 and 191:
Page 192 and 193:
Map Area Coast Ranges 38° 123° Sa
Page 194 and 195:
Depth in Feet 0 5000 10000 15000 20
Page 196 and 197:
EVIDENCE FOR BASIN-CENTERED GAS Acc
Page 198 and 199:
Page 200 and 201:
Depth in Kilometers 0 10 20 A A' Th
Page 202 and 203:
Depth in Feet 0 2,000 4,000 6,000 8
Page 204 and 205:
HYDROCARBON POTENTIAL In central Ut
Page 206 and 207:
Page 208 and 209:
Cenozoic Mesozoic Tertiary Cretaceo
Page 210 and 211:
40° 39° ⊥ ⊥ ⊥ Duchesne Carb
Page 212 and 213:
Several formations within the basin
Page 214 and 215:
Page 216 and 217:
System Quaternary Tertiary Cretaceo
Page 218 and 219:
GEOLOGIC SETTING The Snake River Do
Page 220 and 221:
Page 222 and 223:
U D A 13000 10000 12000 15000 A' 14
Page 224 and 225:
Series Depth Lith. Description Thic
Page 226 and 227:
GEOLOGIC SETTING As one of the larg
Page 228 and 229:
Page 230 and 231:
Kootenai Fm Morrison Fm Swift Sands
Page 232 and 233:
50° 00' 49° 00' 1 R o = 1.5% 7 2
Page 234 and 235:
HYDROCARBON PRODUCTION There is no
Page 236 and 237:
Page 238 and 239:
N Geologic Map Structure Map Therma
Page 240 and 241:
GEOLOGIC SETTING The Wasatch Platea
Page 242 and 243:
Page 244 and 245:
T. 12 S. T. 13 S. T. 14 S. T. 15 S.
Page 246 and 247:
Cenozoic Mesozoic Tertiary Cretaceo
Page 248 and 249:
EVIDENCE FOR BASIN-CENTERED GAS In
Page 250 and 251:
Page 252 and 253:
Years Ma (millions ago) 0 10 20 30
Page 254 and 255:
GEOLOGIC SETTING The western Colvil
Page 256 and 257:
Page 258 and 259:
Russia USA Herald Arch Chukchi Plat
Page 260 and 261:
Elevation in feet 5000 0 5000 10000
Page 262 and 263:
Elevation in Miles Elevation in Mil
Page 264 and 265:
-3550 Axis of Well -8476 Depth to t
Page 266 and 267:
Axis of AKK AKK 0.57 psi/ft 11080'
Page 268 and 269:
Beirei, M.A., 1987, Hydrocarbon mat
Page 270 and 271:
Corbett, K.P., Friedman, M., and Sp
Page 272 and 273:
Fuis, G.S., and Zucca, J.J., 1984,
Page 274 and 275:
Imperato, D.P., Nilsen, T.H., and M
Page 276 and 277:
Lingley, W.S., Jr., 1995, Petroleum
Page 278 and 279:
Neuhauser, K.R., 1988, Sevier-age r
Page 280 and 281:
Royse, F., 1996, Detachment fold tr
Page 282 and 283:
Tennyson, M.E., 1995, Eastern Washi
Page 284 and 285:
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
Page 290 and 291:
BOREHOLE TEMPERATURE DATA Previous
Page 292 and 293:
depth of about 8,350 ft. (2,545 m).
Page 294 and 295:
7 Region: The Geological Society of
Page 296 and 297:
CENOZOIC MESOZOIC PALEOZOIC ERA AGE
Page 298 and 299:
Km 2.5 0 -2.5 -5.0 -7.5 -10.0 WEST
Page 300 and 301:
N37° SAGUACHE ALAMOSA R 72 W R 70
Page 302 and 303:
Lucero Uplift B Ladron Mtns Nacimen
Page 304 and 305:
Lucero Uplift B Ladron Mtns Nacimen
Page 306 and 307:
Depth (feet) 25000 20000 15000 1000
Page 308 and 309:
Depth Subsurface (feet) 0 2000 4000
Page 310 and 311:
Rate of Oil Generation (mg/g TOC*my
Page 312 and 313:
NUMBER OF WILDCATS 10 9 8 7 6 5 4 3
Page 314 and 315:
ABSTRACT IS THERE A BASIN-CENTER GA
Page 316 and 317:
The Woodford Shale has been studied
Page 318 and 319:
An online database of pressure meas
Page 320 and 321:
Deep resistivities measured from du
Page 322 and 323:
MANY DEEP FORMATION TESTS PRODUCED
Page 324 and 325:
Perhaps the source rocks were too l
Page 326 and 327:
REFERENCES Al-Shaieb, Z., Alberta,
Page 328 and 329:
Oklahoma State University, Departme
Page 330 and 331:
NEW MEXICO 0 -5,000' 25 50 MILES 0
Page 332 and 333:
PERMIAN (PART) PENNSYLVANIAN MISSIS
Page 334 and 335:
DEPTH, IN THOUSANDS OF FEET 0 0 5 1
Page 336 and 337:
Well Name FIELD Sec. Twp. Rg. Forma
Page 338 and 339:
Well Name No. FIELD Sec. Twp. Rg. F
Page 340 and 341:
Well Name No. FIELD Sec. Twp. Rg. F
Page 342 and 343:
drilling, but best available data s
Page 344 and 345:
Cotton Valley lithofacies and assoc
Page 346 and 347:
DIAGENESIS OF COTTON VALLEY SANDSTO
Page 348 and 349:
SOURCE ROCKS Relatively scant infor
Page 350 and 351:
In the 1970s, production from low-p
Page 352 and 353:
(1984) and Dutton and others (1993)
Page 354 and 355:
As described above, Cotton Valley s
Page 356 and 357:
Gas-Water Contacts Perhaps the most
Page 358 and 359:
on the right side of Figure 16, min
Page 360 and 361:
20 sandstone trend is not indicativ
Page 362 and 363:
REFERENCES Almon, W.R., 1979, A geo
Page 364 and 365:
3 Meehan, D.N., and B.F. Pennington
Page 366 and 367:
5 Wescott, W.A., 1983, Diagenesis o
Page 368 and 369:
Table 1. Comparison of two producti
Page 370 and 371:
Field FERC Trap Disc CV Disc Date:
Page 372 and 373:
34° N 32° N 30° N APPROX UPDIP L
Page 374 and 375:
DALLAS ELLIS COLLIN ROCK- WALL OKLA
Page 376 and 377:
A SOUTH 1 WINN LIMESTONE 2 3 4 5 6
Page 378 and 379:
OKLAHOMA TEXAS LONE OAK DELTA COTTO
Page 380 and 381:
OK Dallas TX AR DETAIL AREA CALHOUN
Page 382 and 383:
OK AR Dallas TX Porosity DETAIL ARE
Page 384 and 385:
OK AR Dallas TX DETAIL AREA LA MS G
Page 386 and 387:
1477 1000 600 432 500 549 800 178,0
Page 388 and 389:
IS THERE A BASIN-CENTER GAS ACCUMUL
Page 390 and 391:
WELL HISTORIES AND FORMATION TEST D
Page 392 and 393:
CONCLUSIONS Pressures, temperatures
Page 394 and 395:
LAKE MICHIGAN 1000 500 0 Miles 100
Page 396 and 397:
SYSTEM ORDOVICIAN S CAMBRIAN U M L
Page 398 and 399:
LAKE MICHIGAN Burdell Leroy Reed Ci
Page 400 and 401:
FIELD NAME Sec. T. R. County Format
Page 402 and 403:
The Standard Oil Company drilled an
Page 404 and 405:
13,372-13,388 ft increased gas prod
Page 406 and 407:
CONCLUSIONS The Pasco basin has man
Page 408 and 409:
Lingley, W.S. Jr. And Walsh, T.J.,
Page 410 and 411:
A Scale: C DAN ELLENSBURG YAKIMA 6
Page 412 and 413:
PERIOD/ EPOCH PLEISTOCENE PLIOCENE
Page 414 and 415:
DEPTH, IN THOUSANDS OF FEET SOUTH N
Page 416 and 417:
1 POTENTIAL FOR A BASIN-CENTERED GA
Page 418 and 419:
workers such as Jiao and Surdam (19
Page 420 and 421:
DISCUSSION It has long been suspect
Page 422 and 423:
7 Johnson, R. C., Crovelli, R. A.,
Page 424 and 425:
9 Tschudy, R. H., Pillmore, C. I.,
Page 426 and 427:
TERTIARY MESOZOIC AGE PALEOCENE UPP
Page 428 and 429:
West East 40 Feet 1,000 Feet Coal S
Page 430 and 431:
DOES THE FORBES FORMATION IN THE SA
Page 432 and 433:
The Forbes Fm contains thick marine
Page 434 and 435:
CAUSE OF OVERPRESSURE Previous auth
Page 436 and 437:
Forbes gas is mostly methane, with
Page 438 and 439:
CONCLUSIONS Well data, drill stem t
Page 440 and 441:
Horan, E.P., 1992, Pressure-Tempera
Page 442 and 443:
Williams, T.A., Graham, S.A., and C
Page 444 and 445:
40° 00' 39° 30' 39° 00' A 122°
Page 446 and 447:
SYSTEM SERIES QUATER. TERTIARY CRET
Page 448 and 449:
Depth, in thousands of feet SEA LEV
Page 450 and 451:
Depth, in thousands of feet 0 - 5 -
Page 452 and 453:
7N 6N 5N 4N 3N 2N 1N 1S C KIRBY KIR
Page 454 and 455:
Table 2. Mud weights (lb/cubic ft),
Page 456 and 457:
Table 3. Mud weights (lb/cubic ft),
Page 458 and 459:
within the upper 500 feet of the Tr
Page 460 and 461:
As shown in figure 2, the Travis Pe
Page 462 and 463:
Across the Travis Peak hydrocarbon-
Page 464 and 465:
High-Sinuosity Fluvial System High-
Page 466 and 467:
Porosity Porosity and permeability
Page 468 and 469:
BURIAL AND THERMAL HISTORY Vitrinit
Page 470 and 471:
HYDROCARBON-WATER CONTACTS Based on
Page 472 and 473:
in Figures 13 and 14. Multiple valu
Page 474 and 475:
Travis Peak sandstones where it was
Page 476 and 477:
depleting and giving way to water p
Page 478 and 479:
22 Peak in northeast Texas, limited
Page 480 and 481:
2 Herald, F.A., ed., 1951, Occurren
Page 482 and 483:
4 Shreveport Geological Society, 19
Page 484 and 485:
Field County State Discovery Trap D
Page 486 and 487:
Hill Falls OK DETAIL AREA TX Ellis
Page 488 and 489:
Amite St Helena Hinds Copiah Lincol
Page 490 and 491:
34° N 32° N 30° N ANCESTRAL RED
Page 492 and 493:
Depth, in Feet 0 1000 2000 3000 400
Page 494 and 495:
Depth (feet) 5000 6000 7000 8000 90
Page 496 and 497:
TEXAS LOUISIANA Miller Cass Lafayet
Page 498 and 499:
Cass Marion Harrison TEXAS LOUISIAN
Page 500 and 501:
TEXAS LOUISIANA Miller Cass Lafayet
Page 502 and 503:
The following talk was presented at
Page 504 and 505:
Basin or Area Evaluation of Area fo
Page 506:
Basin or Area Evaluation of Area fo
show all

Final Report - National Energy Technology Laboratory - U.S. ...

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?