FORT BERTHOLD RESERVATION List of Topics
BACKGROUND Reservation Overview Production Overview
GEOLOGIC OVERVIEW Geologic History Petroleum Systems Summary of Play Types
CONVENTIONAL PLAY TYPES Play 1 - Folded Structure-Mississippian Carbonate Play� Play 2 - Mississippian Shoreline Play� Play 3 - Mississippian Lodgepole Waulsortian Mounds� Play 4 - Ordovician Red River Play Play 5 - Devonian Nisku-Duperow Play Play 6 - Pre-Prairie (Winnipegosis/Interlake Play) Play 7 - Post Madison Clastics (Tyler-Heath) Play 8 - Pre-Red River Gas Play Play 9 - Bakken Fairway/Sanish Sand Play� �
UNCONVENTIONAL / HYPOTHETICAL PLAY TYPES Play 10 - Niobrara Microbial Gas Play
REFERENCES
OVERVIEW there are approximately 10 formations proved to be productive in the Fort FORT BERTHOLD RESERVATION Berthold area. Of further note, the facies distribution during lower Mississippian
time strongly suggests that Lodgepole trends are present on the Fort Berthold The Three Affiliated Tribes Indian Reservation (USGS). � The Three Affiliated Tribes have purchased seismic data from lines located in
Tribal Headquarter: New Town, North Dakota the western portion of the Reservation, which may be examined by parties Geologic Setting: � Williston Basin interested in oil and gas exploration. Some of the seismic data will be
reprocessed and may be correlated with borehole logs. Sections and data tapes Introduction reside with the Division of Energy and Minerals Resources of the Bureau of � The Fort Berthold Indian Reservation is located in west-central North Dakota Indian Affairs located in Denver, CO. approximately thirty miles southwest of the city of Minot. The Reservation contains portions of Dunn, McKenzie, McLean, Mercer, Mountrail and Ward Area Location and Access Counties and includes an area of about 1,530 square miles or 980,000 acres. � Fort Berthold Indian Reservation comprises parts of Dunn, McKenzie, These lands are located 15 miles east of the center of the Williston Basin, a McLean, Mercer, Mountrail, and Ward Counties in west-central North Dakota geologic area where undiscovered accumulations of oil and gas may be located. (Figure 1), near the confluence of the Missouri and Little Missouri River valleys. � Several studies have been published over the years which indicate high Total area is about 1,530 square miles, approximately 11 percent of which is potential for undiscovered oil and gas reserves on the Fort Berthold Reservation. covered by waters impounded by Garrison Dam (Lake Sakakawea). The lake There has been past interest exhibited by oil companies, however, high royalties, divides the reservation into four distinct areas, here referred to as the western, high lease acquisition costs, inability to assemble large blocks of acreage, rights southern, eastern, and north-central segments. to seismic data, Tribal Employment Rights Office (TERO) regulations, taxes, and � Although reservoir waters somewhat impede travel between the four land a 100 percent signature requirement imposed by the federal statute on Trust lands segments, most of the reservation is accessible over a system of State highways have served as deterrents to oil and gas exploration on the Reservation. The 100 and local roads. Rail service is provided to the northern part of the reservation by percent signature requirement regulation has made exploration on Tribal Allotted the Soo Line Railroad. A main east-west line of the Burlington Northern passes Lands nearly impossible to carry out due to the high fragmentation caused by within 7 miles of the reservation, roughly paralleling the southern boundary. heirship. The Tribes are currently working to correct these problems to open the door for future gas and oil exploration and development. The Three Affiliated Physiography Tribes are striving to work closer with oil companies to make oil and gas � The Fort Berthold Indian Reservation includes land that ranges from rugged exploration on Fort Berthold competitive with lands outside of the Reservation. badlands to rolling plains. Altitudes range from about 1,850 feet at Lake � The Fort Berthold Reservation possesses all the requisites for commercial Sakakawea to over 2,600 feet on Phaelen's Butte near Mandaree. The reservation petroleum development. According to an oil and gas study authorized by Joe H. is within the Northern Great Plains Physiographic Province and may be divided Rawlings, source rocks and reservoir caprock combinations are in evidence from into four physiographic units: (1) the Coteau Slope; (2) the Missouri River trench the Antelope field located near the northwest corner of the Reservation. This (now flooded); (3) the Missouri Plateau; and (4) the Little Missouri Badlands. field produces both oil and gas from four different zones. The relatively new South of Lake Sakakawea the reservation has a bedrock surface with scattered Plaza field, located near the east exterior boundary, is also a major producing oil areas of glacial drift. North of the lake, glacial deposits predominate and only field. Other fields were recently discovered on the Reservation while drilling the patches of bedrock crop out. The landscape reflects this distribution of sediments: Bakken and Mission Canyon formations. This multiplicity of geologic structures south of the lake, hills and badlands are common; north of the lake the glaciated argues the presence of the many deep traps. Regardless of the development of topography is mainly undulating to rolling. these fields, much of the Reservation has not been explored for accumulations of � The reservation area north of Lake Sakakawea is part of the Coteau Slope, oil and gas. which has both erosional and glacial landforms with glacial predominating. � The Williston Basin, which encompasses the Reservation, has a long history Gentle slopes characterize 50 to 80 percent of the area and local relief ranges of production. Much of the oil in this area was sourced by the organically rich from 50 to 200 feet. The Little Missouri Badlands lie adjacent to the Little Bakken Formation. New horizontal drilling technology has made production Missouri River south and west of Lake Sakakawea as well as in a few restricted from Bakken source rocks possible. A report written for the Bureau of Indian areas along the Missouri River. They consist of rugged, deeply-eroded, Affairs by Susan Race Wager, states that the Fort Berthold Reservation is hilly land in which gentle slopes characterize only 20 to 50 percent of the area favorably located for exploration in the Bakken Formation. and local relief is commonly over 500 feet. Areas other than badlands south and � According to George Long of the Bureau of Land Management (BLM), there west of the lake are part of the Missouri Plateau. In these areas, gentle slopes have been 571 tests for oil and gas on or immediately adjacent to the Fort characterize about 50 to 70 percent of the area and local relief ranges from 300 to Berthold Reservation resulting in a total of 392 producing wells and 179 plugged 500 feet. and abandoned wells; a 69% success ratio. The majority of these 179 plugged � The Missouri and Little Missouri Rivers and their larger tributaries have cut and abandoned wells did report oil and gas shows. Of special interest, there deeply into the bedrock and glacial deposits of various compositions. The appears to be production potential in the Mississippian Charles Formation which Missouri River is 300 to 500 feet below the upland plain. Near the western has been bypassed in all of the wells drilled except those few that are too shallow boundary of the reservation, the Little Missouri River has eroded a channel more to reach the Charles Formation located in the Mission Canyon. than 600 feet deep. Occasional ridges and bare buttes extend as much as 400 feet � Water saturation calculations were made on 60 wells to evaluate possible above the plain. bypassed production in the Mississippian Charles Formation. Possible oil and gas production was indicated in 52 of these 60 wells. According to the BLM,
Land Status � The Fort Berthold Indian Reservation was established by the Fort Laramie Treaty of September 17, 1851, for the Arikara, Mandan, and Hidatsa Tribes of Indians who later united to form the Three Affiliated Tribes. Executive Orders and Congressional Acts have limited the reservation to its present boundaries. The act of June 1, 1910, 36 Stat. 455, opened unallotted and unsold reservation lands to non Indians, thus creating the "ceded and diminished lands" boundary. It was assumed by many that only the remaining lands comprised the Fort Berthold Indian Reservation. A Federal appeals court (8th Cir. 1972), however, ruled that the 1910 Act did not change reservation boundaries and that the "homestead" (ceded) area remained a part of the reservation (City of New Town vs. United States, 454 F 2d 121) Public Law 437 and the Act of July 31, 1947 (amended October 29, 1947) made provision for lands inundated by the Garrison Dam reservoir. Table 1 summarizes the present extent of land holdings on the Fort Berthold Indian Reservation. Most of the north and northeast part of the reservation (the homestead area) is in private ownership. Land status data are from Bureau of Indian Affairs records. � Nearly 54 percent of the reservation's subsurface mineral rights are owned by the Three Affiliated Tribes. Mineral rights in the diminished reservation area are all tribally owned with the exception of 164.09 acres owned by the Federal government. The Tribes also retain mineral ownership for 110,623.13 acres of the homestead area. Lands in the Garrison reservoir area were severed.
Percentage
Classification � Acreage of total
Diminished Reservation Area Tribally-owned lands.� 57,954.20� 5.91 Allotted lands� 360,438.57� 36.76 Government-owned land� 164.09� 0.01 Privately owned (alienated) land� 55,865.14� 5.70
Subtotal� 474,422.00� 48.38
Reservoir Taking Area� 152,359.95� 15.54 Homestead (ceded) Area.� 353,792.59� 36.08 Total area of reservation.�
980,574.54� 100.00
TABLE 1 - Summary of land ownership, Fort Berthold Indian Reservation, N. Dakota
Contacts Inquiries concerning oil and gas leases on the Fort Berthold Reservation may
be directed to the Three Affiliated Tribes Natural Resources Department -telephone (701) 627-3627 or the Bureau of Indian Affairs, located in New Town,
North Dakota - (701) 627-3741.
85
73
94
2 8
94
83
52
52
8385
200
Williston
Stanley
Watford City
Minot
Underwood
Bismark
Belfield Dickinson
Beach
Williams
McKenzie
Billings Dunn
Mountrail
Ward
McHenry
McLean
Mercer
Oliver
Sheridan
Burleigh
Morton
FORT BERTHOLD
New Town
MO
NT
AN
AN
OR
TH
DA
KO
TA
Fort Berthold Reservation North Dakota OVERVIEW
Page 1 of 18
INTRODUCTION Fort Berthold Reservation
Williston Basin � Over 700 MMBO have been produced from the Williston Basin, one of the largest cratonic basins in North America. The reservation is ideally situated for numerous exploration targets within this basin. Several source rock horizons, including the world renown Bakken Formation, contribute to the prolific nature of the basin. � The Williston Basin contains an estimated mean value of 650 MMBO and 1.69 TCFG from undiscovered resources in conventional plays. Multiple episodes of maturation and migration occurred during Permian-Cretaceous time from these source intervals. Understanding the trapping mechanisms and migration pathways are critical to successful future exploration within the reservation area. Carbonate reservoirs in Paleozoic formations have been the primary focus of hydrocarbon exploration. Recent exploration targets include microbial gas in Cretaceous sediments and deep Paleozoic sandstone intervals.
Early Exploration in the Williston Basin and Fort Berthold Reservation � Early discoveries were made on large surface structures such as Nesson and Cedar Creek Anticlines, and Poplar Dome. The Williston Basin is distinctive among other Rocky Mountain basins because of its continuous basin subsidence and burial history throughout Paleozoic and Mesozoic time. Large volumes of clastic and carbonate sediments have been preserved. � Since the late 1940's, industry has found more than 960 fields and the basin has undergone multiple exploration cycles. The Williston Basin covers more than 143,000 sq. miles and Fort Berthold reservation covers about one percent of that total (1530 sq. miles). Most of the reservation is unexplored. � Gas was discovered at Cedar Creek Anticline in 1916; oil was discovered on Nesson Anticline in 1951. Nesson is located about 50 miles northwest of the reservation boundary. Antelope Field, a southeast plunging anticline, was discovered in 1953 and extends onto the reservation. Plaza and Wabek Fields, part of the Mississippian shoreline trend, were discovered in the 1980's. Condensate and gas were discovered in the Winnipeg and Deadwood Formations at Antelope Field in 1992.
Fort Berthold Reservation GENERAL PRODUCTION INFORMATION
U.S.G.S. Geologic Province - Williston Basin (031) Tectonic Province - Williston Basin
Fields within reservation boundaries 1996 cumulative production. Parentheses indicates discovery year
(1953) Antelope - 41 MMBO, 19.2 Mmcf, 30 oil wells, 2 gas wells (1989) Plaza - 2.9 MMBO, 3.9 Mmcf, 20 wells total (1982) Wabek - 5.4 MMBO, 3.9 Mmcf, 18 wells total
Nearby fields
(1955) Blue Buttes - 46 MMBO, 29.2 Mmcf, 44 wells total (1957) Bear Den - 1.5 MMBO, 1.7 Mmcf, 2 oil wells, 1 gas well (1952) Croff - 1.8 MMBO, 4.1 Mmcf, 3 wells total (1981) Spotted Horn - 108 MBO, 36,234 Mcf, (Abn'd) (1982) Squaw Creek - 195 MBO, 328,546 Mcf, 1 well total (1982) Mandaree - 160 MBO, 147,325 Mcf, 2 wells total (1990) Lucky Mound - 1.4 MMBO, 890, 670 MCF, 18 wells total
Figure FB-1.1. Producing horizon legend. Many of the potential reservoir intervals can be correlated into Wyoming and Montana. However, the Williston Basin is unique among other Rocky Mountain basins for its thick package of Paleozoic age carbonate sediments. While the other basins are known for their numerous clastic potential reservoir intervals, the Williston Basin is known as a carbonate province (modified after Seventh International Williston Basin Symposium Guidebook, 1995).
Fort Berthold Reservation North Dakota Introduction
Producing Horizon Legend (after Geomap Executive Reference Map, 1983)
= Source Rock
PRODUCING HORIZON LEGEND
Judith River
Niobrara
Greenhorn
Dakota Group
Nesson
Opeche
Minnelusa
Amsden
Heath
Kibbey
Lodgepole
Bakken Three Forks Nisku Duperow Souris River
Winnipegosis
Red River
Winnipeg
Mowry
Muddy
Fall River
Sundance
Canyon Springs
Gypsum
Chugwater
Spearfish
Goose Egg
Minnelusa
Madison
Lance Fox Hills Mesaverde Cody Shannon
Frontier
Mowry Muddy Bear River
Cloverly
Ankareh Thaynes Woodside
Dinwoody
Park City
Weber
Amsden Darwin
Madison
Lodgepole
Gall
Flath
Blackleaf Bow Island
Cat Creek Moulton
Cut Bank
Amsden
Heath
Kibbey
Sun River
Lodgepole
Three Forks
Nisku Duperow
Souris River
Red River
Flathead
WESTERN WYOMING
SOUTHERN MONTANA
WESTERN NORTHERN MONTANA
WILLISTON BASIN
POWDER RIVER BASIN
SE
RIE
S
SY
ST
EM
ER
A
TE
RT
IAR
Y
CE
NO
ZO
IC
CR
ETA
CE
OU
S
UP
PE
RLO
WE
R
JUR
AS
SIC
TR
IAS
SIC
PE
RM
IAN
PE
NN
SY
LVA
NIA
NM
ISS
ISS
IPP
IAN
DE
VO
NIA
N
SIL
UR
IAN
OR
DO
VIC
IAN
CA
MB
RIA
N
M E
S O
Z O
I C
P
A
L E
O
Z
O
I
C
B
I O
G
E
N
I
C
Sundance
Stump-Preuss
Twin Creek
Ellis Group
Reirdon Sawtooth
Wasatch Wasatch
Lance
Parkman Sussex Shannon Niobrara
Hell Creek Judith River
Eagle
Niobrara Greenhorn
Winnipeg
Tensleep
Swift Swift
Fort Union Fort Union
Teckla
Teapot
Telegraph Creek
S
S
S
S
S
S
Fort UnionFort Union
�Morrison
Ellis Group
Reirdon Piper
Morrison Gannet
Morrison Morrison
Nugget Chugwater
Phosphoria
Tyler Tyler
Big Snowy Group
Otter
Madison Group Charles Mission Canyon
Englewood
Mission Canyon
Big Snowy Group
Otter
Madison Group
Charles Mission Canyon
Dawson Bay
Jefferson
Interlake Interlake
Stonewall
Stony Mountain Big Horn Big Horn
Deadwood Deadwood Gros
Emerson
White River Green River Wind River
Fox Hills
Eagle
Mesaverde
Frontier
Niobrara Frontier
Clagget
Dakota
Lakota
Dakota
Kootenai
Sunburst
Spearfish
Jefferson
Darby
Minnekahta
Page 2 of 18
Alberta Shel f CANADA 97 98 114 113 100 99112 111 110 109 108 107 102 101 106 105 104 103 BF Sw
eetgrass
Hogeland Bearpaw Basin
Uplift
Dom
eBow
doin
UNITED STATES
Fault
A Poplar
BK Popla
r Faul
t
Hinsda
le
OVERTHRUST
FP Dome 48 Ness
on
Ant
iclin
e A'Little A
rch
Rocky Mtns Judith Mtns Blood
Big Little Snowy
Syncline
Creek
MONTANA Belt Mtns Cat Creek Fault
Weldo
n-Broc
kton F
ault
BR NORTH DAKOTA
WILLISTONBELT
Mtns Sumatra
Anticline C
edar CreekWheatland Willow
Fault Creek
Syncline
Porcupine BASIN Syncline Dome
Crazy BullMountains Mountains
Miles CityArch Basin
Lake SRBasin Fault Fault Nye-Bowler
Basin Beartooth
Pryor POWDER Mtns Mtns RIVER
Bighorn
BASIN BIGHORN SOU
TH DAKOTA AbsarokaM
tns BASIN Black
Owl
Mtns
Hills Uplift
Creek Mtns
IDAHO
Wind
WIND RIVER
Arch C
asper
WYOMING Fault
River
BASIN Casper Mt
n M
tns Sweetwater
Laramie GREEN Uplift Mtns Ha
rtville
Chadron
Upl
ift
RIVER HANNARED
Arch
BASIN BASINDESERT NEBRASKA Rock BASIN ALLIANCE
UTAH
Bow
Medicine
LARAMIE Springs Uplift BASIN BASIN
Sierra Uinta Mtns WASHAKE Madre
BASIN Mtns
Mtns COLORADO
EXPLANATION
Precambrian Basement Uplifts Anticline
Syncline Other Uplifts or Basins
Faults SR - Standing Rock BK - Fort Belknap Cenezoic Volcanic Fields BR - Fort Berthold BF - Blackfeet
A A' X-section FP - Fort Peck Reservations
Figure FB-2.1. Present day structural features of the northern Rocky Mountain region. Includes major fault zones, uplifts, basins, and reservation areas (modified after Peterson, 1987).
REGIONAL GEOLOGY� The Fort Berthold Reservation is situated near the deepest part of theWilliston Basin (see Fig. FB-2.1 A-A' and associated cross-sections). Duringthe Paleozoic and early part of the Mesozoic, the basin was a stable, cratonicdepocenter which received over 15,000' of sediments. Fort Bertholdreservation is located within the depocenter, near a major structural featurecalled the Nesson Anticline, which produces a significant percentage ofhydrocarbons within the basin. � Predominantly a carbonate depocenter in the Paleozoic, the basin is alsointerbedded with clastics and evaporites. The clastic intervals are composed of marine, organic rich shales which are the principal source rocks for thebasin. In addition, some of the clastic intervals also include nearshore marineor fluvial sandstone deposits. The carbonate and evaporite units are mainlytidal flat, bioherm/reef or sabhka deposits. Cyclic sedimentation of marineshales, limestones/dolomite, and anhydrites or salt are indicative of the Paleozoic section within the Williston Basin. � Potential reservoir intervals can be formed in the limestone or dolomite viaprimary or secondary porosity mechanisms. Porosity may be intergranular,vuggy, intercrystalline or fractured or combinations of all types depending on structural position and depositional environment.
Geologic History - Cambrian and older rocks � Precambrian age supracrustal sedimentary rocks are present in western Montana and extend into Glacier National Park (see Fig. FB-2.1). These rocks are estimated to be from 900 to 1400 million years old. No Precambrian rocks are exposed on the Fort Berthold Reservation. � During Cambrian time, a major seaway existed in western Montana and eastern Idaho (see Figs. FB-2.2 & 2.4). This seaway gradually transgressed from west to east across eastern Montana and the Dakotas. The dominant source of coarse-grained clastics was to the east (from the Sioux Arch) and gradually changed into shales and limestones to the west. Thickness of the Cambrian rocks varies from over 2000 feet in the Montana Disturbed Belt to less than 100 feet along the eastern edge of the Williston Basin. Cambrian sediments buried under the Fort Berthold Reservation are about 300-600 feet thick and composed predominantly of coarse-grained sandstone.
Geologic History - Ordovician to Triassic � A major depocenter evolved along the eastern edge of the Williston Basin which was a stable, marine shelf area throughout much of the Paleozoic (see Fig. FB-2.3). Ordovician and Silurian rocks were deposited mostly in a shallow tidal flat environment which resulted in alternating cycles of limestone/dolomite, marine shales, and evaporites. By the end of Silurian time, a regional lowstand resulted in a basin-wide unconformity separating Silurian and Devonian rocks. This unconformity influenced the development of vuggy, karsted, carbonate sediments adjacent to this horizon. Present-day thickness of Ordovician and Silurian rocks in the reservation area are 1200 feet and 1000 feet , respectively. � Deposition during Devonian time proceeded much as it had in the Silurian except for the development of highly organic-rich shales within the carbonate intervals. Within the reservation boundaries, Devonian sediments are about 1700 feet thick and include the regional Prairie Salt (500-700'), and the Bakken Shale (70-100'). The Prairie Salt forms a regional seal for the older intervals and has been mobilized/dissolved out of this section near the western edge of the basin (105 degrees longitude). The Bakken Shale is thought to be one of the primary source intervals for Mississippian and younger production.
West EastLongitude Values (in degrees) Fort Berthold Reservation A'A
114 113 112 111 110 109 108 107 106 105 104 103 102 101 1000
Cambrian Rocks PreCambrian RocksCambrian Rocks Sands and Shales
1000 Sands and ShalesSweetgrass Arch
2000 Bearpaw Uplift
Thic
knes
s of
Sed
imen
t (fe
et) PreCambrian Rocks
Poplar Dome Williston Basin3000
Rocky Mountain Trench Little Rocky Mountains
4000Overthrust Belt
5000
6000
7000
8000
Figure FB-2.2. Generalized time-slice cross-section along A-A'. Line of section along 48degrees latitude with selected points every 1 degree longitude. Datum is base Ordovician.
WEST EAST Fort Berthold Longitude Values (in Degrees) Reservation
A A'114 113 112 111 110 109 108 107 106 105 104 103 102 101 100
0 Triassic Rocks
Pennsylvanian RocksBakken Shale Permian Rocks
1000 Williston Basin Devonian Rocks
2000 Mississippian Rocks
Thi
ckne
ss o
f Sed
imen
t (in
ft)
Bearpaw Uplift PreCambrian Rocks 3000 Cambrian Rocks Bakken Shale
Sweetgrass Arch Sands and Shales
Rocky Mountain Trench 4000 Ordovician Rocks
Overthrust Belt Little Rocky Mountains Prairie Salt
5000 Poplar Dome
Silurian Rocks
6000 Cambrian Rocks
Sands and Shales 7000
Ordovician Rocks 8000
Figure FB-2.3. Generalized time-slice cross-section A-A'. Triassic through Ordovician. Line of section along 48 degrees latitude with selected points every 1 degree of longitude. Datum is the base of Jurassic, Permian missing (from C.W. O'Melveny, July 1996).
110 100 105 0 100 40
A 20 0
100 60 A' 0
80 Antelope 120
120 Fort Berthold Taylor
100 Reservation
North Dakota 120 80
150 60 40
Montana 20 100
60 40 100
80Cambrian and older rocks exposed
Wyoming South Dakotasandstone facies
40 0 20shale, sandstone and 0 minor limestone facies
green shale facies
40 contour interval, in multiples of 10 feet
Figure FB-2.4. Map showing thickness of Cambrian-aged Deadwood and equivalent rocks along with facies information, location of analog fields from Cambrian sediments, location of reservation, and location of regional cross-section A-A' (modified after Peterson, 1987).
Fort Berthold Reservation North Dakota
GEOLOGY OVERVIEW Geologic History
Page 3 of 18
Cretaceous Epeiric Seaway
Greenland Alaska
Canada
Cretaceous Epeiric Seaway
United States
0 Cretaceous Epeiric Seaway
Mexico Cuba
Figure FB-3.3. Paleogeographic map of North America during Late Cretaceous time, showing the extent of the Cretaceous seaway (after Rice and Shurr, 1980).
GEOLOGIC HISTORY (continued)
Geologic History - Ordovician to Triassic By Mississppian time, the western portion of the Williston Basin was continuously receiving carbonates and evaporites in a shallow, marine shelf environment (see Figure BF-3.1). Most of the producing reservoirs in the basin are from these cyclic marine shales, limestone/dolomite porosity horizons, and evaporitic carbonate sequences. Eventually, the Charles Salt horizon would cover the entire basin and part of eastern and central Montana. By late Mississippian time, deposition of shales and mudstones were mainly confined to the central Williston area and the Big Snowy trough in central Montana. Total thickness of Mississippian rocks within the reservation boundaries is about 2400-2800 feet. � Another major lowstand at the end of the Mississippian time led to widespread erosion and karstification of the underlying carbonate intervals. Pennsylvanian sediments are confined to the center of the Williston basin and central Montana. Pennsylvanian rocks are about 400 feet thick. � Permian deposits are confined to the central Williston basin area and are predominantly sandstone/shale and evaporite sequences. As the Williston basin became filled to base-level, only shallow marine/terrestrial sediments were deposited. This also resulted in numerous unconformities in this horizon. A major unconformity at the end of Permian time has
removed any evidence of these rocks west of longitude 104 degrees. Permian rocks within the reservation are about 500 feet thick. Triassic-aged sediments are also present and of continental origin. Estimated thickness of Triassic rocks across the reservation are about 400-500 feet thick.
Geologic History - Jurassic to Cretaceous A tectonic structural reorganization of the North American continent occurred during Jurassic-Cretaceous time. This resulted in a major change in depocenter position of the Williston basin, shifting from the east to the western side (Figure 4.3). The inital pulses of the Sevier and later Laramide thrusting resulted in dominantly clastic deposition in the Cretaceous Seaway during this time (Figure 4.4). � Thickness of Jurassic rocks across the reservation area are estimated to be about 1200 to 1400 feet thick and are comprised of a complex mixture of nearshore marine, fluvial, and evaporitic deposits. Early Cretaceous-aged continental/fluvial sediments are about 300-400 feet thick. Provenance for these sediments are thought to have been from the southeast in what is present day South Dakota.� The Mowry/Skull Creek Formation is about 400-500 feet thick within thereservation area and was deposited in a transgressive marine sequence which extended from western Montana eastward into the Dakotas; from Texas northward into Canada. Numerous clastic sandstone deposits are present within this sequence and are the result of variations in sea level and clastic influx into the seaway. � During Upper Cretaceous time thrusting and crustal loading from the west had subsided enough to allow the re-establishment of carbonate deposition within the seaway. Extensive chalk deposits of the Greenhorn/Niobrara Formations were deposited as well as thousands of feet of marine carbonate/clastic shale. Upper Cretaceous rocks in the area are more than 2500 feet thick. As the Laramide Orogeny and associated thrusting began to exert influence, nearshore marine and fluvial sandstones began depositing along the shorelines of the seaway.
Geologic History - Tertiary and Quaternary As the orogenic uplifts of the Laramide Orogeny occurred during Late Cretaceous to Tertiary time, older Cretaceous rocks were uplifted and eroded. Only the central portion of the Williston preserved the swamp/peat deposits during the Paleocene and Eocene. Coal deposits of the Fort Union and equivalent rocks are the result. These sediments can be up to 1750 feet thick across the reservation. Alpine glaciers existed in Montana during Quaternary time and extensive glacial lakes and ice sheets covered the reservation area.
Fort Berthold WEST Longitude Values (in Degrees) EAST Reservation A A'
114 113 112 111 110 109 108 107 106 105 104 103 102 101 100 0
1000 Volcanics
Upper Cretaceous 2000
(Niobrara and Eagle Formations)
Thi
ckne
ss o
f Sed
imen
t (in
ft) 3000
4000 Jurassic Rocks
Lower Cretaceous 5000 (Mowry)
Poplar DomeMississippian and Older
6000 RocksLower Cretaceous (Kootenai) Bearpaw Uplift
7000 Sweetgrass Arch Williston Basin
Rocky Mountain Trench8000
Overthrust Belt
Figure FB-3.2. Generalized cross-section A-A' - Cretaceous and Older Rocks. Line of cross-section along 48 degrees latitude with selected points every 1 degree of longitude. Datum located at the top of the Cretaceous.
110 100 105
200
A 600 A'
400 600 Ft. Berthold
0 600 Reservation 600 Dickinson Field 0 1000 400
800 600 400 North Dakota
200
0
Montana
Wyoming
Cambrian and older ricks exposed
South Dakota sandstone and sandy shale facies
green, gray, and red shale with minor limestone
200 200 foot contour interval
Figure FB-3.4 Isopach map showing thickness and facies distribution of late Mississippian and Pennsylvanian sediments of the Tyler and Big Snowy Group suite of rocks. Location of Fort Berthold Reservation, any analog fields, and older basement rocks also shown (modified after Peterson, 1987).
Fort Berthold Reservation North Dakota GEOLOGY OVERVIEW
Geologic History
Page 4 of 18
A
Saskatchewan Manitoba
Poplar Dome
B
Cedar Creek Anticline Petroleum Province North Dakota
South Dakota
Montana
0 Wyoming
Nesson Anticline Petroleum Province
Madison Group Subcrop Petroleum Province
Region of Prairie Formation salt preservation
3000
5000
70
00
200km
Depth of base Madison (ft)
Figure FB-4.1 - Location of the Williston Basin with major petroleum provinces and line of section for burial history diagrams indicated. Structural contours are drawn on the base of the Madison Group (after J. Burrus, K. Osadetz, S. Wolf, et al, 1995).
Petroleum Systems
� Accumulations of hydrocarbons owe their genesis to several critical factors: generation and migration from source intervals, structural/stratigraphic trapping mechanisms, porous reservior rocks, and the appropriate timing of formation/generation of these factors. At least four petroleum systems are present within the Williston Basin with numerous underexplored potential hydrocarbon exploration targets. This discussion focuses on the source intervals.
Source rocks: Generation and Expulsion At least four source intervals have contributed to the hydrocarbon generation and
accumulation patterns within the Williston Basin and all are present in the reservation area.
� Ordovician Winnipeg shale - A very organic rich shale which exceeds richness values of the Bakken shale in some cases. This interval first entered the oil window in latest Cretaceous/Paleocene time. Peak generation and expulsion occurred between 55-38 mya and some generation continues today. Oils typed to this source are found in the Cedar Creek anticline, eastern Montana, and western North Dakota. However, structures which formed in latest Eocene or after (such as the Nesson Anticline) could not trap the oil migrating from this source. This suggests that much of Winnipeg- sourced oil migrated to the northeastern flank of the Williston Basin where undiscovered oil resource may be present in Ordovician and Silurian strata. This source interval is aerally restricted to the southern and central portions of the basin.
� Bakken Shale - Known as a world-class source interval, the Bakken has an average of 11.33 wt. % organic carbon. Oil generation was probably initiated about 75 mya with initial expulsion occurring about 70mya (late Cretaceous). Calculations based on pyrolysis data suggest that between 92.3 - 110 billion barrels of oil have been generated from the Bakken. Except for a few fields utilizing the Bakken as the reservoir, significant volumes of Bakken sourced oil have not been discovered to date. Some researchers suggest that most of the expelled Bakken oil is probably lost into the drainage system, where it remains dispersed, at very low saturations (see Figures 2.2 and 2.3 below). Most of the larger structures in the Williston Basin contain mixtures of Lodgepole (Madison) and Bakken oils with the latter at low relative concentrations.
� Lodgepole source interval - This zone contains predominantly carbonate source horizons with relatively low initial yields; 8 kg HC/t rock. However, large volumes of oil have been discovered typed to this source interval, especially within the Nesson Anticline Petroleum Province. This horizon seems to be geographically restricted to the central and southern portions of the Williston Basin. It appears that migration and trapping efficiencies were much higher in this horizon when compared to the Bakken. This may be due to advantageous timing of structure development relative to expulsion/migration.
� Winnipegosis source interval - The rich, basinal carbonate horizons within this unit (47 kg HC/t rock) are restricted to a starved, Devonian which begins along the northern end of the Nesson anticline and continues north into Canada. This interval charges many of the Waulsortian mounds found in some of the Mississippian-aged sequences.
A Distance (km) B50 100 150 200 250 300
0
1
2
Potential in Ordovician source &
Bakken
0Ma
Northern limit of Ordovician source
Bakken thickness exaggerated x 2.5
Madison
Duperow
Interlake Winnipeg source
Bighorn interval
TR=.10
TR=.20
TR=.65
TR=.90
HC saturation
< 2%
2 - 5%
5 - 10%
10 - 80%
> 80%
Prairie salt horizon
Dep
th (
km)
3
4
Figure FB-4.2 - Burial history model with patterns of transformation ratio (TR) at the present and distribution of oil saturations, calculated using a finite model, two-dimensional computer model that simulates oil generation, expulsion, and migration. Generation kinetics determined by experimental data from Williston Basin source rocks. Thermal history model constrained by both present temperature and source rock maturity data. Saturations compared to known patterns of hydrocarbon accumulation within the basin. Saturations between 2-5% represent dispersed oil; saturations above 10% represent oil accumulation or depleted source rocks. Arrows show patterns of active oil migration (after J. Burrus, K. Osadetz, S. Wolf, et al., 1995)
A Distance (km) B 50 100 150 200 250 300
Potential in Winnipegosis &
Lodgepole
0Ma
TR=.10
TR=.20
TR=.90
0
1
Dep
th (
km)
2
3
4
Lodgepole
Winnepegosis thickness exaggerated x 2.5 between 0-250km
HC saturation
TR=.65
< 2%
2 - 5%
5 - 10%
10 - 80%
> 80%
Prairie salt horizon
Figure FB-4.3- Burial history model with patterns of transformation ratio (TR) at the present and distribution of oil saturations, calculated using a finite model, two-dimensional computer model that simulates oil generation, expulsion, and migration. Generation kinetics determined by experimental data from Williston Basin source rocks. Thermal history model constrained by both present temperature and source rock maturity data. Saturations compared to known patterns of hydrocarbon accumulation within the basin. Saturations between 2-5% represent dispersed oil; saturations above 10% represent oil accumulation or depleted source rocks.Arrows show patterns of active oil migration (after J. Burrus, K. Osadetz, S. Wolf, et al., 1995).
Fort Berthold Reservation North Dakota Petroleum Systems
Page 5 of 18
Schematic Diagram of Play Types - Fort Berthold Reservation WEST EAST
Upper Cretaceous
Play Types - Explanation
1. Madison Structure Play Niobrara
10 10 2. Madison Shoreline/Truncation Play
Jurassic 3. Mississippian Lodgepole Waulsortian Mound Play
Triassic 4. Ordovician Red River Play
Permian 5. Devonian Nisku/Duperow Play
Pennsylvanian 7 6. Silurian Interlake Play1
2 2 7 7. Pennsylvanian Tyler-Heath Play
9 8. Pre-Red River GasMississippian 3 Winnipeg/Deadwood Clastics 35 Bakken Shale MississippianDevonian 9. Fractured Bakken Play6 9
Red River 4 10. Shallow Microbial Gas PlayInterlake8 Winnipeg
Deadwood
No scale implied - drawing is approximate width of Reservation Dolomite Precambrian Fluvial/Clastic dominated shorelines
Limestone Sandstone Clastic/calcareous shale
Organic-rich Limestone shorelines shale or Waulsortian Mounds
Oil Gas
Figure FB-5.1. Schematic diagrams of play types at Blackfeet Reservation
Play Summary
The diagram and summary charts are coded to the play type number and provide a quick reference to the discovered and undiscovered resource for the reservation area. Also listed are USGS (1996) risk estimates and designations for each of the play types. A qualitative brief review of the summary aspects of each play are also shown.
Reservation: Geologic Province: Province Area: Reservation Area:
Fort Berthold Central Wiliston Basin Williston Basin (143,000 sq. miles) 1530 sq. miles (980,000 acres)
Total Production ( by province-1996) Oil: Gas: NGL:
Williston Basin 1496 MMBO 1735 BCFG 192 MBNGL
Undiscovered resources and numbers of fields arefor Province-wide plays. No attempt has been madeto estimate number of undiscovered fields within theFort Berthold Reservation
Play Type USGSDesignation
Description of Play Oil or Gas Known Accumulations Undiscovered Resource (MMBOE) Play Probability (chance of success) Drilling depths Favorable factors Unfavorable factors
Madison, structure
1
3101a folded structures, primary and secondary porosity in carbonates
Both 878 MMBO 916.5 BCFG 77.9 MMBNGL (numbers include 1, 2,& 3)
Median: 600 MMBO(30 fields @ 20MMBO)
Field Size (> 1 MMBOE) 2 MMBO (min), 20 MMBO (median), 5.3 MMBO(mean)
No. of undiscovered fields (> 1 MMBOE) 9 (min) 30 (median) 60 (max) 31.9 (mean) numbers include plays 1, 2, & 3
1 high
3,000 - 12,000 ft 1) confirmed play; excellent production within reservation
2) thermally mature source rocks 3) source rocks and reservoir present 4) seismic delineation is useful
1) lack of well control 2) rough topography 3) porosity and facies may be
highly variable
Madison shoreline/ truncation play
2
3101b Cyclic evaporite/ carbonate sequence, structure/stratigraphic updip pinchout, multiple shoreline cycles
Both 878 MMBO 916.5 BCFG 77.9 MMBNGL (numbers include 1, 2,& 3)
Median of 600 MMBO (30 fields @ 20MMBO)
Field Size ( >1 MMBOE) 2 MMBO(min) 20 MMBO(median) 5.3 MMBO(mean)
No of undiscovered fields (> 1 MMBOE) 9 (min) 30 (median) 60 (max) 31.9 (mean) numbers include plays 1, 2, & 3
1 high
3,000 - 12,000 ft 1) confirmed play; excellent production within reservation
2) thermally mature source rocks 3) source rocks and reservoir present 4) trend extends into reservation 5) mostly shallow drilling depths
1) lack of well control 2) rough topography 3) porosity and facies may be
highly variable 4) seismic may not be able to
delineate shoreline trends
Miss. Lodgepole/ aulsortian Mound play W
3
3101c Mound buildups; 'reefs', small but prolific structures; excellent porosity and permeability
Both 878 MMBO 916.5 BCFG 77.9 MMBNGL (numbers include 1, 2,& 3)
Median of 600 MMBO (30 fields @ 20MMBO)
Field Size ( >1 MMBOE) 2 MMBO(min) 20 MMBO(median) 5.3 MMBO(mean)
No of undiscovered fields (> 1 MMBOE) 9 (min) 30 (median) 60 (max) 31.9 (mean) numbers include plays 1, 2, & 3
1 high
3,000 - 12,000 ft 1) confirmed play; trend probably extends to reservation
2) thermally mature source rocks 3) source rocks and reservoir present 4) seismic may be very useful
1) lack of well control 2) rough topography 3) small areal extent, may
be difficult to explore for
Ordovician Red River Play
4
3102 Cyclic evaporite/ carbonate sequence, structure/stratigraphic updip pinchouts; multiple shoreline cycles
Both 188.3 MMBO 555.7 BCFG 70.5 MMBNGL
Median of 250 MMBO (25 fields @ 10 MMBO)
Field Size ( >1 MMBOE) 2 MMBO/10 BCFG(min) 10 MMBO/35 BCFG(median) 2.1 MMBO/11.7 BCFG(mean)
No of undiscovered fields (> 1 MMBOE) 5 (min) 25 (median) 50 (max) 26 (mean)
1 high
7,000 - 12,000 ft 1) confirmed play; production within reservation
2) thermally mature source rocks 3) source rocks and reservoir present 4) seismic useful in locating
structures
1) lack of well control 2) rough topography 3) possible small exploration
targets
able FB-5.1. Play summary chart T
Fort Berthold Reservation North Dakota Play Types
Page 6 of 18
Reservation: Fort Berthold Total Production ( by province-1996) Williston Basin Undiscovered resources and numbers of fields are Geologic Province: Central Williston Basin Oil: 1496 MMBO for Province-wide plays. No attempt has been made Province Area: Williston Basin (143,000 sq. miles) Gas: 1735 BCFG to estimate number of undiscovered fields within the Reservation Area: 1530 sq. miles (980,000 acres) NGL: 192 MBNGL Fort Berthold Reservation
USGS Undiscovered Resource (MMBOE) Play Probability Play Type Description of Play Oil or Gas Known Accumulations Drilling depths Favorable factors Unfavorable factors Designation Field Size (> 1 MMBOE) min, median, mean (chance of success)
Median 250 MMBO (25 fields @ 10 MMBO) Nisku and Duperow 3103 Cyclic evaporite/carbonate Both 160.5 MMBO 1 8,000 - 12,500 ft 1) confirmed play; 1) lack of well control sequences. Structural and 159.2 BCFG Field Size (> 1MMBOE) high production within reservation 2) rough topography
2 MMBO/10 BCFG 10 MMBO/60 BCFG 2.1 MMBO/13.1 BCFG stratigraphic pinchouts. Excellent 12.7 MMBNGL 2) thermally mature source rocks porosity and permeability No.of undiscovered fields (> 1 MMBOE) 3) source rocks and reservoir present 5 9 (min) 25 (median) 60 (max) 26.9 (mean) 4) seismic delineation is useful
Silurian Winnipegosis Median 225 MMBO (15 fields @ 15 MMBO)3105 Cyclic evaporite/ carbonate Both 55.5 MMBO 1 8,000 - 12,500 ft 1) confirmed play; 1) lack of well control and Interlake Field Size (> 1MMBOE)sequence, erosional surfaces. 180 MMCFG mod.- high production within reservation 2) rough topography
3 MMBO/15 MCFG(min) 15 MMBO/90 MMCFG(median)Primary and secondary porosity. 24.8 MMBNGL 2) thermally mature source rocks 3.3 MMBO/19.7 MMCF(mean) Structural and unconformity related 3) source rocks and reservoir present 6 trapping mechanisms No. of undiscovered fields (> 1 MMBOE) 4) seismic useful in prospect 5 (min) 15 (median) 25 (max) 15 (mean) delineation
Post Madison 3106 Fluvial and nearshore sandstones Both 133.5 MMBO Median 16 MMBO (8 fields @ 2 MMBO) 1 5,500 - 9,000 ft 1) Thermally mature source rocks 1) No production within Penn. Tyler/Heath with structural closures. Traps may 28.8 BCFG mod.-high 2) source rocks and reservoir present reservation
Field Size (> 1MMBOE) also occur as discontinuous sandstone 3) shallow drilling depths 2) rough topography 2 MMBO 10 MMBO 2.1 MMBO lenses. 3) lack of well control 7 4) depositional area within No of undiscovered fields (> 1 MMBOE)
reservation may be marine 4 (min) 8 (median) 15 (max) 8.6 (mean) instead of shoreline
Ordovician Pre-Red River 3107 Clastic sequences, fluvial and NGL and low no information Median 50 BCFG (5 fields @ 10 BCFG) 1 10,000 - 16,000 ft 1) confirmed play; 1) lack of well control Play nearshore blanket sandstones. BTU gas available moderate production within reservation 2) rough topography
Field Size (> 1MMBOE) Large, faulted structures 2) thermally mature source rocks 3) low BTU, contains 10 BCFG 25 BCFG 13.1 BCFG
3) source rocks and reservoir present nitrogen 8 4) seismic useful in locating No. of undiscovered fields (> 1 MMBOE) 1 (min) 5 (median) 20 (max) 7.3 (mean) structures
5) high volume reserves
Fractured Bakken 3111 Organic rich shale, marine siltstone; Both No information available not estimated 1 7,500 - 11,100 ft 1) confirmed play; 1) lack of well control fractured; thermally mature oil shale Oil shows from Sanish sandstones 70.3 MMBO/ sq. mile generated hydrocarbons 0.2 (20%) production within reservation 2) rough topography
56.24 MMCFG/ sq. mile generated hydrocarbons 2) thermally mature source rocks 3) Probable narrow bands of Area of play = 8185 sq. miles 3) source rocks and reservoir present potential fractured reservoir 9 7806 sq. miles untested 4) seismic delineation is useful zones
Niobrara Microbial 3113 Niobrara limestone and other Microbial gas Only production to date is from not estimated 1 500 - 4500 ft 1) large volume play 1) lack of well control Gas Play shallow reservoirs, self-sourced; Cedar Creek Anticline and 180 MMCFG/160 acres (median) 0.5 (50%) 2) shallow drilling depths 2) rough topography
porosity decreasing with increasing Bowdoin dome. These fields are 256 MMCFG/160 acres (mean) 3) accumulations in structural 3) reservoir continuity isdepth. Large volume accumulations from shallow Eagle Formation Area of play = 55,000 sq. miles traps, seismic may be useful problematic 10 possible sandstones, not Niobrara. 29,958 sq. miles untested (mean) in delineation of traps 4) areal extent may be small
Table BR-6.1. Play type summaries. Conventional play type
Unconventional/Hypothetical play type
Fort Berthold Reservation North Dakota Summary of Plays (continued)
Page 7 of 18
A A.P.C. A.P.C. A' #3 M Aura #1 Aura
Se Sw Sec. 19 Se Se Sec. 19 KB 2346' KB 2388'
GR
A.P.C. A.P.C. #2 Selliseth Texaco
#20 Sivertson Se Sw Sec. 20 #4 Gov't-Dorough
Se Se Sec. 20 KB 2495' Se Sw Sec. 21
KB 2493' KB 2690'
Last Charles Salt
Mississippian
Madison
Gamma Ray MarkerFormation
Top Blue Buttes Pay
90
00
91
00
91
00
93
00
91
00
92
00
92
00
94
00
92
00
93
00
93
00
95
00
93
00
94
00
94
00
96
00
94
00
95
00
97
00
-6500
-6600
-6700
-6800
-6900
-7000
90
00
91
00
92
00
93
00
LL GR
LL
Blue Buttes Field Structural Cross-Section
Figure FB-7.1. Blue Buttes Field structural cross-section (after Connelly, North Dakota Geological Society, 1962).
Blue Buttes Field Parameters
Formation: � Mississippian Madison
Lithology: Interbedded limestones and dolomites.
Average depth: 9200 feet (in reservation area)
Porosity: � averages 7.7%
Permeability: � 0.1-8 md, average is 3 md.
Oil/gas column: � oil 280 feet
Average net pay: � variable
Other Formations with shows: Kibbey sandstone, Kibbey limestone and Charles Formation
161
7 12
1318
19 24
2530
3136 36
161
7 12
1318
1924 24
R 96 W R 95 W
T 151 N
T 150 N
Blue Buttes Field
Top Lower Charles Salt Structure Map
CI = 20 feet
Note: Only Madison penetrations are shown
R 95 WR 96 W
A A'
-670
0
-670
0
-680
0
-660
0
-660
0
Figure FB-7.2. Structure contour map of Blue Buttes Field showing location of cross-section A-A'. Structure on top of Lower Charles Salt.
PLAY TYPE 1
Folded Structure - Mississippian Carbonate Play
General Characteristics - The Mississippian Madison play is primarily a structural play combined with superimposed facies/porosity changes and pinch-outs. This play is the dominant hydrocarbon producer in the Williston basin. The Madison is subdivided into several producing horizons (see cross-sections below), based on porosity zones. These zones are overlain by evaporite or shale seals. The Charles Salt horizon is a regional evaporite seal which overlies most of the Madison Formation. � Reservoir rocks are generally dolomitized carbonate rocks with either algal, oolitic, crinoidal, or micritic components. Source rocks are thought to be either of Bakken origin or cyclic marine shales within the evaporite-carbonate cycle. Onset of oil generation and migration is modeled to begin in the Late Cretaceous.
Analog Fields (*) denotes fields within Reservation
Antelope* - � 39 MMBO� 18.9 Mmcf(includes Bakken, Duperow, and Interlake)
Blue Buttes -� 45 MMBO� 28.3 Mmcf (includes Duperow, Interlake, and Red River)
Bear Den -� 1.4 MMBO� 1.5 Mmcf (Madison, Duperow)
Croff -� 1.7 MMBO� 4.0 Mmcf (Madison, Duperow)
Antelope Field Parameters
Formation:� Mississippian Madison
Lithology:� Limestone, brown, dolomitic, fossil fragments, occasional chalky horizons.
Average depth: � 9100 feet
(in reservation area).�
Porosity: � 4.7% gross, intergranular, vuggy
Permeability: � info. not available
Oil/gas column: � highly variable
Average net pay: � variable
Other shows: � Sanish, Duperow, Interlake.
Other information: contains 4.7% H2S
Kibbey Kibbey
Charles Charles
Madison Madison Lodgepole
Bakken
Three Forks - Nisku
Duperow
Souris River
Dawson Bay-Prairie Evaporite
Winnipegosis- Elm Point - Ashern
Silurian
Stony Mountain
Red River
Winnipeg
Cambrian ?
PreCambrian
-5603 -5589 -5557 -5494 -5619 -5876
-6161
-6809
-8555
-5908
-6536
-8226
-5794
-6409
-8081
-8367
-8770 -8997
-9273
-9631
-10779 -10993
-11632
-12274
-13012
-5838
-6466
-5882
-6492
-5889
-5000
-6575
TD -6866 TD -6908
TD -7212
unconformity horizons
A.P.C. #1 Swenson Heirs A.P.C. #1 AB Fleming Estate A.P.C. #1 T Larson Tract 1 A.P.C. #1 Antelope Unit 'A' A.P.C. Gulf #1 J Strand A.P.C. Carter #1 Reed-Norby UnitC Se Ne 11-152N-95W C Nw Nw 12-152N-95W C Se Sw 1-152N-95W Ne Se 1-152N-95W S/2 Nw/4 6-152N-94W Lot 2 6-152N-94W
2242 KB 2210 KB 2136 KB 2117 KB 2129 KB 2198 KB
-5000'
TD -8255
TD -8570
R 94 W
Fort Berthold Reservation
T 152 N
B'
A
Structural Cross Section
Antelope Field McKenzie Co., North Dakota
Index Map
B B'
Figure FB-7.3. Antelope field cross-section (after North Dakota Geological Society, 1962).
Fort Berthold Reservation North Dakota
CONVENTIONAL PLAY TYPE 1 Folded Structure - Mississippian Carbonate Play
Page 8 of 18
Analog Fields (*) denotes fields which lie within reservation
Plaza* - 2.6 MMBO, 1.7 Mmcf out of 20 wells, 3-4 MMBO ultimate (Bluell)
Wabek* - 5.1 MMBO, 3.6 Mmcf, out of 18 wells, 6-7 MMBO ultimate (Sherwood)
Carnduff
Elmore
MouseRiverPark
Lake
Darling
LoneTree
Wabek
Plaza
Lucky Mound
Centennial
Renville
Ward
McLean
0
Canada
StudyArea
North Dakota
U.S.A. North Dakota
Burke Bottineou
McHenry
Mountrail
Sherwood Shoreline
Index Map 12 24
miles
Figure FB-8.1. Sherwood shoreline trend and position of major oil fields ( after Sperr et al, 1993).
PLAY TYPE 2
Mississippian Shoreline Play
General characteristics - This play is an extension of the northeast shelf playwhich produces from Sherwood and Bluell porosity cycles. In an eastward direction the Mississippian interval subcrops the following formations: Midale, Nesson, Bluell, Sherwood, Mohall, Glenburn, Landa, Wayne, and Lodgepole. Reservoirs are dolomitized carbonates of either algal, oolitic, or bioherm banksalong the shoreline trend. The updip seal can either be an evaporite or a shale. Source rocks are likely contained within the Bakken or other marine shales within the evaporite sequence.R 88 W R 87 W
Figure FB-8.2. Structure map of the Sherwood subinterval - Plaza and Wabek fields (after Sperr et al, 1993).
T 153
Wabek N Field
(Sherwood Prod.) A'
-5200
A
Plaza Field
(Bluell Production)
T 152 N
B B' -5300
-5500
-5400
Plaza Field Parameters
Formation: Mississippian Mission Canyon, Bluell subinterval
Lithology: Light brown-brown, peloidal, ooliticpisolitic, intraclastic andcomposite wackestone-grainstone
Average depth: � 7400-7500 feet
Porosity: � intergranular, vugular, intraparticle; 6-16%
Permeability:� no information
Oil/Gas column:� at least 120 feet, no oil/water contact known
Average net pay: 6 feet
Wabek Field Parameters
Formation: Mississippian Mission Canyon Sherwood subinterval
Lithology: � Light brown-brown, peloidal, oolitic, pisolitic intraclastic and composite wackestone-grainstone
Average depth: � 7300-7500 feet
Porosity: � intergranular, vugular, intraparticle 6-26%, ave.=10%
Permeability: � no information
Oil/Gas column: � at least 100 feet
Average net pay: � 26 feet
7200
7200
Rival
7200
7300
7300
7300L. Bluell
Sherwood
Mohall 7400
Glenburn
7500
7500 D & AIPF 308 BO, 134 MCFG & DST: Rec. 45' SO&GCM,
0 BWPD 270' GCWPerfs: 7324-7366
DEN POR DEN PORDEN POR
8 ø 8 ø
8 ø
NEU POR NEU POR NEU POR
A Se Se 3 Se Nw 2 Sw Sw 32 A'
SW 152N-88W 152N-88W 152N-87W NE
GR CNL/FDC GR CNL/FDC GR CNL/FDC
IPF 259 BO, 129 MCFG & Intershoal Mudstone0 BWPD
Perfs: 7354-7390
Wabek Field Cross-section
Figure FB-8.3. Wabek Field cross-section showing position of productive interval. Datum is top of Sherwood horizon (after Sperr et al, 1993)).
B Ne Ne 20 Ne Ne 21 Ne Ne 22 B'
West 152N-88W 152N-88W 152N-88W East
GR CNL/FDC GR CNL/FDC GR CNL/FDC
IPP 29 BO, 45 MCFG &65 BWPD
Perfs: 7482-7484, 7490-7496 Plaza Field Cross-section
Figure FB-8.4. Plaza field cross-section showing position of productive interval. Datum is top of Sherwood horizon (after Sperr et al, 1993).
Rival
L. Bluell
Sherwood
Mohall
Glenburn IPP 34 BO, 15 MCFG & IP: Non-commercial 57 BWPD Perfs: 7388-7402, 7408-7412
Perfs: 7415-7424,7436-7438 7416-7422
DEN ø DEN ø DEN ø
8 ø 8 ø
8 ø
NEU ø NEU ø NEU ø
7300
7400 7300
7400 7500
7600 7500
7600
7700
Fort Berthold Reservation North Dakota CONVENTIONAL PLAY TYPE 2
Mississippian Shoreline Play
Page 9 of 18
WILLISTON BASIN Lodgepole Buildups
West East
Trough shelfbasin shelf
sea level
Montana
slope
Explanation
Grainstone-packstone beds on flanks of mound
Bryozoan-crinoid buildup facies (potential hydrocarbon reservoir)
Mudstone-wackestone core facies of mound
Wackestone-packstone buildup facies
Figure FB-9.1. Diagrammatic cross-section of Waulsortian Mounds within the Williston Basin, shows facies distribution and general location within the basin (after Burke and Lasemi, 1995).
CANADA
S S
S ?
?
100
300 500 ?
? Montana 900
LB Trough 700 500
BS 500
B ?
300 500
Approximate erosional limit of Madison Formation
Postulated Waulsortian mounds
Known Waulsortian mounds
Fort Berthold
Figure FB-9.2. Generalized isopach map (c.i.=200') of the Lodgepole Formation, Williston Basin in relation to the Fort Berthold Reservation. LB=Little Belt Mountains, B=Bridger Range, BS=Big Snowy Mountains, D=Dickinson Lodgepole Field, S=Saskatchewan (modified from Burke and Lasemi, 1995).
PLAY TYPE 3
Mississippian Lodgepole Waulsortian Mounds
General Characteristics - No production has been established within the reservation, however, there is a productive trend in neighboring Stark County. Similar mounds have been found in outcrop in the big Snowy Mountains, Montana. � Waulsortian facies within the Lodgepole formation are lens-like buildups of massive limestone with abundant crinoid and bryozoan fragments. Potential reservoir intervals are boundstones whose framework constituents consist of crinoids, bryozoans, and lesser amounts of mollusks and corals. Inter and intra-particle porosity is the result of leaching and alteration of these particles.
260
240
234
237
262
303
255
368
Dickinson Field, Lodgepole Formation Williston Basin
R 97 W R 96 W
T 140 N
378
T 139 N
20' Contour Interval
Figure FB-9.3. Isopach map of lower Lodgepole at Dickinson Field (after Burke and Lasemi,1995).
Dickinson Field Lodgepole Parameters
Formation:� Mississippian Lodgepole
Lithology: primarily fossiliferous grainstones with minor amounts of dolomite boundstones, packstones
Average depth: � 9800 feet
Porosity: � 9.4-10% mound core up to 15% in mound flanks
Permeability: � variable, up to 460md
Oil/Gas column: � no information
Average net pay: � at least 50 feet
Other shows: � no information
CONOCO, INC. Figure FB-9.4. Generalized Lodgepolesection depicting Waulsortian MoundKadramas 75 Buildup (after Burke and Lasemi, 1995).NW SE 31-140-96
Stark Co., N.D.
9200
9300
9400
9500
9600
9700
9800
9900
10000
10100
Mission oolitic, pelletal, light yellow-brown, Canyon dolomitic, skeletal packstone to wackestone
Lodgepole
Supra Mound medium to dark gray-brown slightly argillaceous and cherty skeletal wackestones and mudstones
Lower Mound Core Lodgepole light to medium gray-brown mottled with dark brown, bryozoan baffle and
boundstones with grainstone, packstone, and wackestone matrix; abundant coarse calcite cement
Bakken black shale interbedded with argillaceous mudstone and calcareous siltstones
Three Forks light brown gray dolomite interbedded with gray green shale
log marker
GR DLL
oil/water
contact (-7365)
Fort Berthold Reservation North Dakota
CONVENTIONAL PLAY TYPE 3 Mississippian Lodgepole Waulsortian Mound Play
Page 10 of 18
110 100105
A 300 A'
500 100 Antelope300 Ft. Berthold
Blue Buttes Reservation500
700
100
500 North Dakota Montana 500
300 300
300
Ordovician or 100 South Dakota older rocks exposed
Dolomite facies -Red River Wyoming Limestone and dolomite facies Red River
400 contour interval, 200'
Figure FB-10.1. Map showing thickness of Ordovician Red River Formation within the Williston basin and surrounding area, location of analog fields and reservation, and location of regional cross-section A-A' (modified after Peterson, 1987).
PLAY TYPE 4
Ordovician Red River Play
General Characteristics: This is the second most productive formation in theWilliston basin. Reservoirs are dolomite intervals and dolomitic limestonesformed from bioclastic mounds and tidal flat deposits. Cyclic deposits ofcarbonate, evaporite, and organic rich shale provide reservoir, source, and seal.Major accumulations are found on structural noses such as Nesson and Cedar Creek Anticlines. Smaller fields are found in fold structures draped overbasement fault blocks, or small carbonate mounds.� The source intervals are thermally mature to overmature at the basin center,and become somewhat immature along the basin flanks. Winnipeg shale and marine shales in the Red River Formation are thought to be the primary source of the reservoir oil. Hydrocarbon generation and migration is estimated to have begun in late Paleozoic time.
R 95 W R 94 W
30 29 28 27 26
-11,000 T T 153 -11,145 153
N N
31 32 33 34 35
-11,200 -11,080
-11,100 -11,000
3 2 1 6 5 4
T T -10,993 152 152
N N
7 8 9 10 11 12
Fort Berthold Reservation
R 95 W R 94 W
Note: Wells shown are Red River penetrations only.
Red River production was established at ANTELOPE FIELD Antelope Field in 1989 with the 30-23 Mckeen Red River Structure Map well in section 30, T 153 N, R 94 W
C.I. = 50 feet
Figure FB-10.2. Structure contour map of the Red River Fm., Antelope Field. Contours show the general trend of anticline/fold development.
Blue Buttes Field Parameters
Formation: Ordovician Red River
Lithology: black to dark gray dolomite, limestone very fine grained to crystalline � occasionally sucrosic texture
Average depth: � -11,300 MSL
Porosity: � 9.8%
Permeability: � 1.0 md
Oil/Gas column: � unknown
Average net pay thickness: � 23 feet
Other shows: � Kibbey Sandstone, Kibbey Limestone Charles Formation
Other information:� Initial IP 564 BOPD, API 58 2928 Mcfgpd-discovery well
R 96 W R 95 W
11,300
1 6 1
11,400
11,400 7 12
11,500
T 18 13 11,500 151
N
19 24 11,600
30 25
36 31 36
11,300 1 6 1
7 12 T
11,400 150 N
11,500 18 13
24 19 24
R 96 W R 95 W
Note: Only Red River penetrations Blue Buttes Field are shown
Red River Structure Map
CI = 25 feet
Figure FB-10.3. Red River Structure Map - Blue Buttes Field. Showstrend of Anticline development and production.
Antelope Field Parameters
Formation: Ordovician Red River
Lithology: black to dark gray limestone/dolomite very fine grained to crystalline Occasionally sucrosic texture
Average depth: � 13,480-13,490 feet
Porosity: � 12% log density porosity
Permeability: � not known
Oil/Gas column: � no information
Average net pay thickness: � 10 feet
Other shows:� Minnelusa and Charles Formations
Cumulative production: (1995)� 94 MBO, 1.15 Mmcf API 56.2, IP 113 BC, 1452 Mcfgpd
Fort Berthold Reservation North Dakota
CONVENTIONAL PLAY TYPE 4 Ordovician Red River Play
Page 11 of 18
North Dakota
Wyoming
110 100 105
Silurian and older rocks exposed
Limit of Bakken source rocks
A A'
South Dakota
Ft. Berthold Reservation
Montana
contour interval, 200'
Antelope
400
400
200 400
200 200
200
600
600
1000 800
800 1000
2000 1200
1400
1600 1200
1800
600
Bear Den
Limit of Prairie salt
Figure FB-11.1. Map showing thickness of Devonian rocks, limit of Prairie salt, limit of Bakken source rock, location of analog fields and reservation, and location of regional cross-section A-A' (modified after Peterson, 1987).
PLAY TYPE 5
Devonian Nisku-Duperow Play
General Characteristics- This play consists of a carbonate evaporite sequence interbedded with cyclic marine shales. Reservoir rocks are typically dolomite or dolomitized limestone. Source rock for the oil is thought to be from the Bakken interval which is mature-overmature in the central portion of the basin and immature on the flanks. Oil migration and generation are estimated to have begun in early to late Cretaceous time. � Traps are gentle folds and closures related to carbonate bank deposition on paleohighs or shelf areas. These paleostructures are present on regional structural trends such as the Nesson Anticline and Antelope Anticline.
Analog Fields (*) denotes fields which lie within Reservation
Antelope*- � 39 MMBO, 18.9 Mmcf (includes Bakken, Duperow, and Interlake)
Blue Buttes - � 45 MMBO, 28.3 Mmcf (includes Duperow, Interlake, and Red River)
Bear Den - � 1.4 MMBO, 1.5 Mmcf (includes Madison, Duperow)
Croff - � 1.7 MMBO, 4.0 Mmcf (includes Madison, Duperow)
R 96 W R 95 W
Ne Ne Sec. 36, T 149 N, R 96 W GR Laterolog
Birdbear
Duperow
11,300
11,250
T 149 N
-8900
23 24 19
-8950
-9000
26 25 30
-8900
35 36 31
Souris River
dolomite
evaporite Bear Den - Devonian Field shale Mckenzie County
North Dakota
TOP DUPEROW STRUCTURE CI= 50'
Figure FB-11.2. Bear Den - Devonian Field. Shows position of dolomitic intervals relative to the interbedded evaporite seals. Productive interval indicated in black.
Bear Den Field Parameters
Formation: Devonian Duperow
Lithology: microcrystalline dolomite with fair microsucrosic porosity
Average depth: � 11,300 feet
Porosity: � variable, microsucrosic
Permeability: � not known
Oil/Gas column: � variable
Average net pay thickness: 13 feet
Other info: � no H2S
Antelope Field Parameters
Formation: � Devonian Duperow
Lithology: � dolomite, brown, finely crystalline, granular to vugular limestone intervals, fossiliferous
Average depth:� 10,750 feet
Porosity: � variable, granular, vuggy
Permeability:� not known
Oil/Gas column:� variable
Average net pay thickness:� variable
Other shows:� Madison, Interlake, Sanish
Other information:� No H2S
Figure FB-11.3. Structure map of Antelope Field. Shows general anticlinal fold trend to the southeast. Inset shows position of Bakken relative to Duperow Formation.
R 95 W R 94 W
30 29 28 27 26
T T 153 153
N N
31 32 33 34 35
R 95 W R 94 W
3 2 1 6 5 4
T T 152 152
N N
7 8 9 10 11 12
18 17 16 15 14 13
18 20 21
22 24
30 29 28
ANTELOPE FIELD
Devonian Duperow Structure Map
C.I. = 100 feet
Fort Berthold Reservation
-8200
-8100
-8300
-8400
-8600
Bakken
Devonian Duperow
Limestone
Shale
Dolomite
Fort Berthold Reservation North Dakota
CONVENTIONAL PLAY TYPE 5 Devonian Nisku - Duperow Play
Page 12 of 18
Ft. Berthold 110 105 Reservation 100
A 1100 Antelope
A'
900
700 0
500 0
North Dakota 300
South Dakota
100 Montana
Wyoming
Silurian and older rocks exposed
Limey dolomite facies
dolomite facies
100 contour interval, 200'
Figure FB-12.1. Map showing thickness of Silurian Interlake Formation, facies type, location of analog field and reservation, and location of regional cross-section A-A' (modified after Peterson, 1987).
PLAY TYPE 6
Pre-Prairie ( Winnipegosis/Interlake Play)
General Characteristics - Regional carbonate units of lower Devonianand Silurian age are overlain by the Prairie Evaporite which acts as a seal rock. Typical reservoirs in the Winnipegosis are reefs or dolomitized carbonate mounds. Unconformity traps are thought to exist in the Silurian Interlake Formation which can result in dolomitized reefs, minor karsting, and dissolution porosity in tidal deposits. � The Ordovician Red River shales are thought to be the source rocks for this play and are thermally mature within the basin center. Typical traps consist of gentle folds with flexure faulting associated with the regionalstructure. Stratigraphic traps (either pinch-outs or porosity variations) may exist as well.
Antelope Field Parameters
Formation:� Silurian Interlake
Lithology: dolomite, cream to dark brown possible algal forms, microcrystalline and vugular in part
Average depth: � -9600 feet MSL
Porosity:� variable, granular, vuggy, 7.5%
Permeability:� 1.3md
Oil/Gas column:� variable
Average net pay thickness:� variable
Other shows:� Madison, Duperow, Sanish
Blue Buttes Field Parameters
Formation:� Silurian Interlake
Lithology:� Dolomite
Average depth:� 12,300 feet (-9967 MSL)
Porosity:� 12%
Permeability:� not known
Oil/Gas column:� not known
Average net pay thickness:� 30 feet Borehole Compensated
Sonic Log Amerada Hess
9-43 Jones ne se 9-150n-95w
Interlake: 12,315-12,356 12,372-12,394 12,404-12,418
1220
012
300
Productiveinterval
1240
012
500
Figure FB-12.2. Example of wireline log through Silurian interval in Blue Buttes Field.
T 30 25
152-9898 N
NDE NDE
NDE 32 36
NDE
NDE
-9951 NDE NDE NDE
5 1 -9917
NDE-9997
NDE NDE
8 12
NDENDE
-10027 T -9967
NDE 17 13 151
-9996 N NDENDE -9935
-10022 -9880
20 24
Blue Buttes Field 25
Interlake Structure Map Fort Berthold
C.I. = 25 feet R 96 W
Figure FB-12.3. Structure contour map of Interlake interval, Blue Buttes Field. Shows anticlinal nose development withproduction located somewhat off structure. This indicates a strong stratigraphic component which assists trapping mechanism.
Laterolog with Gamma Ray
Amerada Petroleum 1 Antelope Unit 'A' ne se 1-152n-95w
Silurian 11,727-11826
1170
0
ProductiveInterval
1180
0
Figure FB-12.4. Example of Antelope Field wireline log in the Silurian interval.
R 95 W R 94 W
-9759
30 29 28 27 26-9733
T -9702 T153 -9755 153
N -9694 N
31 32 33 34 35 -9650
-9722 -9600
-9653
3 2 1 6 5 4
-9800 -9700 -9600 TT 152152 -9615 NN
Fort Berthold Reservation7 8 9
10 11 12
R 95 W R 94 W
Note: Wells shown are deeper than Devonian
ANTELOPE FIELDSilurian Structure Map
C.I. = 25 feet
Figure FB-12.5. Silurian structure map, Antelope Field. Shows anticlinal fold trend to thesoutheast with production strongly coincident with structure.
Fort Berthold Reservation North Dakota
CONVENTIONAL PLAY TYPE 6 Pre-Prairie (Winnipegosis/Interlake Play)
Page 13 of 18
110 100 105
200
A 600 A'
400 600 Ft. Berthold
0 Reservation 600 600 Dickinson Field 0 1000 400
800 600 400 North Dakota
200
0
Montana
Cambrian and older rocks exposed
sandstone and sandy Wyoming South Dakota shale facies 0 green, gray, and red shale with minor limestone
200 200 foot contour interval
Figure FB-13.1. Thickness of Upper Mississippian - Lower Pennsylvanian Big Snowy Group interval (Tyler-Heath), location of Fort Berthold Reservation, Dickinson Field (analog), and location of regional cross-section A-A' (modified after Peterson, 1987).
Fd
Gamma Ray / Neutron Log UNITEX Ltd. 6 - 1 Walton
ne ne 6 - 139n - 96w HEATH 7,800- 7,832 FT
7500
7600
7700
7800
Productive interval
Figure FB-13.3. Well log example from Dickinson Field. Upper Mississippian -Lower Pennsylvanian
Dickinson Field - Heath Pool R 97 W R 98 W
6 1 6 1
T 140 N
-5380
-5360 -5320
-5300 -5340
31 36 31 -5280 36 -5240
6 -5260 6 1 -5260
T 139 CI = 20 ' N
igure FB-13.2. Structure map of Dickinson Field, top of Heath. Complex structural configuration reflects the epositional patterns associated with fluvial, deltaic and nearshore marine environments (after Williston Basin Field
Summaries, 1984).
PLAY TYPE 7 Post Madison Clastics (Tyler-Heath)
General Characteristics - Regional deposition of fluvial, deltaic, and nearshore marine sandstones and carbonates provides the potential reservoirs for this play type. Dark gray to black, organic rich, marine shales of the Tyler are considered to be the main source rock which charge these reservoirs. The shales are thermally mature in the center of the basin and immature along the flanks. Onset of oil generation and migration is thought to have occurred in late Cretaceous to early Tertiary time. � Lateral discontinuity of potential reservoirs in the well-sorted fluvial and nearshore marine sandstones is the norm. In general, areal extent of reservoirs is limited with possible internal porosity and permeability barriers. Overall porosities may be quite good (10-16%). Tyler sandstones are roughly time equivalent to the Morrow sandstones of the mid-continent.
Dickinson Field Parameters
Formation: � Pennsylvanian TylerMississippian Heath
Lithology: Interbedded sandstones and
shales
Average Depth: � 7800 feet
Porosity: � 12%
Permeability: � 194 md
Oil/Gas Column: � not known
Average net pay: � variable
Other Shows: � shows in deeper Mississippian intervals�
Fort Berthold Reservation North Dakota
CONVENTIONAL PLAY TYPE 7 Post Madison Clastics (Tyler-Heath)
Page 14 of 18
110 100 105 0 100 40 20 0
A 100 60 A' 0 80 Antelope
120 Ft. Berthold Reservation 120
Taylor 100
North Dakota 120 80
150 60 40
Montana 20 100
60 40 100
80 Cambrian and older rocks exposed
Wyoming South Dakota sandstone facies
40 0 20shale, sandstone and 0 minor limestone facies
green shale facies
40 contour interval, 20'
Figure FB-14.1. Thickness of Deadwood and equivalent rocks, location of analog fields, location of reservation, and location of regional cross-section A-A' (modified after Peterson, 1987).
PLAY TYPE 8
Pre-Red River Gas Play
General Characteristics - Production has been established from Ordovician (Winnipeg) and Cambrian (Deadwood) sandstones. These units are located within the thermally mature or overmature hydrocarbon window of the Williston basin. Both gas and condensate are produced. � Reservoir intervals contain a 'clean' quartz sandstone, silica cement, and enhanced fracture porosity. Source rock is considered to be a marine shale either within the Deadwood or the Winnipeg sandstone. Hydrocarbon generation is thought to have occurred in late Cretaceous to early Tertiary time. Traps are generally asymmetric folds associated with major structural fault zones or hinge lines. � Locations of the fields used as analogs for this play type are noted on the regional facies map. Fort Berthold reservation is bracketed by these fields and in an optimum facies position for possible plays of this type to occur within the boundary of the reservation.
Taylor Field - Winnipeg Pool R 93 W R 92 W
T
-9650 140 N
-9600
-9550
-9500
-9550 TA
-9450
-9362 TA -9453 TA -9400 Taylor Field T Area 139
-9500 -9400
-9350 N -9336 -9322
-9450
-9300
-9248 -9400
-9250
-9350
T -9300 -9200-9250 138
N
-9200 -9150 CI=50 ft
Figure FB-14.4. Taylor Field, Winnipeg Structure. Production strongly correlated to major fault with associated anticlinal nose development to the northwest (from Williston Basin Summaries, 1994).
R 95 W R 94 W
30 29 28 27 26
T -12,044 T 153 153
N N
31 32 33 34 35 -11,622
-12,000-11,700
-11,830
3 2 1 6 5 4 -11,647
T T 152 152
NN 7 8 9
10 11 12 Fort Berthold Reservation
R 95 W R 94 W
Note: Gas wells shown are Winnipeg/Deadwood penetrations only.
ANTELOPE FIELD Winnipeg/Deadwood production was established at the 1-32 Brenna Lacy well in Winnipeg Structure Map section 1, T 152 N R 95 W. Cumulative production (1995) is 3037 BO and 5.3 MMcf.
C.I. = 100 feet
Figure FB-14.2. Structure contour map of the Winnepeg Fm., Antelope Field. Shows Winnepeg production correlated with anticlinal fold trend to the southeast.
Antelope Field Parameters
Formation: Ordovician Winnipeg and Cambrian Deadwood
Lithology: very fine to fine grained, occasionally medium grainedquartz sandstone, occasionally carbonaceous and pyritic
Average Depth:� 13,900 feet
Porosity:� 12-18% depending upon interval
Permeability: � no information
Oil/Gas column:� no information
Average net pay: � 40-50 feet
Other shows:� no information
Other information: 1-32 Brenna-Lacy (1992) completed in Winnipeg-Deadwood. IPF 8BCPD, 5924 MCFGPD. SI for gas. Cumulative production - (1995) 3037 BO, 5.4 MMCF.
Compensated Densilog-Compensated Neutron-Gamma Ray Log
Gulf Oil 1-24-1C Ogre
se nw 24-139n-93w
1140
011
400
1150
0
GR
1160
011
700
N
D
1180
0
Productiveinterval
Figure FB-14.3. Example of Winnipeg-Deadwood formation log signature from Taylor field.
Taylor Field Parameters
Formation: � Ordovician Winnipeg and Cambrian Deadwood
Lithology:� Interbedded shales and sandstones Sandstone consists of very fine grained quartz (based on Richardson Field core, Gulf Oil Leviathan 1-21-B
Average depth: � 11,760-11,780 feet
Porosity: � variable, 12-14% density log porosity
Permeability: � no information
Oil/gas column: � no information
Average net pay: no information
Other shows: � no information
Other information: Discovery well for Taylor Field, 120 BCPD, 4.54 MMCFPD, 57.9 API. Cumulative production (1995) 128,730 BO, 5.3 MMCF.
Fort Berthold ReservationNorth Dakota
CONVENTIONAL PLAY TYPE 8 Pre - Red River Gas Play
Page 15 of 18
?
Canada United States
100
? 200
225
125
? 250
225 Immature
200 "Low-Resistivity"
Approximate Limit Of Bakken Formation Bakken Shale (Modified from Sandberg, 1962) Organic-rich rocks
175 150 have not yet generated
Mature "High" Resistivity Bakken Shale hydrocarbons - matrix Organic-rich rocks have generated porosity is water
Resistivity hydrocarbons-matrix porosity is saturated. Control Point oil saturated. (Induction or Laterolog)
North Dakota
South Dakota
Mon
tana
Figure FB-15.1. Areas of "high" and "low" electrical resistivity in Bakken shales, with subsurface isotherm contours (degrees) and interpreted area of source-rock maturity (after Messiner, 1984).
PLAY TYPE 9
Bakken Fairway/Sanish Sand Play
General Characteristics - The fractured Bakken Formation can be subdivided into three distinct rock types. The upper and lower zones are black shale with a high organic matter content. The middle zone is a relatively lean organic shale/siltstone. U.S.G.S. analyses of the Bakken indicates that 11.5-12.1 weight percent of the shale is organic carbon. Evidence suggests that the Bakken has generated hundreds of billions of barrels of oil. � The Bakken Fm, where it exists, is thermally mature (see map). It forms a continuously sourced, self-sealed reservoir. Production is
controlled by fractures; matrix porosity and permeability are low. Different fairways are assumed to exist. The areas with the highest potential have elevated thermal maturity, proximity to subcrop, close fracture spacing and proximity to basin flexure hinge lines. Vitrinite reflectance should be greater than 0.9-1.02. � The United States Geological Survey considers Antelope field a special category of Bakken fairway production. The Sanish sand is locally developed, brown, dolomitic, friable, and a slightly argillaceous sandstone with about 6-7% porosity.
Fort Berthold reservation is ideally situated for mature Bakken production. The Bakken source interval is thought to have generated over 1 billion barrels of oil but production/migration from the interval is problematic. Mechanisms for emplacement outside the Bakken interval are described below in the west/east cross-section. Production within the Bakken must be concentrated in intervals where fractures (original or induced) can remain open to fluid flow.
Dakota
CANADA
North
South Dakota
USA
-5500
Oil and/or Gas Production
Contour Interval 500 Feet
-2000 -2000
Rock
ton-Fr
oid
Fault
Zone
-3000
-4000 W
eldon
Fau
lt
-9000
-5000
South Limit
-800
0-7
000
-6000
of Bakken
-600
0
-4000-3000
-5500 Formation
-500
0
-500
0
-400
0
-500
0
-300
0
-200
0
Mo
nt.
-100
0
Wyo
min
g -1000
-2000
Figure FB-15.2. Williston Basin with structure contours on the base of Mississippian strata and limit of Bakken Formation (after Webster, 1987).
Borehole Compensated Sonic Log
William C. Kirkwod 42-8 Melby
se ne 8-152n-94w
Caliper SPHI Limestone 6.0 GR 16.0 6.300 DT -0.100 0.0 100.0 96.00 40.00
10500
caliper
GR
10600
DT
Ø Bakken Shale
interval
10700
Figure FB-15.3. Example of log signature from Antelope Field showing Bakken shale interval with sand/silt development
Antelope Field - Sanish Pool R 94 W
-8362
-8350
-8483
-8404
-8450
-8425
-8400
-8375 -8475
-8450
-8468
-8477
T
153
N
T 151 N
Antelope Field Parameters
Formation:� Bakken shale/Sanish sandstone interval
Lithology: � sandstone, dolomitic, brown, friable, slightly argillaceous
Average depth:� 10,525 feet
Porosity: � 7.4 average
Permeability:� low, changes across structure with the sand/silt content
Oil/Gas column: � no information
Average net pay: variable
Other formations Mission Canyon, with shows:� Devonian and Winnipegosis
Other information: Discovery well was Woodward Star-Tribal, sw se 21 T152N R 94 W; 550 BOPD (1953)
Figure FB-15.4. Structure map of the Sanish Pool, Antelope field (from Williston Basin Field Summaries, 1984).
West
Nesson Axis
Source Rock (Upper and Lower Bakken Shales)
Charles Formation
Bakken Formation "Maturity"
? East
Jurassic Jurassic
Big Snowy Group
Triassic
Devonian
Madison Group (L-M Miss.)Mission Canyon Fm.
Lodgep
ole
Nisku Fm.
Poor Porosity
Good Porosity
Interbedded Salt, Anhydrite and generally Black organic-rich Shale: Upper and "Maturity" dense "tight" Dolomite and Limestone: Lower Bakken Shale Members Charles Formation Hydrocarbon Accumulation
Migration Flow Direction Light-colored generally porous Limestone and Dolomite- Calcareous-dolomitic Siltstone: Middle oolitic, pelletal and skelletal i.p.: Mission Canyon and Bakken Siltstone Member Nisku Fms.
Dark-colored generally dense "tight" Shaley Limestone- Grey-green-red Dolomite, Shale, and Overpressure Cell Siliceous (tr iangle), i.p.: Lodgepole Formation Siltstone: Three Forks Formation Fractures
Figure FB-15.5. Schematic east-west section across the Williston Basin showing source-rock maturity, fluid over-pressure, fracture, migration and hydrocarbon accumulation patterns in the Bakken formation and adjacent units (after Messiner, 1984).
Fort Berthold Reservation North Dakota
UNCONVENTIONAL PLAY TYPE 9 Bakken Fairway/Sanish Sand Play
Page 16 of 18
http:0.9-1.02
Cretaceous Epeiric Seaway
Greenland Alaska
Canada
Cretaceous Epeiric Seaway
United States
0 Cretaceous Epeiric Seaway
Mexico Cuba
Figure FB-16.1. Paleogeographic map of North America during Late Cretaceous time, showing the extent of the Cretaceous seaway (after Rice and Shurr, 1980).
Sys
tem
Ser
ies
Formations
Te
rtia
ry
Pa
leo
cen
e
Fort Union Formation
Hell Creek Formation
Fox Hills Sandstone
Bearpaw Shale
Judith River Formation
Up
per PierreClaggett Shale
Shale
Eagle Sandstone Gammon
Shale
Cre
tace
ou
s
Niobrara Formation
Carlile Shale
Greenhorn Formation
Belle Fourche Shale
Mowry Shale
Muddy Sandstone unconformity
Skull Creek Shalenonmarine
Lo
wer
Fall River Sandstone rocks coastal sandstones
Kootenai Formation calcareous rocks
Sunburst SS Mbr. marine siltstones and shalesCut Bank SS Mbr.
uncon