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Montana – North Dakota? Middle Member Bakken Play

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Title: Montana – North Dakota? Middle Member Bakken Play


1
Montana North Dakota?Middle Member Bakken Play
  • Julie A. LeFever
  • North Dakota Geological Survey

2
Williston Basin
SK
AB
MB
MT
ND
SD
WY
Richland Co.
McKenzie Co.
MT
ND
Study Area
3
Bakken Formation
  • Geology
  • Stratigraphy
  • Lithology
  • Depositional Environments/History
  • Age
  • Source Rock Potential

4
Stratigraphy
  • Three Forks Formation (Devonian)
  • Conformable Unconformable
  • 250 ft thick
  • Shales, dolostones, siltstones, and sandstones
  • Sanish Sand
  • Sublittoral to supralittoral

5
Three Forks Fm.
10608 ft.
SESW Sec. 13, T.23N.,R.56E. AHEL 1 H8 Nevins
6
Stratigraphy
  • Bakken Formation
  • Nomenclature
  • Defined in 1953
  • Amerada Petroleum - 1 H.O. Bakken
  • Restricted to the Subsurface
  • 105 ft thick
  • upper and lower shale
  • middle limestone member

7
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8
Isopach of the Bakken Formation
9
Distribution of the Bakken Shale
10
StratigraphyBakken Formation
  • Lithology
  • Lower Shale Member
  • 50 ft thick
  • Dark brown to black, fissile, non-calcareous,
    organic-rich shale
  • Quartz, pyrite
  • fossils - conodonts, algal spores, brachiopods,
    fish teeth, bones, and scales
  • Fractured with oil staining

11
Isopach of theLower Bakken Shale
12
Bakken/Three ForksContact
10604.5 ft.
SESW Sec. 13, T.23N.,R.56E. AHEL 1 H8 Nevins
13
StratigraphyBakken Formation
  • Middle Member
  • 85 ft thick
  • 5 different lithofacies
  • Calcareous siltstone to sandstone, dolostone,
    silty limestone, and oolitic limestone
  • Locally productive

14
Isopach of theMiddle Bakken Member
15
Lithofacies of the Middle Member
Upper Shale
Lithofacies 5 - Siltstone
Lithofacies 4 Interbedded Dark Grey Shale
and Buff Silty Sandstone
Lithofacies 3 - Sandstone
Productive
Lithofacies 2 Interbedded Dark Grey Shale
and Buff Silty Sandstone
Productive
Lithofacies 1 - Siltstone
Lower Shale
(From LeFever and others, 1991)
16
Middle MemberLithofacies 2
SESW Sec. 13, T.23N.,R.56E. AHEL 1 H8 Nevins
17
Middle MemberLithofacies 2
10585 ft.
SESW Sec. 13, T.23N.,R.56E. AHEL 1 H8 Nevins
18
Upper Shale/Middle MbrContact
10582 ft
SESW Sec. 13, T.23N.,R.56E. AHEL 1 H8 Nevins
19
StratigraphyBakken Formation
  • Upper Member
  • Maximum extent of the Bakken
  • 23 ft thick
  • Conformable and Unconformable
  • Laminated to massive with poorly sorted beds of
    silt-sized material
  • Lag sandstone

20
Isopach of theUpper Bakken Shale
21
Bakken FormationUpper Shale Member
10580 ft.
SESW Sec. 13, T.23N.,R.56E. AHEL 1 H8 Nevins
22
Stratigraphy
  • Lodgepole Formation
  • Conformable
  • 900 ft thick
  • False Bakken Pelmatozoan Limestone
  • 5 major lithofacies representing a marine
    transgression

23
False Bakken
24
Lodgepole Fm.False Bakken
10562 ft.
SESW Sec. 13, T.23N.,R.56E. AHEL 1 H8 Nevins
25
Lodgepole Fm.Pelmatozoan Limestone
10564 ft.
SESW Sec. 13, T.23N.,R.56E. AHEL 1 H8 Nevins
26
Bakken Formation
  • Depositional Environments/Age
  • Stratified water column offshore, marine
    environment
  • Bakken Shales
  • Anoxic bottom conditions
  • Middle Member
  • Aerobic marine to marginal marine conditions
  • Devonian/Mississippian

27
Depositional History
  • Three Forks Formation
  • Shallow marine to terrestrial sedimentation
  • Bakken Formation
  • Transgression
  • Shales anoxic conditions
  • Middle Member normal, shallow marine
  • Non-deposition/erosion
  • Lodgepole Formation
  • Normal marine conditions

28
Source Rock Potential
  • Total Organic Content 0 to 40
  • Decrease towards depositional edge
  • Kerogen
  • 70-90 amorphous
  • 0-20 herbaceous
  • 30 coaly
  • 5 woody
  • Formed in subaquatic oxygen-restricted environment

29
Source Rock Potential
  • Hydrocarbon Generation
  • Depth of 9000 ft
  • 100o C
  • Volume of Oil Generated
  • Up to 413 billion barrels (ND MT)

30
Immature
Onset of Generation
Intense Generation
Source Rock Maturity Zones
31
Richland County
80 Producing Fields1. Red River Fm2. Madison
Fm 3. Bakken Fm4. Duperow Fm5. Interlake
Fm 20 Fields produce(d) from the Bakken Formation
32
Bakken FormationRichand County, MT
  • Historically 46 wells have produced
    from the Bakken a few commingled wells
  • Currently 31 wells reported production
    in 2000 Total production for 2000 145,323
    bbls oil

33
Richland County
  • 555 Wells Examined inRichland County
  • Data Included
  • Last Charles Salt
  • Lower Lodgepole
  • Bakken Formation
  • Porosity zone
  • Three Forks Formation
  • Devonian Prairie Salt
  • Combined with Existing
  • ND Data

34
Extent of Data
35
BLCS Structure Map
ft
Contour Interval
Montana
North Dakota
36
Formation Limits
Bakken Formation
Upper
Middle
Lower
Prairie Salt Edge
Montana
North Dakota
37
Isopach of the Bakken Formation
ft
Contour Interval
Montana
North Dakota
38
Isopach of the Lower MemberBakken Formation
Bakken Limit
ft
Contour Interval
Montana
North Dakota
39
Isopach of the Upper MemberBakken Formation
ft
Contour Interval
Montana
North Dakota
40
Isopach of the Middle MemberBakken Formation
ft
Contour Interval
North Dakota
Montana
41
Balcron Oil - 44-24 VairaSESE Sec. 24, T.24N.,
R.54E.
GR
Density Porosity
Lodgepole Fm.
10000
upper
Bakken Fm.
middle
Three Forks Fm.
Neutron Porosity
42
Bakken Middle MemberPorosity Zone
Porosity Zone Contours
ft
70
65
60
55
50
45
40
Contour Interval
35
30
25
20
15
10
5
0
Montana
North Dakota
43
Bakken Middle MemberPrairie Salt
Prairie Salt Edge
ft
Contour Interval
Montana
North Dakota
44
Bakken Middle MemberPrairie Salt
Prairie Salt
ft
Contour Interval
Montana
North Dakota
45
Middle MemberPorosity Zone

Contour Interval
McKenzie Co.
Richland Co.
Contour Interval 2 ft.
46
Bakken Middle MemberSandstone Unit
ft
Richland Co.
McKenzie Co.
Contour Interval
Montana
North Dakota
47
Shell Oil Company - 12-6-44 U.S.A.SENWNW Sec.
6-T.148N.-R.104W.
Density Porosity
GR
Lodgepole Fm.
Upper Shale
Bakken Fm.
10600
MiddleMbr
Neutron Porosity
Three Forks Fm.
48
Can the Bakken Play Extend into North Dakota?
  • YES!
  • Production from the same interval
  • Mappable log characterisitics from MT into ND
  • Prominent trends illustrated on Bakken maps
  • Other intervals within the middle member that
    have similar potentials
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