Montana – North Dakota? Middle Member Bakken Play

48
Montana Montana North Dakota? North Dakota? Middle Member Middle Member Bakken Bakken Play Play Julie A. LeFever Julie A. LeFever North Dakota Geological Survey North Dakota Geological Survey

Transcript of Montana – North Dakota? Middle Member Bakken Play

Page 1: Montana – North Dakota? Middle Member Bakken Play

Montana Montana –– North Dakota?North Dakota?Middle Member Middle Member BakkenBakken PlayPlay

Julie A. LeFeverJulie A. LeFeverNorth Dakota Geological SurveyNorth Dakota Geological Survey

Page 2: Montana – North Dakota? Middle Member Bakken Play

MTMT

WYWY

SDSD

NDND

MBMBSKSKABAB

Richland Co.

Richland Co.

McKenzie Co.

McKenzie Co.

MTMT NDND Study AreaStudy Area

Williston BasinWilliston Basin

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BakkenBakken FormationFormation

•• Geology Geology –– StratigraphyStratigraphy–– LithologyLithology–– Depositional Environments/HistoryDepositional Environments/History–– AgeAge–– Source Rock PotentialSource Rock Potential

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StratigraphyStratigraphy

Three Forks Formation (Devonian)Three Forks Formation (Devonian)•• Conformable & UnconformableConformable & Unconformable•• 250 ft thick250 ft thick•• ShalesShales, , dolostonesdolostones, siltstones, and sandstones, siltstones, and sandstones•• ““SanishSanish SandSand””

•• SublittoralSublittoral to to supralittoralsupralittoral

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10608 ft.10608 ft.

SESW Sec. 13, T.23N.,R.56E.SESW Sec. 13, T.23N.,R.56E.

AHEL #1 H8 AHEL #1 H8 NevinsNevins

Three Forks Fm.Three Forks Fm.

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StratigraphyStratigraphy

BakkenBakken FormationFormation•• NomenclatureNomenclature

–– Defined in 1953Defined in 1953–– Amerada Petroleum Amerada Petroleum -- #1 H.O. #1 H.O. BakkenBakken–– Restricted to the SubsurfaceRestricted to the Subsurface

–– 105 ft thick105 ft thick–– upper and lower shaleupper and lower shale–– middle limestone membermiddle limestone member

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IsopachIsopach of the of the BakkenBakken FormationFormation

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Distribution Distribution of the of the

BakkenBakken ShaleShale

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StratigraphyStratigraphyBakkenBakken FormationFormation

LithologyLithologyLower Shale MemberLower Shale Member

50 ft thick50 ft thickDark brown to black, fissile, nonDark brown to black, fissile, non--calcareous, calcareous, organicorganic--rich shalerich shaleQuartz, pyrite Quartz, pyrite

fossils fossils -- conodontsconodonts, algal spores, brachiopods, , algal spores, brachiopods, fish teeth, bones, and scalesfish teeth, bones, and scales

Fractured with oil stainingFractured with oil staining

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IsopachIsopach of theof theLower Lower BakkenBakken ShaleShale

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10604.5 ft.10604.5 ft.

SESW Sec. 13, T.23N.,R.56E.SESW Sec. 13, T.23N.,R.56E.

AHEL #1 H8 AHEL #1 H8 NevinsNevins

Bakken/Three ForksContact

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StratigraphyStratigraphyBakkenBakken FormationFormation

Middle MemberMiddle Member85 ft thick85 ft thick5 different 5 different lithofacieslithofacies

Calcareous siltstone to sandstone, Calcareous siltstone to sandstone, dolostonedolostone, , siltysiltylimestone, and limestone, and ooliticoolitic limestonelimestone

Locally productiveLocally productive

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IsopachIsopach of theof theMiddle Middle BakkenBakken MemberMember

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LithofaciesLithofacies of the Middle Memberof the Middle Member

Upper Shale

LithofaciesLithofacies 5 5 -- SiltstoneSiltstone

LithofaciesLithofacies 4 4 –– InterbeddedInterbedded Dark Grey ShaleDark Grey Shaleand Buff and Buff SiltySilty SandstoneSandstone

LithofaciesLithofacies 3 3 -- SandstoneSandstone

ProductiveProductive

LithofaciesLithofacies 2 2 –– InterbeddedInterbedded Dark Grey ShaleDark Grey Shaleand Buff and Buff SiltySilty SandstoneSandstone ProductiveProductive

LithofaciesLithofacies 1 1 -- SiltstoneSiltstone

Lower Shale (From LeFever and others, 1991)

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SESW Sec. 13, T.23N.,R.56E.SESW Sec. 13, T.23N.,R.56E.

AHEL #1 H8 AHEL #1 H8 NevinsNevins

Middle MemberMiddle MemberLithofaciesLithofacies 22

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10585 ft.10585 ft.SESW Sec. 13, T.23N.,R.56E.SESW Sec. 13, T.23N.,R.56E.

AHEL #1 H8 AHEL #1 H8 NevinsNevins

Middle MemberMiddle MemberLithofaciesLithofacies 22

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1058210582 ftft

SESW Sec. 13, T.23N.,R.56E.SESW Sec. 13, T.23N.,R.56E.

AHEL #1 H8 AHEL #1 H8 NevinsNevins

Upper Shale/Middle Upper Shale/Middle MbrMbrContactContact

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StratigraphyStratigraphyBakkenBakken FormationFormation

Upper MemberUpper MemberMaximum extent of the Maximum extent of the BakkenBakken23 ft thick23 ft thickConformable and UnconformableConformable and UnconformableLaminated to massive with poorly sorted Laminated to massive with poorly sorted beds of siltbeds of silt--sized materialsized materialLag sandstoneLag sandstone

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IsopachIsopach of theof theUpper Upper BakkenBakken ShaleShale

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10580 ft.10580 ft.

SESW Sec. 13, T.23N.,R.56E.SESW Sec. 13, T.23N.,R.56E.

AHEL #1 H8 AHEL #1 H8 NevinsNevins

BakkenBakken FormationFormationUpper Shale MemberUpper Shale Member

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StratigraphyStratigraphy

•• LodgepoleLodgepole FormationFormation–– ConformableConformable–– 900 ft thick900 ft thick–– ““False False BakkenBakken””; ; PelmatozoanPelmatozoan LimestoneLimestone–– 5 major 5 major lithofacieslithofacies representing a marine representing a marine

transgressiontransgression

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“False Bakken”

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SESW Sec. 13, T.23N.,R.56E.SESW Sec. 13, T.23N.,R.56E.

AHEL #1 H8 AHEL #1 H8 Nevins

10562 ft.10562 ft.

Nevins

LodgepoleLodgepole Fm.Fm.False False BakkenBakken

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10564 ft.10564 ft.

SESW Sec. 13, T.23N.,R.56E.SESW Sec. 13, T.23N.,R.56E.

AHEL #1 H8 AHEL #1 H8 NevinsNevins

LodgepoleLodgepole Fm.Fm.PelmatozoanPelmatozoan LimestoneLimestone

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BakkenBakken FormationFormation

•• Depositional Environments/AgeDepositional Environments/Age–– Stratified water column offshore, marine Stratified water column offshore, marine

environmentenvironment–– BakkenBakken ShalesShales

•• Anoxic bottom conditionsAnoxic bottom conditions–– Middle MemberMiddle Member

•• Aerobic marine to marginal marine conditionsAerobic marine to marginal marine conditions–– Devonian/MississippianDevonian/Mississippian

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Depositional HistoryDepositional History

•• Three Forks FormationThree Forks Formation–– Shallow marine to terrestrial sedimentationShallow marine to terrestrial sedimentation

•• BakkenBakken FormationFormation–– TransgressionTransgression

•• ShalesShales –– anoxic conditionsanoxic conditions•• Middle Member Middle Member –– normal, shallow marinenormal, shallow marine•• NonNon--deposition/erosiondeposition/erosion

•• LodgepoleLodgepole FormationFormation–– Normal marine conditionsNormal marine conditions

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Source Rock PotentialSource Rock Potential

•• Total Organic Content Total Organic Content –– 0 to 40%0 to 40%–– Decrease towards depositional edgeDecrease towards depositional edge

•• KerogenKerogen–– 7070--90% amorphous90% amorphous–– 00--20% herbaceous20% herbaceous–– 30% coaly30% coaly–– 5% woody5% woody

•• Formed in Formed in subaquaticsubaquatic oxygenoxygen--restricted restricted environmentenvironment

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Source Rock PotentialSource Rock Potential

•• Hydrocarbon GenerationHydrocarbon Generation–– Depth of 9000 ftDepth of 9000 ft–– 100100oo CC

•• Volume of Oil GeneratedVolume of Oil Generated–– Up to 413 billion barrels (ND & MT)Up to 413 billion barrels (ND & MT)

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Immature

Onset of Generation

IntenseGeneration

Source Rock Maturity ZonesSource Rock Maturity Zones

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Richland CountyRichland County

80 Producing Fields80 Producing Fields1.1. Red River FmRed River Fm2. Madison Fm 2. Madison Fm 3. 3. BakkenBakken FmFm4. 4. DuperowDuperow FmFm5. Interlake Fm5. Interlake Fm

20 Fields produce(d) from the 20 Fields produce(d) from the BakkenBakken FormationFormation

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BakkenBakken FormationFormationRichandRichand County, MTCounty, MT

• HistoricallyHistorically ––46 wells have produced from the 46 wells have produced from the BakkenBakken+ a few commingled wells+ a few commingled wells

•• CurrentlyCurrently ––31 wells reported production in 200031 wells reported production in 2000Total production for 2000 = 145,323 Total production for 2000 = 145,323 bblsbbls oiloil

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Richland CountyRichland County

1.1. 555 Wells Examined in555 Wells Examined inRichland CountyRichland County

2.2. Data Included:Data Included:1.1. Last Charles SaltLast Charles Salt2.2. Lower Lower LodgepoleLodgepole3.3. BakkenBakken FormationFormation4.4. Porosity zonePorosity zone5.5. Three Forks FormationThree Forks Formation6.6. Devonian Prairie SaltDevonian Prairie Salt

3.3. Combined with ExistingCombined with ExistingND DataND Data

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Extent of DataExtent of Data

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-7500-7400-7300-7200-7100-7000-6900-6800-6700-6600-6500-6400-6300-6200-6100-6000-5900-5800-5700

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BLCS Structure MapBLCS Structure Map

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Formation LimitsFormation Limits

?

MontanaMontana North DakotaNorth Dakota

BakkenBakken FormationFormation

UpperUpper

MiddleMiddle

LowerLower

Prairie Salt EdgePrairie Salt Edge

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ft

0102030405060708090100110120130140

IsopachIsopach of the of the BakkenBakken FormationFormation

MontanaMontana North DakotaNorth Dakota

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IsopachIsopach of the Lower Memberof the Lower MemberBakkenBakken FormationFormation

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BakkenBakken LimitLimit

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IsopachIsopach of the Upper Memberof the Upper MemberBakkenBakken FormationFormation

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IsopachIsopach of the Middle Memberof the Middle MemberBakkenBakken FormationFormation

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BalcronBalcron Oil Oil -- #44#44--24 24 VairaVairaSESE Sec. 24, T.24N., R.54E.SESE Sec. 24, T.24N., R.54E.

Neutron PorosityNeutron Porosity

DensityDensity PorosityPorosity

GRGR

LodgepoleLodgepole Fm.Fm.

Three Forks Fm.Three Forks Fm.

Bak

ken

Bak

ken

Fm.

Fm. upper

middle10

000

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BakkenBakken Middle MemberMiddle MemberPorosity ZonePorosity Zone

MontanaMontana NorthNorth DakotaDakota

Porosity Zone Porosity Zone ContoursContours

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BakkenBakken Middle MemberMiddle MemberPrairie SaltPrairie Salt

MontanaMontana North DakotaNorth Dakota

Prairie SaltPrairie SaltEdgeEdge

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PrairiePrairie SaltSalt

BakkenBakken Middle MemberMiddle MemberPrairie SaltPrairie Salt

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Middle MemberMiddle MemberPorosity ZonePorosity Zone

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Contour Interval: 2 ft.Contour Interval: 2 ft.

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BakkenBakken Middle MemberMiddle MemberSandstone UnitSandstone Unit

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Shell Oil Company Shell Oil Company -- #12#12--66--44 U.S.A.44 U.S.A.SENWNW Sec. 6SENWNW Sec. 6--T.148N.T.148N.--R.104WR.104W..

1060010600

Bak

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Bak

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Fm.

Fm.

MiddleMiddleMbrMbr

UpperUpperShaleShale

GR Density Porosity

Neutron PorosityThree Forks Fm.Three Forks Fm.

LodgepoleLodgepole Fm.Fm.

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Can the Can the BakkenBakken Play Play Extend into North Dakota?Extend into North Dakota?

YES!YES!

•• Production from the same intervalProduction from the same interval

•• MappableMappable log log characterisiticscharacterisitics from MT into NDfrom MT into ND

•• Prominent trends illustrated on Prominent trends illustrated on BakkenBakken mapsmaps

•• Other intervals within the middle member that Other intervals within the middle member that have similar potentialshave similar potentials