Skip to main contentThe Bakken Source System: Emphasis on the Three Forks Formation – North Dakota Geologic Survey Investor Presentation | Shale Experts
The Bakken Source System: Emphasis on the Three Forks Formation Stephan H. Nordeng
Bakken Pool Source Upper and Lower Bakken Informal System Formation Units Shales Lodgepole Reservoirs Mississippian Bakken Shales upper Clastic carbonate middle Bakken middle member of the Bakken Fm. lower Devonian Three…
Bakken Source System Source Reservoirs Upper and lower Middle member Bakken members of the Bakken Lower 50 Lodgepole High TOC average 11% Upper 50 Three Forks by weight Low permeability Oil prone kerogen 7 % porosity…
Where in the Three Forks is the oil
Distribution of Bakken and Three Forks Rocks in North Dakota Lower Middle Bakken Shale Bakken Upper Bakken Shale Three Forks Fm.
Formation water resistivity (0.04 ohm-m) corrected to formation temperature. (1/2)(Rw/Rt)1/2 = Sw
Calculate Oil In Place for One Well Total Oil In Place = Oil in Place Sum Porosity x Oil Saturation x Interval Thickness (ft) = Oil In Place (acre-feet)
Distribution of the wells used to total oil in place. Bakken Bakken and Three Forks Absent Three Forks
Upper 50 Feet of the Three Forks Formation Total Acre-feet oil in place Structure on the top of the Three Forks Fm.
Maturation-Compaction Model Maturation coverts lithostatic load bearing kerogen to oil. Results in source bed compaction. Expels pore fluids from source bed. Resistance to pore fluid expulsion by bounding beds results in fluid…
Formation Pressures in the Antelope Field. Modified from Meissner (1978)
Continuous Water Continuous Oil Water Expulsion Oil Expulsion Chemical Compaction Mechanical Compaction Oil Window Mechanical Compaction Kerogen Discontinuous Oil Discontinuous Water Modified from Meissner, 1978
Why is overpressure significant Surface BuoyancySurface Tension Water Tension Mineral Surface Buoyancy Tension Buoyancy Oil
Unit 5 Unit 3 Unit 2 Unit 6 Anhydrite Unit 4Anhydrite
Oil Generation : When Time Temperature Index and Burial History 43-28H Deadwood Canyon Ranch well (NESE Sec. 28, T154N, R92E) Pierre Onset of Oil Generation Mowry Inyan Kara Swift Spearfish Madison Bakken Three…
Hydrogen Index as a Function of Depth 900 800 700 600 Hydrogen Index 500 400 300 200 100 0 12000 11000 10000 9000 8000 7000 6000 5000 Depth to Bakken (ft.)
900 800 Oil Generation: Where 700 600 Hydrogen Index 500 400 300 200 100 0 12000 11000 10000 9000 8000 7000 6000 5000 Depth to Bakken (ft.)
Apparent Maximum Density Porosity Compaction of the 6000 0 0.2 0.4 0.6 0.8 upper Bakken with depth 7000 8000 Depth (ft.) 9000 10000 11000 12000
Change in porosity with increasing maturation Based on density-neutron porosity logs. 9% decrease in porosity between immature and mature upper Bakken shale.
Conclusions The Three Forks is a basin centered petroleum accumulation. Source rocks are currently in the oil window Porosity and pressure trends in the source system are consistent with maturation driven oil expulsion and…
Acknowlegments Julie LeFever Lynn Helms Ed Murphy Marron Bingle-Davis
Kinetic Model of Oil Generation Continuous Oil Discontinuous Oil 140oC 4oC
Three Forks Porosity from Logs 2000 1800 1600 1400 1200 Map of North Dakota showing the 175 Frequency 1000 800 wells used to determine the frequency 600 distribution of porosity in the upper 50 400 feet of the Three Forks…
Bakken Source System Stratigraphy
Structural Trap Stratigraphic Trap
Extent of the Bakken and Three Forks Formations
Overpressured Oil
Bakken Three Forks Combined County OOIP per County EUR per County OOIP per County EUR per County OOIP per County EUR per County Billings 3,141,271,156 115,858,434 1,717,909,400 154,611,846 4,859,180,556 270,470,280 Botineau --- ---…
Missouri River 2,000 Coal 0 -5,000 Bakken & Three Forks -10,000
Topics Basin Centered Petroleum Accumulations Bakken Source System Three Forks Assessment
Bakken Kerogen Quality Bakken shales are an excellent source rock Quantity of crackable kerogen Total amount of kerogen
Bakken Shale Contains Oil Prone Kerogen Bakken contains Type I and Type II kerogen. Type I and II kerogens tend to generate oil.
Three Forks Grain Density Well Name NDIC Average Grain S.D. Grain Number of Density Density Samples matrix (g/cm3) VAN HOOK 1-13H 16997 2.785 0.0168 37 ST-ANDES-151-89- 17043 2.801 0.0292 14 2413H-1 SUN MARATHON 12033 2.774 0.0175 16…
Pore Fluid Pressurization by Maturation of Kerogen Kerogen Oil Solid Fluid 1) Generated oil displaces pore water. 2) Oil generated at the expense of load bearing kerogen. 3) Water displacement and reduced porosity caused by…
Summary statistics submitted as DMR exhibits Three Forks Pay Thickness Oil Saturation Formation Recovery Porosity (%) Formation (ft.) (% pore space) Volume Factor Factor (%) Average 30.5 64.8 6.93 1.45 8.9 Standard 19.78 11.4 2.33…
Methods Archie Equation for Estimating Water Saturation from Wire Line Logs. Sw = (a/m)(Rw/Rt)1/n a = tortuosity factor = 1 = porosity from logs m = cementation factor = 2 Rw = Resistivity of formation water (0.04 ohm-m 75oF) Rt…
Correcting Rw to Formation Temperature Bottom Hole Temperature (oF) Mean Surface Temp = 40oF Formation Temp (oF) = (BHT- MST) / TD * Formation Depth + MST Total Depth (ft.) Rw depth = R1 * ( T1 +7)/(Formation Temp (oF) +7)…
Calibrating Limestone Density Porosity Logs to Three Forks Density Porosity Logs = (ma-b)/( ma-fl) 40 ls = (2.71 b)/ (2.71-1.18) 35 30 ls(2.71-1.18)-2.71 = b 25 Frequency 20 TF = (2.79 b) / (2.79-1.18) 15 10 5 TF =…
Bottom Hole Temperature (oF) Mean Surface Temp = 40oF Formation Temp (oF) = (BHT- MST) / TD * Formation Depth + MST Sw Water Total Depth (ft.) Saturation or Rw depth = R * ( T +7)/(Formation Temp ( F) +7) o the fraction of 1…
Conventional vs. Bakken Type Conventional Bakken Type Maturation of Source Rock Maturation of Source Rock Expulsion Expulsion Migration Accumulation Driven by buoyancy (oil over water) Trap/Reservoir Short to long distances from…
Paleogeography of North America at the end of the Devonian North Dakota From Ron Blakley
Bakken Source System Stratigraphy Open Marine Open Marine Oxygen Stratified Open Marine Deepening Upward Open Marine - Shoaling Upward Open Marine Oxygen Stratified Regional Unconformity Subtidal to Supratidal Normal Marine Saline…