3D Seismic Attribute Interpretation from the Red River Formation By Mark Sippel Luff Exploration Company for the 14th Williston Basin Petroleum Conference & Prospect Expo Presentation Outline • • • • • • Introduction and Location Overview of Red River Reservoirs Seismic Response and Modeling Description of Red River B Reservoirs Prediction of Depositional Setting Transforms to Reservoir Properties Area of Interest Map 100 Type Log for Red River Formation Stony Mountain Shale 0 C Zone Porosity Member D Zone Porosity Member -300 Lower Red River Relative Depth (feet) -200 -400 -500 Winnipeg Shale -600 Winnipeg Sandstone -700 -800 0 100 200 Gamma 30 20 10 0 -10 Porosity % Paleozoic Ordovician -100 Red River Formation B Zone Porosity Member Upper Red River A Zone Porosity Member The Upper Red River Consists of Four Episodes in Shallow Shelf Setting Main Reservoirs are: Red River B Zone Red River D Zone Time Seconds Normal Polarity 0.7 0.8 0.9 Reverse Forward Seismic Modeling Mission Canyon Upper Red River Reservoirs Are “Seismic Thin Beds” Duperow Reservoir Information Contained in Two Peak-Trough Pairs Interlake 1.0 T1 T2 1.1 P1 P2 Red River Base D zone Winnipeg Each Event Consistently Labeled in Every Seismic Survey Use Synthetic Seismogram for Study of Response to Thickness and Porosity Variation Weak Amplitude Response Low Porosity Strong Amplitude Response High Porosity Time - Seconds 0.0 Interlake Red River 1.0 P1 T1 P2 T2 Winnipeg Description of Red River B Reservoirs • Red River B Porosity Averages Thickness of 7 Feet • Develops at the Top of B Cycle Between Two Anhydrite Layers • Red River B Porosity is Divided into Two Members – Upper and Lower • Red River B (Upper) is Productive Layer • Red River B Development is Strongly Influenced by Depositional Setting • B Cycle Thickness Can Be Predicted from Seismic Attributes Type Log from Red River B Reservoir Top Red River B Anhydrite Upper B Lower B B Cycle 38-55 feet C Anhydrite 0 100 Gamma Ray 30% 0% Neutron-Density Porosity Depositional Model of Red River B Interpretation by Lyn Canter Analytical Description of Red River B Neutron phi Density phi Core phi Core RQI Log BVW 9240 9240 RQI ~ √ k/φ 9242 9242 Evaporite, Anhydrite Depth (feet) 9244 9244 9246 RQI - 10 "Upper B" Dolomite, Agal Boundstone RQI - 13 "Upper B" Dolomite, Bedded Packstone and Grainstone 9246 9248 9248 "Lower B" Dolomitic Limestone, Wackestone RQI - 4 9250 9250 Open Shelf Limestone 9252 9252 9254 9254 0.3 0.2 0.1 0.0 -0.1 Porosity (decimal) -0.2 0.0 0.2 0.4 0.6 Rank (decimal) 0.8 1.0 Capillary Properties Red River B Rock Types Height Above Oil-Water (feet) 1000 RQI = Rock Quality Index RQI ~ √ k/φ Lower B RQI ~ 2 ~ 0.3 microns Pore Throat Diameter 100 Upper B RQI ~ 16 ~ 3.0 microns Pore Throat Diameter 10 0.0 0.2 0.4 0.6 Saturation Sw (decimal) 0.8 1.0 Prediction of B Cycle Thickness from Seismic Attributes • Understand Seismic Response from Forward Modeling • Pick Consistent Times and Amplitudes of Events in Red River Interval • Normalize Each Attribute (Interval Times and Amplitudes) to Mean of 0 and Standard Deviation of 1 • Integration of Multiple 3D Surveys • Determine Thickness of B Cycle from Well Logs in 3D Seismic Surveys • Capture Seismic Attributes at Well Locations • Perform Statistical Correlation of B Cycle Thickness and Seismic Attributes Transform of B Cycle Thickness from Seismic Attributes B Cycle Thickness from Logs (feet) 58 Single 3D Survey Correlation from 9 Wells R = 0.9 Std Dev Error +/- 1.2 feet 56 54 52 50 48 46 44 Well Locations Are Offset 150 feet for Each Compass Direction 42 40 42 44 46 48 50 52 54 Predicted B Cycle Thickness (feet) 56 Inferred Reservoir Properties from B Cycle Thickness • • • • Log Analysis – Porosity and Saturation Drill Stem Tests – Permeability and Oil Cut Production History – Oil Cut Thin B Cycle Wells Usually Have Poor Porosity and Permeability But High Oil-Cut • Thick B Cycle Wells Usually Have Thick Porosity and Low Oil-Cut Reservoir Properties with Depositional Setting More Lagoonal 1.0 2.00 0.9 1.80 Oil Cut Phi-h 0.8 1.60 0.7 1.40 Optimal Depositional Setting 0.6 0.5 1.20 1.00 0.4 0.80 0.3 0.60 0.2 0.40 ~So*phi-h (Moveable) 0.1 0.20 0.0 0.00 38 40 42 44 46 48 50 52 54 Red River B Cycle Thickness (Feet) 56 Pore Volume phi-h (Porosity-Feet) Producing Oil-Cut (Fraction) More Supra-tidal Producing Oil Cut from Structure 1.0 • Red River B Production Characteristics Are Also Affected by Structure • Height Above Regional Depth Trend Has High Correlation with Oil-Cut Producing Oil Cut (Fraction) 0.9 0.8 0.7 0.6 0.5 0.4 0.3 0.2 0.1 0.0 -80 -60 -40 -20 0 20 40 60 80 Height Above Critical Datum (Feet) 100 Producing Oil-Cut Transform Example Amor South Red River Unit Bowman County, ND One Mile • Map of Oil-Cut Transform from B Cycle Thickness and Height Above Regional Depth Trend • Map of Oil Saturation Can Be Inferred from Capillary Pressure Properties and OilCut • Map of Oil Pore-Volume Can Be Estimated from Average or Mapped PHI-H and Oil Saturation
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