Geologic Framework

Geologic Framework

STRUCTURAL COMPARTMENTALIZATION AT CAVE GULCH FIELD, WIND RIVER BASIN, WYOMING by Kimberly Hélène Doupé A thesis submitted to the faculty and Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology) Golden, Colorado Date ___________ Signed: _____________________ Kimberly H. Doupé Approved: ___________________ Dr. Neil F. Hurley Thesis Advisor Golden, Colorado Date ___________ _______________________ Dr. Murray W. Hitzman Professor and Head, Department of Geology and Geological Engineering ii ABSTRACT Cave Gulch field is located in the Wind River basin, Natrona County, Wyoming. The field has an estimated recovery of 600 billion cubic feet (BCF) of gas from sandstones of the Paleocene Fort Union (thickness = 1,500 ft, 457 m), and Upper Cretaceous Lance (thickness = 2,500 ft, 762 m), Meeteetse (thickness = 1,500 ft, 457 m), and Mesaverde (thickness = 2,000 ft, 610 m) Formations. Cave Gulch field is a structurally complex reservoir due its origin as a faulted anticline that lies in the footwall of the Owl Creek thrust (18,000 ft, 5,486 m in vertical offset). The purpose of this study is to determine the depths of subseismic-scale faults in wells with borehole image logs, and to calculate the size of fault-bounded compartments based upon a 3D stochastic model. Formation MicroImager (FMI) logs covering 62,000 ft (18,898 m) of vertical section are available in 11 wells in Cave Gulch field. These logs were interpreted for bed boundaries, fractures and microfaults. Bed boundaries in interbedded shales were used to create cumulative dip, dip azimuth vector, and statistical curvature analysis technique (SCAT) plots. Inflection points on these plots are interpreted as subseismic-scale faults. 320 subseismic-scale faults were identified from 11 FMI logs, with an average of 3.9 faults per 1,000 ft (304 m) of vertical log depth. iii Published structure maps of the top of the Lance and Meeteetse Formations were digitized and used to build a 3D geologic model. This model includes 3 deterministic seismic-scale faults. Subseismic-scale faults were generated using a grid-based fracture generator within 3D Move software. The model was constructed based on microfault orientations interpreted from FMI logs, and the depths to subseismic-scale faults interpreted from dip-domain analysis of FMI data. After subseismic-scale faults were generated, a horizontal plane was cut through the model at the middle of the Lance Formation. For the purpose of this study, subseismic-scale faults were assumed to be no- flow boundaries. Area sizes for fault-bounded compartments ranged from <1 to 387 ac (<0.004 to 1.6 km2). Well spacing templates of 5, 10, 20, 40, 80, and 160 ac (0.02, 0.04, 0.08, 0.16, 0.32, and 0.65 km2) were superimposed on the model to determine the drainage efficiency of various infill-drilling programs. Comparison of compartment size with ideal well spacing has identified the most efficient development strategy. A well spacing of 30 ac (0.12 km2) is recommended, with a closer spacing (5 ac, 0.02 km2) needed in proximity to seismic-scale faults. This study does not address stratigraphic compartmentalization, which adds another layer of complexity because of the abundance of stacked fluvial sandstones in the reservoir. iv TABLE OF CONTENTS Page ABSTRACT ...................................................................................................................... iii LIST OF FIGURES ......................................................................................................... viii LIST OF TABLES........................................................................................................... xiv ACKNOWLEDGEMENTS...............................................................................................xv CHAPTER 1 Introduction ...................................................................................................1 1.1 Introduction....................................................................................................... 1 1.2 Purpose of Study............................................................................................... 4 1.3 Research Contributions..................................................................................... 5 CHAPTER 2 Geologic Framework.....................................................................................7 2.1 Location of Study Area..................................................................................... 7 2.2 Stratigraphy....................................................................................................... 9 2.2.1 Regional Stratigraphy ........................................................................ 9 2.2.2 Local Stratigraphy............................................................................ 16 2.3 Structural Geology.......................................................................................... 23 2.3.1 Regional Tectonics........................................................................... 23 2.3.2 Regional Structure ........................................................................... 31 2.3.3 Local Structure................................................................................. 36 2.4 History of Field............................................................................................... 40 CHAPTER 3 Analysis and Interpretationof Borehole Image Logs...................................48 3.1 Borehole Images ............................................................................................. 48 3.2 Data Available ................................................................................................ 53 3.3 Borehole Image Log Processing..................................................................... 53 3.4 Methods of Borehole Image Log Interpretation ............................................. 56 3.4.1 Fracture and Microfault Interpretation............................................. 60 3.4.2 Quality of Borehole Images............................................................. 62 3.4.3 Dips.................................................................................................. 65 v 3.4.3 Cumulative Dip Plots....................................................................... 72 3.4.5 Dip Azimuth Vector Plots................................................................ 73 3.4.6 SCAT Plots ...................................................................................... 73 3.5 Results............................................................................................................. 74 3.5.1 Structural Analysis........................................................................... 76 3.5.2 Fractures and Microfaults ................................................................ 81 3.5.3 Fault Drag ...................................................................................... 106 3.6 Discussion..................................................................................................... 106 3.6.1 Pitfalls and Assumptions................................................................ 108 3.6.2 Discussion of Results..................................................................... 109 3.6.3 Dip Domains .................................................................................. 109 3.6.4 Fractures and Microfaults .............................................................. 111 3.6.5 Subseismic-Scale Faults................................................................. 113 CHAPTER 4 Integrated Analysis....................................................................................115 4.1 Introduction................................................................................................... 115 4.2 Data Available .............................................................................................. 115 4.3 3-D Seismic Data .......................................................................................... 117 4.4 Production Data ............................................................................................ 122 4.5 Discussion..................................................................................................... 131 CHAPTER 5 3-D Fault Model ........................................................................................135 5.1 Introduction................................................................................................... 135 5.2 Data Available .............................................................................................. 135 5.3 Methods: Building the Model ....................................................................... 137 5.3.1 Discrete Faults for the Background Model.................................... 141 5.3.2 Discrete Faults for the Fault-Proximal Model ............................... 149 5.4 Results........................................................................................................... 151 5.4.1 Results for the Background Model ................................................ 154 5.4.2 Results for the Fault-Proximal Model............................................ 164 5.5 Discussion..................................................................................................... 173 5.5.1 Parameters...................................................................................... 173 5.5.2 Assumptions..................................................................................

View Full Text

Details

  • File Type
    pdf
  • Upload Time
    -
  • Content Languages
    English
  • Upload User
    Anonymous/Not logged-in
  • File Pages
    97 Page
  • File Size
    -

Download

Channel Download Status
Express Download Enable

Copyright

We respect the copyrights and intellectual property rights of all users. All uploaded documents are either original works of the uploader or authorized works of the rightful owners.

  • Not to be reproduced or distributed without explicit permission.
  • Not used for commercial purposes outside of approved use cases.
  • Not used to infringe on the rights of the original creators.
  • If you believe any content infringes your copyright, please contact us immediately.

Support

For help with questions, suggestions, or problems, please contact us