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Sedimentology of the Charlie Lake Formation

  • Author / Creator
    Fefchak, Chelsea
  • The Carnian Charlie Lake Formation is a hydrocarbon bearing formation found predominantly in northeastern British Columbia, Canada. Aeolian sand bodies are present in both the subsurface and outcrop occurrences, and in fields like Brassey, are the primary hydrocarbon reservoir. For this study, 2 outcrop occurrences of Charlie Lake Formation in its entirety (Brown Hill and Schooler Creek) and a case study on the Artex member sandstone involving 15 cores from Brassey Field were evaluated. Although non-correlatable, the relationships between the outcrop and subsurface Charlie Lake Formation were assessed and, show similar preservation of the coastal dune bodies, related to deposition in shore-parallel depressions that were initiated as lagoons or lakes. Consequently, it is proposed that preserved aeolian dune thickness is directly related to lagoon / lake depth, which in turn is likely related to local tidal regime.

  • Subjects / Keywords
  • Graduation date
    2011-11
  • Type of Item
    Thesis
  • Degree
    Master of Science
  • DOI
    https://doi.org/10.7939/R3203M
  • License
    This thesis is made available by the University of Alberta Libraries with permission of the copyright owner solely for non-commercial purposes. This thesis, or any portion thereof, may not otherwise be copied or reproduced without the written consent of the copyright owner, except to the extent permitted by Canadian copyright law.
  • Language
    English
  • Institution
    University of Alberta
  • Degree level
    Master's
  • Department
    • Department of Earth and Atmospheric Sciences
  • Supervisor / co-supervisor and their department(s)
    • Dr. John-Paul Zonneveld (Earth and Atmospheric Sciences)
  • Examining committee members and their departments
    • Dr. Murray Gingras (Earth and Atmospheric Sciences)
    • Dr. Heather Proctor (Biological Science)
    • Dr. S. George Pemberton (Earth and Atmospheric Sciences)