Evolution of a stratigraphic model in a fluvial deltaic wedge: implications for groundwater resource protection in an oil and gas-bearing region in the Upper Cretaceous Dunvegan Formation, Northwest Territories, Canada

Author:

Glas Nathan H.12ORCID,Bhattacharya Janok P.34,Steelman Colby M.125,Munn Jonathan D.12,Pierce Amanda A.12,Parker Beth L.12ORCID

Affiliation:

1. Morwick G360 Groundwater Research Institute, College of Engineering and Physical Sciences, School of Engineering, University of Guelph, Guelph, ON, N1G 2W1, Canada

2. School of Engineering, N1G 2W1, University of Guelph, Guelph, ON, Canada

3. Quantitative Sedimentology Laboratories, McMaster University, Hamilton, ON, L8S 4K1, Canada

4. School of Earth, Environment and Society, McMaster University, Hamilton, ON, L8S 4K1, Canada

5. Department of Earth and Environmental Sciences, niversity of Waterloo, Waterloo, ON, N2L 3G1, Canada

Abstract

The Liard Basin, in northwestern Canada, contains one of Canada’s largest natural gas reserves. There are concerns about degradation of Dunvegan Formation groundwater quality, which is the basin's main shallow freshwater aquifer, as a consequence of oil and gas development. Previous lithostratigraphic studies interpreted the Dunvegan as conglomeratic alluvial fans. In this study, newly collected cores and surface resistivity surveys are integrated with legacy hydrocarbon well data and measured sections for improved sedimentary bedrock characterization. Rather than alluvial fans, we interpret the upper Dunvegan as a coarse-sand to gravel bed fluvial system that was likely tributive to incised valleys associated with linked Alberta Basin base-level falls. Correlation of well logs and measured sections suggest the lower Dunvegan comprises a prograding delta complex with off-lapping clinoforms fed by smaller sand-bed rivers that grade into the upper Dunvegan conglomeratic system, which built southeast towards the Cretaceous Western Interior Seaway. This sequence stratigraphic and facies architectural approach is employed to inform the aquifer–aquitard flow system and aid in understanding the 3D groundwater flow system, once hydrogeologic characterisation confirms position and thickness of important hydrogeologic units. Resistivity surveys suggest upper Dunvegan channel-belt facies may be well-connected and laterally extensive, potentially acting as interconnected aquifer units; whereas lower Dunvegan channel belts may be discontinuous, indicating smaller-scale flow units separated by floodplain and marine shale. This revised geologic understanding provides opportunities for determining impacts or resilience from shallow and deep sources of contamination associated with human activities, including oil and gas development, land-use, and (or) climate change.

Publisher

Canadian Science Publishing

Subject

General Earth and Planetary Sciences

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