S
Stephen M. Hubbard
Researcher at University of Calgary
Publications - 118
Citations - 4116
Stephen M. Hubbard is an academic researcher from University of Calgary. The author has contributed to research in topics: Foreland basin & Outcrop. The author has an hindex of 35, co-authored 107 publications receiving 3353 citations. Previous affiliations of Stephen M. Hubbard include University of Alberta & Stanford University.
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Seismic geomorphology and sedimentology of a tidally influenced river deposit, Lower Cretaceous Athabasca oil sands, Alberta, Canada
Stephen M. Hubbard,Derald G. Smith,Haley Nielsen,Dale A. Leckie,Milovan Fustic,Ronald J. Spencer,Lorraine Bloom +6 more
TL;DR: In this paper, seismic reflection data and extensive drill cores from acreage located approximately 50 km (31 mi) south of Fort McMurray provide important insights into the sedimentologic organization of reservoir and non-reservoir deposits in the upper one third of the reservoir interval.
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Assessment of widely used methods to derive depositional ages from detrital zircon populations
TL;DR: In this article, the impact of sample size and calculation method on the accuracy of a resulting maximum depositional age (MDA) has been evaluated using large populations of synthetic zircon dates.
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Counter point bar deposits: lithofacies and reservoir significance in the meandering modern Peace River and ancient McMurray Formation, Alberta, Canada
TL;DR: Counter point bar deposits in the meandering Peace River, North-central Alberta, Wood Buffalo National Park, are distinct from point bars interms of morphology, lithofacies and reservoir potential for fluids as mentioned in this paper.
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Deep-Water Sediment Bypass
Christopher J. Stevenson,Christopher A.-L. Jackson,David M. Hodgson,Stephen M. Hubbard,Joris T. Eggenhuisen +4 more
TL;DR: In this paper, a suite of criteria are established to recognize bypass in the geological record from field data, each of which is associated with a set of diagnostic criteria: slope-channel bypass, slope-bypass from mass wasting events, base-of-slope bypass, and basin-floor bypass.
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Deep‐water foreland basin deposits of the Cerro Toro Formation, Magallanes basin, Chile: architectural elements of a sinuous basin axial channel belt
TL;DR: The Lago Sofia Member of the Cerro Toro Formation in the Cordillera Manuel Senoret, southern Chile, represents the deposits of a major channel belt (4 to 8 km wide by >100 km long) that occupied the foredeep of the Magallanes basin during the Late Cretaceous.