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Bergen, Anika Arnott, Robert 2017-07-24T15:21:20Z 2017-07-24T15:21:20Z 2017 http://hdl.handle.net/10393/36434 http://dx.doi.org/10.20381/ruor-20714 At the Castle Creek study area, levee deposits are well-exposed over an area of ~2.6 km wide and ~90 m thick. This provides an opportunity to describe their lateral and vertical lithological changes, and accordingly details about their reservoir geometry and stratal continuity. Here, levee deposits are divided vertically into packages, each consisting of a sand-rich lower part overlain sharply by a mud-rich upper part. Each lower part displays a consistent thickening then thinning trend laterally away from its genetically related channel. The characteristics of these packages suggest that they were controlled by recurring changes in the structure of channellized flows, which in turn was controlled by grain size and grain sorting. This ultimately was controlled by short-term changes in relative sea level. Moreover, some mud- and sand-rich strata are rich in residual carbon suggesting that mid-fan levees can serve as source rocks for hydrocarbon generation, and also reservoirs. en Université d'Ottawa / University of Ottawa sedimentology stratigraphy total organic carbon deep marine levee deposits Windermere Supergroup deep marine channel deposits Vertical and Lateral Facies Architecture of Levees and Their Genetically-Related Channels, Isaac Formation, Neoproterozoic Windermere Supergroup, Cariboo Mountains, B.C. Thesis MSc Masters Sciences / Science Sciences de la Terre et de l'environnement / Earth and Environmental Sciences open.access