Reservoir characterization of channel-belt strata, McMurray Formation, northeastern Alberta

dc.contributor.advisorHubbard, Stephen M.
dc.contributor.authorCurkan, Jordan Anne
dc.contributor.committeememberLeckie, Dale A.
dc.contributor.committeememberGates, Ian Donald
dc.contributor.committeememberQuinney, Annie E.
dc.date2020-11
dc.date.accessioned2020-08-27T14:57:47Z
dc.date.available2020-08-27T14:57:47Z
dc.date.issued2020-08-25
dc.description.abstractThe reconstruction of stacked channel-belt strata provides important insights into the heterogeneity that results from fluvial depositional processes over a range of spatial and temporal scales. The Lower Cretaceous McMurray Formation of northeastern Alberta represents one of the world’s most significant bitumen reserves, which is hosted in part, within fluvial strata. An extensive subsurface dataset, including production data, is used in this study to characterize stacked channel-belt deposits and demonstrate the impact of numerous scales of heterogeneity on reservoir quality and performance. Bed- through bar- and channel-belt-scale investigations of the McMurray Formation are numerous, however almost all previous studies have overlooked the impact of vertically stacked meander-belt deposits on heterogeneity delineation and production performance. This is a consequence of the difficulty in readily mapping older channel-belt units, which are partially eroded and unresolvable in seismic data. In this study, the delineation of channel-belt remnants that persist beneath the youngest, seismically-defined fluvial system, is achieved. A novel approach to mapping these units relies on: (1) correlating a recently-refined stratigraphic framework into the study area, and in particular, beneath the well-characterized upper channel-belt strata; (2) fine-scale focus of underlying units to define criteria to distinguish vertically stacked channel-belts, including changes in facies, bioturbation type and intensity, sandstone content, grain size, and dip azimuth of dipping strata, which help to define belt boundaries; and (3) the use of preserved parasequence elevations in combination with sub-Cretaceous unconformity paleotopographic elevations, which help identify restricted areas of potential channel-belt development at each stratigraphic level. We show that heterogeneous boundaries between belts, as well as differing stratigraphic architecture amongst successive channel systems, significantly impacts production performance. It is clear that detailed characterization of stacked channel-belt strata at the outset of a project could have a profound impact on their performance and long-term viability.en_US
dc.identifier.citationCurkan, J. A. (2020). Reservoir characterization of channel-belt strata, McMurray Formation, northeastern Alberta (Master's thesis, University of Calgary, Calgary, Canada). Retrieved from https://prism.ucalgary.ca.
dc.identifier.doihttp://dx.doi.org/10.11575/PRISM/38115
dc.identifier.urihttp://hdl.handle.net/1880/112433
dc.language.isoeng
dc.publisher.facultyScience
dc.publisher.institutionUniversity of Calgaryen
dc.rightsUniversity of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.en_US
dc.subjectMcMurray Formationen_US
dc.subjectStratigraphyen_US
dc.subjectOil Sandsen_US
dc.subjectStacked channel-belten_US
dc.subject.classificationEducation--Sciencesen_US
dc.subject.classificationGeologyen_US
dc.titleReservoir characterization of channel-belt strata, McMurray Formation, northeastern Albertaen_US
dc.typemaster thesisen_US
thesis.degree.disciplineGeoscienceen_US
thesis.degree.grantorUniversity of Calgaryen_US
thesis.degree.nameMaster of Science (MSc)en_US
ucalgary.item.requestcopytrue

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