Paleodepositional Environments and Stratigraphic Framework for the Lower Cretaceous Bluesky Formation and Related Strata in the Peace River Oil Sands Deposit of Alberta
Notice bibliographique
Résumé
The Early Cretaceous Bluesky Formation in the Peace River oil sands area of west-central Alberta, Canada hosts significant bitumen resources. This work is part of an ongoing endeavour by researchers and practitioners in academia and industry to develop paleodepositional and sequence stratigraphic models for the Bluesky Formation and related deposits of the underlying Gething Formation and the overlying Wilrich Member. In this thesis, sedimentological, ichnological, and micropaleontological datasets are acquired from core, and paleodepositional interpretations for the formations of interest are made. Sediments in the upper Gething Formation preserve remnants of brackish bay and paralic swamp and marsh deposits. The Bluesky Formation is described by thirteen facies. Recurring succession of these facies are grouped into six facies associations representing both proximal and distal marginal marine environments and include: 1) fluvial- to wave-influenced distributary channel and terminal mouth bars, 2) mixed-influence proximal delta fronts, 3) wave- and storm-influenced, proximal to distal delta fronts, 4) wave-influenced delta fronts and shoreface environments, 5) lower bay shoreface to distal bay settings, and 6) tidal flats. Wilrich Member successions are represented by a Glossifungites-demarcated discontinuity and marine mudstones. These depositional environments are linked spatially and temporally by important sequence stratigraphic surfaces that formed during a series of regressive and transgressive events. Bluesky successions were deposited at fourth- or fifth-order scales and formed within the longer duration third-order phase of sea-level rise in the Early Cretaceous. Importantly, relative sea-level rise was episodic. During stillstand episodes of transgression, Bluesky progradation ensued. Regressive surfaces of marine and fluvial erosion mark these retrogradational episodes. Cross-section analysis reveals an apparent backstepping of the Bluesky Formation in the region as transgression proceeded. These progradational pulses were interrupted by high-order flooding events that are correlatable across the study area. Complete inundation of the study area by the Boreal Sea is marked by a third-order major flooding surface and is represented by transgressive Wilrich Member deposits. In addition to building a depositional model for the study area and understanding the paleoenvironmental evolution of the area in terms of sequence stratigraphic events, a number of complimentary studies are conducted. One particular study focuses on a facies that preserves world-class specimens of stacked Rosselia, which formed when burrowing tracemakers vertically re-adjusted their positions in the sediment following depositional events. Where present, these traces help to refine paleoenvironmental interpretations and can be used as proxies for assessing the magnitude and frequency of depositional events. The use of Rosselia illustrates a method of evaluating sedimentation events within a brief temporal window, one lying beyond the resolution of more traditional dating methods. The second study considers palynomorphs and microfossils preserved in cored intervals. The micropaleontological assemblages are calibrated with sedimentological and ichnological features to fine-tune depositional interpretations. Foraminifera and microfossils provide semi-quantitative paleosalinity ranges for the various depositional environments preserved in cored successions. Dinoflagellate cysts are used to identify important stratigraphic boundaries between Gething, Bluesky, and Wilrich sediments and to constrain the age of the Bluesky Formation to Early Aptian, an age older than previously recorded.
Récupéré en direct depuis OpenAlex et désinversé. Les résumés ne sont pas conservés dans cette base de données : les index inversés représentent 8,6 Go des 9,3 Go de texte de la base, et le serveur dispose de 13 Go libres.
Comment cette classification a été obtenuedéplier
Prédiction distillée sur la base complète
Imitation des enseignantsNi prévalence calibrée, ni vérité terrain. Validation humaine à venir. Apprise à partir de 10 348 étiquettes directes de Codex et de 10 348 étiquettes directes de Gemma. Le mode candidate est l'union des têtes enseignantes seuillées; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont ni des étiquettes humaines ni des étiquettes directes de modèles de pointe.
Scores Codex et Gemma par catégorie
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,000 | 0,000 |
| Méta-épidémiologie (sens strict) | 0,000 | 0,000 |
| Méta-épidémiologie (sens large) | 0,000 | 0,000 |
| Bibliométrie | 0,000 | 0,000 |
| Études des sciences et des technologies | 0,000 | 0,000 |
| Communication savante | 0,000 | 0,001 |
| Science ouverte | 0,000 | 0,000 |
| Intégrité de la recherche | 0,000 | 0,000 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,000 | 0,000 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découleClassification
machine, non validéePrédiction automatique; un appel candidat d’une seule tête enseignante, pas un consensus.
Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».