Sedimentology and stratigraphy of a thick, areally extensive fluvial-marine transition, Missisauga Formation, offshore Nova Scotia, and its correlation with shelf margin and slope strata
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Résumé
Research Article| June 01, 2006 Sedimentology and stratigraphy of a thick, areally extensive fluvial–marine transition, Missisauga Formation, offshore Nova Scotia, and its correlation with shelf margin and slope strata Don I. Cummings; Don I. Cummings Department of Earth Sciences, University of Ottawa, Ottawa, ON K1N 6N5, cummings@geol.queensu.ca 1Current address: Department of Geological Sciences and Geological Engineering, Queen’s University, Kingston, Ontario. Search for other works by this author on: GSW Google Scholar Bruce S. Hart; Bruce S. Hart Department of Earth and Planetary Sciences, McGill University, Montreal, Quebec H3A 2A7 Search for other works by this author on: GSW Google Scholar R. William C. Arnott R. William C. Arnott Department of Earth Sciences, University of Ottawa, Ottawa, ON K1N 6N5 Search for other works by this author on: GSW Google Scholar Author and Article Information Don I. Cummings 1Current address: Department of Geological Sciences and Geological Engineering, Queen’s University, Kingston, Ontario. Department of Earth Sciences, University of Ottawa, Ottawa, ON K1N 6N5, cummings@geol.queensu.ca Bruce S. Hart Department of Earth and Planetary Sciences, McGill University, Montreal, Quebec H3A 2A7 R. William C. Arnott Department of Earth Sciences, University of Ottawa, Ottawa, ON K1N 6N5 Publisher: Canadian Society of Petroleum Geologists Received: 11 May 2005 Accepted: 05 Apr 2006 First Online: 02 Mar 2017 Online ISSN: 2368-0261 Print ISSN: 0007-4802 © The Society of Canadian Petroleum Geologists Bulletin of Canadian Petroleum Geology (2006) 54 (2): 152–174. https://doi.org/10.2113/gscpgbull.54.2.152 Article history Received: 11 May 2005 Accepted: 05 Apr 2006 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Don I. Cummings, Bruce S. Hart, R. William C. Arnott; Sedimentology and stratigraphy of a thick, areally extensive fluvial–marine transition, Missisauga Formation, offshore Nova Scotia, and its correlation with shelf margin and slope strata. Bulletin of Canadian Petroleum Geology 2006;; 54 (2): 152–174. doi: https://doi.org/10.2113/gscpgbull.54.2.152 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyBulletin of Canadian Petroleum Geology Search Advanced Search Abstract A 100 m thick, more than 20 km wide upward-fining succession at the top of the Lower Cretaceous Upper Member of the Missisauga Formation was investigated in the Panuke Field, offshore Nova Scotia, using core, well logs and 3-D seismic data. The succession consists of 50 m of dune cross-stratified sandstone overlain by 50 m of tide-influenced heterolithic strata, which in turn is overlain by 150 m of mudstone of the Naskapi Member of the Logan Canyon Formation. The succession is interpreted to be a fluvial–marine transition formed during a long-term (3rd order) relative sea-level rise. The two main Panuke reservoirs are thin (<5 m) sheet-like sandstones at the Missisauga–Naskapi contact interpreted to be remnants of a wave-formed barrier system. In seismic data, the Upper Member of the Missisauga Formation correlates basinward with progradational shelf-margin reflections, suggesting that the sheet-like fluvial sandstone at the base of the upward-fining succession transferred sediment, and possibly sand, to the continental slope. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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 | 0,000 |
| Science ouverte | 0,000 | 0,000 |
| Intégrité de la recherche | 0,000 | 0,000 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,002 | 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 ».