Regional-scale variation of characteristics of hydrocarbon fluid inclusions and thermal conditions along the Paleozoic Laurentian continental margin in eastern Quebec, Canada
Notice bibliographique
Résumé
Research Article| September 01, 2000 Regional-scale variation of characteristics of hydrocarbon fluid inclusions and thermal conditions along the Paleozoic Laurentian continental margin in eastern Quebec, Canada* G. Chi; G. Chi Geological Survey of Canada - Quebec Division, 880 chemin de Ste-Foy, bur. 840, Quebec, QC, G1S 2L2 Search for other works by this author on: GSW Google Scholar D. Lavoie; D. Lavoie Geological Survey of Canada - Quebec Division, 880 chemin de Ste-Foy, bur. 840, Quebec, QC, G1S 2L2 Search for other works by this author on: GSW Google Scholar R. Bertrand R. Bertrand INRS-Géoresources, 880 chemin de Ste-Foy, bur. 840, Quebec, QC, G1S 2L2 Search for other works by this author on: GSW Google Scholar Author and Article Information G. Chi Geological Survey of Canada - Quebec Division, 880 chemin de Ste-Foy, bur. 840, Quebec, QC, G1S 2L2 D. Lavoie Geological Survey of Canada - Quebec Division, 880 chemin de Ste-Foy, bur. 840, Quebec, QC, G1S 2L2 R. Bertrand INRS-Géoresources, 880 chemin de Ste-Foy, bur. 840, Quebec, QC, G1S 2L2 Publisher: Canadian Society of Petroleum Geologists Received: 08 Sep 1999 Accepted: 29 Feb 2000 First Online: 02 Mar 2017 Online ISSN: 2368-0261 Print ISSN: 0007-4802 © The Society of Canadian Petroleum Geologists Bulletin of Canadian Petroleum Geology (2000) 48 (3): 193–211. https://doi.org/10.2113/48.3.193 Article history Received: 08 Sep 1999 Accepted: 29 Feb 2000 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 G. Chi, D. Lavoie, R. Bertrand; Regional-scale variation of characteristics of hydrocarbon fluid inclusions and thermal conditions along the Paleozoic Laurentian continental margin in eastern Quebec, Canada. Bulletin of Canadian Petroleum Geology 2000;; 48 (3): 193–211. doi: https://doi.org/10.2113/48.3.193 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 Fluid inclusions in diagenetic mineral phases and organic matter in host rocks were studied in Paleozoic strata along the Laurentian continental margin in eastern Quebec. The types of hydrocarbon fluid inclusions correspond broadly with the tectonic units: the St. Lawrence Platform contains oil inclusions; the Humber Zone contains mainly methane inclusions; and the successor basin (the Gaspé Belt) contains oil inclusions in the upper succession, oil and methane in the middle succession, and methane inclusions in the lower interval. The nature of hydrocarbon fluid inclusions also corresponds to the maturation level of organic matter in the host rocks: oil inclusions occur in host rocks that were heated to the oil window or the condensate zone, whereas methane inclusions occur in the condensate zone or dry gas zone, but mainly in the latter. The variation in the nature of hydrocarbon fluid inclusions is related to the thermal history of the successions studied: oil inclusions correspond to relatively low thermal conditions, and methane inclusions to relatively high conditions. These observations suggest that oil reservoirs, if they exist, are more likely to occur in host rocks that have not been buried beyond the condensate zone than in those that have gone through the dry gas zone. The occurrence of oil inclusions in condensate zone rocks suggests that oil was generated and migrated after maximum burial of the host rocks, from mature source rocks either overlying or overthrusted by the host rocks. However, the absence of oil inclusions in the dry gas zone rocks suggests that such a late oil generation-migration scenario may not be viable if the host rocks are heated far beyond the oil window. This is probably because these rocks are farther from, thus less likely connected to, a younger source rock. This study suggests that part of the St. Lawrence Platform and the Gaspé Belt have the thermal conditions for the formation of oil reservoirs, whereas the Humber Zone is prone to natural gas formation. 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 ».