FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2130893527> ?p ?o ?g. }

• W2130893527 endingPage "350" @default.
• W2130893527 startingPage "334" @default.
• W2130893527 abstract "Abstract The Anticosti Basin is a large Paleozoic basin in eastern Canada where potential source and reservoir rocks have been identified but no economic hydrocarbon reservoirs have been found. Potential source rocks of the Upper Ordovician Macasty Formation overlie carbonates of the Middle Ordovician Mingan Formation, which are underlain by dolostones of the Lower Ordovician Romaine Formation. These carbonates have been subjected to dissolution and dolomitization and are potential hydrocarbon reservoirs. Numerical simulations of fluid‐overpressure development related to sediment compaction and hydrocarbon generation were carried out to investigate whether hydrocarbons generated in the Macasty Formation could migrate downward into the underlying Mingan and Romaine formations. The modeling results indicate that, in the central part of the basin, maximum fluid overpressures developed above the Macasty Formation due to rapid sedimentation. This overpressured core dissipated gradually with time, but the overpressure pattern (i.e. maximum overpressure above source rock) was maintained during the generation of oil and gas. The downward impelling force associated with fluid‐overpressure gradients in the central part of the basin was stronger than the buoyancy force for oil, whereas the buoyancy force for gas and for oil generated in the later stage of the basin is stronger than the overpressure‐related force. Based on these results, it is proposed that oil generated from the Macasty Formation in the central part of the basin first moved downward into the Mingan and Romaine formations, and then migrated laterally up‐dip toward the basin margin, whereas gas throughout the basin and oil generated in the northern part of the basin generally moved upward. Consequently, gas reservoirs are predicted to occur in the upper part of the basin, whereas oil reservoirs are more likely to be found in the strata below the source rocks. Geofluids (2010) 10 , 334–350" @default.
• W2130893527 created "2016-06-24" @default.
• W2130893527 creator A5001444682 @default.
• W2130893527 creator A5021559920 @default.
• W2130893527 creator A5074036333 @default.
• W2130893527 creator A5086715266 @default.
• W2130893527 date "2010-08-01" @default.
• W2130893527 modified "2023-10-16" @default.
• W2130893527 title "Downward hydrocarbon migration predicted from numerical modeling of fluid overpressure in the Paleozoic Anticosti Basin, eastern Canada" @default.
• W2130893527 cites W1607305776 @default.
• W2130893527 cites W1969961393 @default.
• W2130893527 cites W1970719883 @default.
• W2130893527 cites W1971613502 @default.
• W2130893527 cites W1971985935 @default.
• W2130893527 cites W1973170581 @default.
• W2130893527 cites W1995269115 @default.
• W2130893527 cites W2004538472 @default.
• W2130893527 cites W2005937040 @default.
• W2130893527 cites W2006987817 @default.
• W2130893527 cites W2009022965 @default.
• W2130893527 cites W2025945545 @default.
• W2130893527 cites W2062090437 @default.
• W2130893527 cites W2075929381 @default.
• W2130893527 cites W2091414028 @default.
• W2130893527 cites W2095459281 @default.
• W2130893527 cites W2096064288 @default.
• W2130893527 cites W2106792405 @default.
• W2130893527 cites W2127133205 @default.
• W2130893527 cites W2134860114 @default.
• W2130893527 cites W2141104216 @default.
• W2130893527 cites W2157421823 @default.
• W2130893527 cites W2168052720 @default.
• W2130893527 cites W2168097570 @default.
• W2130893527 cites W2170384715 @default.
• W2130893527 cites W2227347199 @default.
• W2130893527 cites W2320725276 @default.
• W2130893527 cites W2333344449 @default.
• W2130893527 cites W2885006670 @default.
• W2130893527 cites W2909769950 @default.
• W2130893527 cites W2909949449 @default.
• W2130893527 cites W2910147669 @default.
• W2130893527 cites W2910522082 @default.
• W2130893527 cites W2910580050 @default.
• W2130893527 cites W2981897762 @default.
• W2130893527 cites W4240899137 @default.
• W2130893527 cites W4248392206 @default.
• W2130893527 cites W4302413624 @default.
• W2130893527 doi "https://doi.org/10.1111/j.1468-8123.2010.00280.x" @default.
• W2130893527 hasPublicationYear "2010" @default.
• W2130893527 type Work @default.
• W2130893527 sameAs 2130893527 @default.
• W2130893527 citedByCount "30" @default.
• W2130893527 countsByYear W21308935272012 @default.
• W2130893527 countsByYear W21308935272013 @default.
• W2130893527 countsByYear W21308935272014 @default.
• W2130893527 countsByYear W21308935272015 @default.
• W2130893527 countsByYear W21308935272016 @default.
• W2130893527 countsByYear W21308935272017 @default.
• W2130893527 countsByYear W21308935272018 @default.
• W2130893527 countsByYear W21308935272019 @default.
• W2130893527 countsByYear W21308935272020 @default.
• W2130893527 countsByYear W21308935272021 @default.
• W2130893527 countsByYear W21308935272022 @default.
• W2130893527 countsByYear W21308935272023 @default.
• W2130893527 crossrefType "journal-article" @default.
• W2130893527 hasAuthorship W2130893527A5001444682 @default.
• W2130893527 hasAuthorship W2130893527A5021559920 @default.
• W2130893527 hasAuthorship W2130893527A5074036333 @default.
• W2130893527 hasAuthorship W2130893527A5086715266 @default.
• W2130893527 hasBestOaLocation W21308935271 @default.
• W2130893527 hasConcept C109007969 @default.
• W2130893527 hasConcept C114793014 @default.
• W2130893527 hasConcept C121332964 @default.
• W2130893527 hasConcept C126559015 @default.
• W2130893527 hasConcept C127313418 @default.
• W2130893527 hasConcept C13106087 @default.
• W2130893527 hasConcept C146588470 @default.
• W2130893527 hasConcept C151730666 @default.
• W2130893527 hasConcept C17409809 @default.
• W2130893527 hasConcept C187930136 @default.
• W2130893527 hasConcept C29452850 @default.
• W2130893527 hasConcept C538625479 @default.
• W2130893527 hasConcept C5900021 @default.
• W2130893527 hasConcept C62520636 @default.
• W2130893527 hasConcept C63662990 @default.
• W2130893527 hasConcept C91442348 @default.
• W2130893527 hasConcept C97355855 @default.
• W2130893527 hasConceptScore W2130893527C109007969 @default.
• W2130893527 hasConceptScore W2130893527C114793014 @default.
• W2130893527 hasConceptScore W2130893527C121332964 @default.
• W2130893527 hasConceptScore W2130893527C126559015 @default.
• W2130893527 hasConceptScore W2130893527C127313418 @default.
• W2130893527 hasConceptScore W2130893527C13106087 @default.
• W2130893527 hasConceptScore W2130893527C146588470 @default.
• W2130893527 hasConceptScore W2130893527C151730666 @default.
• W2130893527 hasConceptScore W2130893527C17409809 @default.
• W2130893527 hasConceptScore W2130893527C187930136 @default.
• W2130893527 hasConceptScore W2130893527C29452850 @default.

• next