Baltimore Canyon untested gas potential
Abstract Hydrocarbon exploration in the Baltimore Canyon during the 1980’s targeted Upper Jurassic and younger elastics and carbonates in stratigraphic traps consisting of possibly erosionally enhanced mounds and pinnacles. Five wells encountered hydrocarbons with cumulative flow rates testing 90 mm...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Epstein, Samuel Abraham [verfasserIn] |
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| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2009 |
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| Schlagwörter: |
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| Anmerkung: |
© Northeasten Science Foundation 2009 |
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| Übergeordnetes Werk: |
Enthalten in: Carbonates and evaporites - Springer-Verlag, 1986, 24(2009), 1 vom: Jan., Seite 58-76 |
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| Übergeordnetes Werk: |
volume:24 ; year:2009 ; number:1 ; month:01 ; pages:58-76 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF03228057 |
|---|
| Katalog-ID: |
OLC2076499822 |
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| 520 | |a Abstract Hydrocarbon exploration in the Baltimore Canyon during the 1980’s targeted Upper Jurassic and younger elastics and carbonates in stratigraphic traps consisting of possibly erosionally enhanced mounds and pinnacles. Five wells encountered hydrocarbons with cumulative flow rates testing 90 mm cfg/d. Apparent discontinuity in reservoir extent resulted in project abandonment. Highly mature, organic source rocks in this area were not identified. A recent organic reinterpretation of gas condensates from the Hudson Canyon suggests a deeper Lower Jurassic source, analogous to that of the U.S. Gulf Coast’s Smackover Formation, Late Jurassic in age. The Houston Oil Minerals 676 Well encountered salt at a depth of 3,800 meters on the eastern flank of the Schlee Dome. Reprocessed seismic data (AVO Analysis) indicate reflectors typical of widespread salt layers deposited during the Early Jurassic (60 m thick and 25 km wide) suggesting arid and restricted (anoxic) depositional climatic conditions in the Early Jurassic. Impermeable evaporites and shales, between the Lower and Upper Jurassic, may provide excellent seals explaining the lack of significant migration of hydrocarbons into porous rocks of the Upper Jurassic and Cretaceous. The Gulf Coast Smackover may be an excellent analog for this area. The Red Sea-Dead Sea-Sea of Galilee rift zone may be an important modern analog for the Baltimore Canyon Trough. Carbonates in this area have porosities that range between 30% and 60% permeabilities that range between 0.01 and 10,000 millidarcys. The thermal maturation profile (based on the Shell 273-1 well) for the Baltimore Canyon Trough indicates that Jurassic age sediments entered the early oil phase at a depth of approximately 2500 m and the main gas generation window at a depth of 5000 m. Gas generation in Early to Middle Jurassic sediments started in the Late Jurassic and continued through the Tertiary. Sediments younger than the Early Cretaceous are not thermally mature. A new exploration strategy should focus on deeper sections of the Lower and Middle Jurassic, at depths much greater than previously drilled. Drilling should be significant distances from igneous emplacements, which may have breached upper reservoir seals. Reservoirs should be in carbonates and shelf elastics. An isopach map of the Baltimore Canyon Trough indicates that a significant area of Jurassic Age sediments, greater than 6 km thick, is buried to depths of mature hydrocarbon generation. | ||
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10.1007/BF03228057 doi (DE-627)OLC2076499822 (DE-He213)BF03228057-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Epstein, Samuel Abraham verfasserin aut Baltimore Canyon untested gas potential 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Northeasten Science Foundation 2009 Abstract Hydrocarbon exploration in the Baltimore Canyon during the 1980’s targeted Upper Jurassic and younger elastics and carbonates in stratigraphic traps consisting of possibly erosionally enhanced mounds and pinnacles. Five wells encountered hydrocarbons with cumulative flow rates testing 90 mm cfg/d. Apparent discontinuity in reservoir extent resulted in project abandonment. Highly mature, organic source rocks in this area were not identified. A recent organic reinterpretation of gas condensates from the Hudson Canyon suggests a deeper Lower Jurassic source, analogous to that of the U.S. Gulf Coast’s Smackover Formation, Late Jurassic in age. The Houston Oil Minerals 676 Well encountered salt at a depth of 3,800 meters on the eastern flank of the Schlee Dome. Reprocessed seismic data (AVO Analysis) indicate reflectors typical of widespread salt layers deposited during the Early Jurassic (60 m thick and 25 km wide) suggesting arid and restricted (anoxic) depositional climatic conditions in the Early Jurassic. Impermeable evaporites and shales, between the Lower and Upper Jurassic, may provide excellent seals explaining the lack of significant migration of hydrocarbons into porous rocks of the Upper Jurassic and Cretaceous. The Gulf Coast Smackover may be an excellent analog for this area. The Red Sea-Dead Sea-Sea of Galilee rift zone may be an important modern analog for the Baltimore Canyon Trough. Carbonates in this area have porosities that range between 30% and 60% permeabilities that range between 0.01 and 10,000 millidarcys. The thermal maturation profile (based on the Shell 273-1 well) for the Baltimore Canyon Trough indicates that Jurassic age sediments entered the early oil phase at a depth of approximately 2500 m and the main gas generation window at a depth of 5000 m. Gas generation in Early to Middle Jurassic sediments started in the Late Jurassic and continued through the Tertiary. Sediments younger than the Early Cretaceous are not thermally mature. A new exploration strategy should focus on deeper sections of the Lower and Middle Jurassic, at depths much greater than previously drilled. Drilling should be significant distances from igneous emplacements, which may have breached upper reservoir seals. Reservoirs should be in carbonates and shelf elastics. An isopach map of the Baltimore Canyon Trough indicates that a significant area of Jurassic Age sediments, greater than 6 km thick, is buried to depths of mature hydrocarbon generation. Jurassic Source Rock Late Jurassic Middle Jurassic Callovian Clark, Donald aut Enthalten in Carbonates and evaporites Springer-Verlag, 1986 24(2009), 1 vom: Jan., Seite 58-76 (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:24 year:2009 number:1 month:01 pages:58-76 https://doi.org/10.1007/BF03228057 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_381 GBV_ILN_2027 GBV_ILN_4112 GBV_ILN_4309 AR 24 2009 1 01 58-76 |
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10.1007/BF03228057 doi (DE-627)OLC2076499822 (DE-He213)BF03228057-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Epstein, Samuel Abraham verfasserin aut Baltimore Canyon untested gas potential 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Northeasten Science Foundation 2009 Abstract Hydrocarbon exploration in the Baltimore Canyon during the 1980’s targeted Upper Jurassic and younger elastics and carbonates in stratigraphic traps consisting of possibly erosionally enhanced mounds and pinnacles. Five wells encountered hydrocarbons with cumulative flow rates testing 90 mm cfg/d. Apparent discontinuity in reservoir extent resulted in project abandonment. Highly mature, organic source rocks in this area were not identified. A recent organic reinterpretation of gas condensates from the Hudson Canyon suggests a deeper Lower Jurassic source, analogous to that of the U.S. Gulf Coast’s Smackover Formation, Late Jurassic in age. The Houston Oil Minerals 676 Well encountered salt at a depth of 3,800 meters on the eastern flank of the Schlee Dome. Reprocessed seismic data (AVO Analysis) indicate reflectors typical of widespread salt layers deposited during the Early Jurassic (60 m thick and 25 km wide) suggesting arid and restricted (anoxic) depositional climatic conditions in the Early Jurassic. Impermeable evaporites and shales, between the Lower and Upper Jurassic, may provide excellent seals explaining the lack of significant migration of hydrocarbons into porous rocks of the Upper Jurassic and Cretaceous. The Gulf Coast Smackover may be an excellent analog for this area. The Red Sea-Dead Sea-Sea of Galilee rift zone may be an important modern analog for the Baltimore Canyon Trough. Carbonates in this area have porosities that range between 30% and 60% permeabilities that range between 0.01 and 10,000 millidarcys. The thermal maturation profile (based on the Shell 273-1 well) for the Baltimore Canyon Trough indicates that Jurassic age sediments entered the early oil phase at a depth of approximately 2500 m and the main gas generation window at a depth of 5000 m. Gas generation in Early to Middle Jurassic sediments started in the Late Jurassic and continued through the Tertiary. Sediments younger than the Early Cretaceous are not thermally mature. A new exploration strategy should focus on deeper sections of the Lower and Middle Jurassic, at depths much greater than previously drilled. Drilling should be significant distances from igneous emplacements, which may have breached upper reservoir seals. Reservoirs should be in carbonates and shelf elastics. An isopach map of the Baltimore Canyon Trough indicates that a significant area of Jurassic Age sediments, greater than 6 km thick, is buried to depths of mature hydrocarbon generation. Jurassic Source Rock Late Jurassic Middle Jurassic Callovian Clark, Donald aut Enthalten in Carbonates and evaporites Springer-Verlag, 1986 24(2009), 1 vom: Jan., Seite 58-76 (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:24 year:2009 number:1 month:01 pages:58-76 https://doi.org/10.1007/BF03228057 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_381 GBV_ILN_2027 GBV_ILN_4112 GBV_ILN_4309 AR 24 2009 1 01 58-76 |
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10.1007/BF03228057 doi (DE-627)OLC2076499822 (DE-He213)BF03228057-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Epstein, Samuel Abraham verfasserin aut Baltimore Canyon untested gas potential 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Northeasten Science Foundation 2009 Abstract Hydrocarbon exploration in the Baltimore Canyon during the 1980’s targeted Upper Jurassic and younger elastics and carbonates in stratigraphic traps consisting of possibly erosionally enhanced mounds and pinnacles. Five wells encountered hydrocarbons with cumulative flow rates testing 90 mm cfg/d. Apparent discontinuity in reservoir extent resulted in project abandonment. Highly mature, organic source rocks in this area were not identified. A recent organic reinterpretation of gas condensates from the Hudson Canyon suggests a deeper Lower Jurassic source, analogous to that of the U.S. Gulf Coast’s Smackover Formation, Late Jurassic in age. The Houston Oil Minerals 676 Well encountered salt at a depth of 3,800 meters on the eastern flank of the Schlee Dome. Reprocessed seismic data (AVO Analysis) indicate reflectors typical of widespread salt layers deposited during the Early Jurassic (60 m thick and 25 km wide) suggesting arid and restricted (anoxic) depositional climatic conditions in the Early Jurassic. Impermeable evaporites and shales, between the Lower and Upper Jurassic, may provide excellent seals explaining the lack of significant migration of hydrocarbons into porous rocks of the Upper Jurassic and Cretaceous. The Gulf Coast Smackover may be an excellent analog for this area. The Red Sea-Dead Sea-Sea of Galilee rift zone may be an important modern analog for the Baltimore Canyon Trough. Carbonates in this area have porosities that range between 30% and 60% permeabilities that range between 0.01 and 10,000 millidarcys. The thermal maturation profile (based on the Shell 273-1 well) for the Baltimore Canyon Trough indicates that Jurassic age sediments entered the early oil phase at a depth of approximately 2500 m and the main gas generation window at a depth of 5000 m. Gas generation in Early to Middle Jurassic sediments started in the Late Jurassic and continued through the Tertiary. Sediments younger than the Early Cretaceous are not thermally mature. A new exploration strategy should focus on deeper sections of the Lower and Middle Jurassic, at depths much greater than previously drilled. Drilling should be significant distances from igneous emplacements, which may have breached upper reservoir seals. Reservoirs should be in carbonates and shelf elastics. An isopach map of the Baltimore Canyon Trough indicates that a significant area of Jurassic Age sediments, greater than 6 km thick, is buried to depths of mature hydrocarbon generation. Jurassic Source Rock Late Jurassic Middle Jurassic Callovian Clark, Donald aut Enthalten in Carbonates and evaporites Springer-Verlag, 1986 24(2009), 1 vom: Jan., Seite 58-76 (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:24 year:2009 number:1 month:01 pages:58-76 https://doi.org/10.1007/BF03228057 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_381 GBV_ILN_2027 GBV_ILN_4112 GBV_ILN_4309 AR 24 2009 1 01 58-76 |
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10.1007/BF03228057 doi (DE-627)OLC2076499822 (DE-He213)BF03228057-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Epstein, Samuel Abraham verfasserin aut Baltimore Canyon untested gas potential 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Northeasten Science Foundation 2009 Abstract Hydrocarbon exploration in the Baltimore Canyon during the 1980’s targeted Upper Jurassic and younger elastics and carbonates in stratigraphic traps consisting of possibly erosionally enhanced mounds and pinnacles. Five wells encountered hydrocarbons with cumulative flow rates testing 90 mm cfg/d. Apparent discontinuity in reservoir extent resulted in project abandonment. Highly mature, organic source rocks in this area were not identified. A recent organic reinterpretation of gas condensates from the Hudson Canyon suggests a deeper Lower Jurassic source, analogous to that of the U.S. Gulf Coast’s Smackover Formation, Late Jurassic in age. The Houston Oil Minerals 676 Well encountered salt at a depth of 3,800 meters on the eastern flank of the Schlee Dome. Reprocessed seismic data (AVO Analysis) indicate reflectors typical of widespread salt layers deposited during the Early Jurassic (60 m thick and 25 km wide) suggesting arid and restricted (anoxic) depositional climatic conditions in the Early Jurassic. Impermeable evaporites and shales, between the Lower and Upper Jurassic, may provide excellent seals explaining the lack of significant migration of hydrocarbons into porous rocks of the Upper Jurassic and Cretaceous. The Gulf Coast Smackover may be an excellent analog for this area. The Red Sea-Dead Sea-Sea of Galilee rift zone may be an important modern analog for the Baltimore Canyon Trough. Carbonates in this area have porosities that range between 30% and 60% permeabilities that range between 0.01 and 10,000 millidarcys. The thermal maturation profile (based on the Shell 273-1 well) for the Baltimore Canyon Trough indicates that Jurassic age sediments entered the early oil phase at a depth of approximately 2500 m and the main gas generation window at a depth of 5000 m. Gas generation in Early to Middle Jurassic sediments started in the Late Jurassic and continued through the Tertiary. Sediments younger than the Early Cretaceous are not thermally mature. A new exploration strategy should focus on deeper sections of the Lower and Middle Jurassic, at depths much greater than previously drilled. Drilling should be significant distances from igneous emplacements, which may have breached upper reservoir seals. Reservoirs should be in carbonates and shelf elastics. An isopach map of the Baltimore Canyon Trough indicates that a significant area of Jurassic Age sediments, greater than 6 km thick, is buried to depths of mature hydrocarbon generation. Jurassic Source Rock Late Jurassic Middle Jurassic Callovian Clark, Donald aut Enthalten in Carbonates and evaporites Springer-Verlag, 1986 24(2009), 1 vom: Jan., Seite 58-76 (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:24 year:2009 number:1 month:01 pages:58-76 https://doi.org/10.1007/BF03228057 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_381 GBV_ILN_2027 GBV_ILN_4112 GBV_ILN_4309 AR 24 2009 1 01 58-76 |
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10.1007/BF03228057 doi (DE-627)OLC2076499822 (DE-He213)BF03228057-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Epstein, Samuel Abraham verfasserin aut Baltimore Canyon untested gas potential 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Northeasten Science Foundation 2009 Abstract Hydrocarbon exploration in the Baltimore Canyon during the 1980’s targeted Upper Jurassic and younger elastics and carbonates in stratigraphic traps consisting of possibly erosionally enhanced mounds and pinnacles. Five wells encountered hydrocarbons with cumulative flow rates testing 90 mm cfg/d. Apparent discontinuity in reservoir extent resulted in project abandonment. Highly mature, organic source rocks in this area were not identified. A recent organic reinterpretation of gas condensates from the Hudson Canyon suggests a deeper Lower Jurassic source, analogous to that of the U.S. Gulf Coast’s Smackover Formation, Late Jurassic in age. The Houston Oil Minerals 676 Well encountered salt at a depth of 3,800 meters on the eastern flank of the Schlee Dome. Reprocessed seismic data (AVO Analysis) indicate reflectors typical of widespread salt layers deposited during the Early Jurassic (60 m thick and 25 km wide) suggesting arid and restricted (anoxic) depositional climatic conditions in the Early Jurassic. Impermeable evaporites and shales, between the Lower and Upper Jurassic, may provide excellent seals explaining the lack of significant migration of hydrocarbons into porous rocks of the Upper Jurassic and Cretaceous. The Gulf Coast Smackover may be an excellent analog for this area. The Red Sea-Dead Sea-Sea of Galilee rift zone may be an important modern analog for the Baltimore Canyon Trough. Carbonates in this area have porosities that range between 30% and 60% permeabilities that range between 0.01 and 10,000 millidarcys. The thermal maturation profile (based on the Shell 273-1 well) for the Baltimore Canyon Trough indicates that Jurassic age sediments entered the early oil phase at a depth of approximately 2500 m and the main gas generation window at a depth of 5000 m. Gas generation in Early to Middle Jurassic sediments started in the Late Jurassic and continued through the Tertiary. Sediments younger than the Early Cretaceous are not thermally mature. A new exploration strategy should focus on deeper sections of the Lower and Middle Jurassic, at depths much greater than previously drilled. Drilling should be significant distances from igneous emplacements, which may have breached upper reservoir seals. Reservoirs should be in carbonates and shelf elastics. An isopach map of the Baltimore Canyon Trough indicates that a significant area of Jurassic Age sediments, greater than 6 km thick, is buried to depths of mature hydrocarbon generation. Jurassic Source Rock Late Jurassic Middle Jurassic Callovian Clark, Donald aut Enthalten in Carbonates and evaporites Springer-Verlag, 1986 24(2009), 1 vom: Jan., Seite 58-76 (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:24 year:2009 number:1 month:01 pages:58-76 https://doi.org/10.1007/BF03228057 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_381 GBV_ILN_2027 GBV_ILN_4112 GBV_ILN_4309 AR 24 2009 1 01 58-76 |
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Five wells encountered hydrocarbons with cumulative flow rates testing 90 mm cfg/d. Apparent discontinuity in reservoir extent resulted in project abandonment. Highly mature, organic source rocks in this area were not identified. A recent organic reinterpretation of gas condensates from the Hudson Canyon suggests a deeper Lower Jurassic source, analogous to that of the U.S. Gulf Coast’s Smackover Formation, Late Jurassic in age. The Houston Oil Minerals 676 Well encountered salt at a depth of 3,800 meters on the eastern flank of the Schlee Dome. Reprocessed seismic data (AVO Analysis) indicate reflectors typical of widespread salt layers deposited during the Early Jurassic (60 m thick and 25 km wide) suggesting arid and restricted (anoxic) depositional climatic conditions in the Early Jurassic. Impermeable evaporites and shales, between the Lower and Upper Jurassic, may provide excellent seals explaining the lack of significant migration of hydrocarbons into porous rocks of the Upper Jurassic and Cretaceous. The Gulf Coast Smackover may be an excellent analog for this area. The Red Sea-Dead Sea-Sea of Galilee rift zone may be an important modern analog for the Baltimore Canyon Trough. Carbonates in this area have porosities that range between 30% and 60% permeabilities that range between 0.01 and 10,000 millidarcys. The thermal maturation profile (based on the Shell 273-1 well) for the Baltimore Canyon Trough indicates that Jurassic age sediments entered the early oil phase at a depth of approximately 2500 m and the main gas generation window at a depth of 5000 m. Gas generation in Early to Middle Jurassic sediments started in the Late Jurassic and continued through the Tertiary. Sediments younger than the Early Cretaceous are not thermally mature. A new exploration strategy should focus on deeper sections of the Lower and Middle Jurassic, at depths much greater than previously drilled. Drilling should be significant distances from igneous emplacements, which may have breached upper reservoir seals. Reservoirs should be in carbonates and shelf elastics. 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baltimore canyon untested gas potential |
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Baltimore Canyon untested gas potential |
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Abstract Hydrocarbon exploration in the Baltimore Canyon during the 1980’s targeted Upper Jurassic and younger elastics and carbonates in stratigraphic traps consisting of possibly erosionally enhanced mounds and pinnacles. Five wells encountered hydrocarbons with cumulative flow rates testing 90 mm cfg/d. Apparent discontinuity in reservoir extent resulted in project abandonment. Highly mature, organic source rocks in this area were not identified. A recent organic reinterpretation of gas condensates from the Hudson Canyon suggests a deeper Lower Jurassic source, analogous to that of the U.S. Gulf Coast’s Smackover Formation, Late Jurassic in age. The Houston Oil Minerals 676 Well encountered salt at a depth of 3,800 meters on the eastern flank of the Schlee Dome. Reprocessed seismic data (AVO Analysis) indicate reflectors typical of widespread salt layers deposited during the Early Jurassic (60 m thick and 25 km wide) suggesting arid and restricted (anoxic) depositional climatic conditions in the Early Jurassic. Impermeable evaporites and shales, between the Lower and Upper Jurassic, may provide excellent seals explaining the lack of significant migration of hydrocarbons into porous rocks of the Upper Jurassic and Cretaceous. The Gulf Coast Smackover may be an excellent analog for this area. The Red Sea-Dead Sea-Sea of Galilee rift zone may be an important modern analog for the Baltimore Canyon Trough. Carbonates in this area have porosities that range between 30% and 60% permeabilities that range between 0.01 and 10,000 millidarcys. The thermal maturation profile (based on the Shell 273-1 well) for the Baltimore Canyon Trough indicates that Jurassic age sediments entered the early oil phase at a depth of approximately 2500 m and the main gas generation window at a depth of 5000 m. Gas generation in Early to Middle Jurassic sediments started in the Late Jurassic and continued through the Tertiary. Sediments younger than the Early Cretaceous are not thermally mature. A new exploration strategy should focus on deeper sections of the Lower and Middle Jurassic, at depths much greater than previously drilled. Drilling should be significant distances from igneous emplacements, which may have breached upper reservoir seals. Reservoirs should be in carbonates and shelf elastics. An isopach map of the Baltimore Canyon Trough indicates that a significant area of Jurassic Age sediments, greater than 6 km thick, is buried to depths of mature hydrocarbon generation. © Northeasten Science Foundation 2009 |
| abstractGer |
Abstract Hydrocarbon exploration in the Baltimore Canyon during the 1980’s targeted Upper Jurassic and younger elastics and carbonates in stratigraphic traps consisting of possibly erosionally enhanced mounds and pinnacles. Five wells encountered hydrocarbons with cumulative flow rates testing 90 mm cfg/d. Apparent discontinuity in reservoir extent resulted in project abandonment. Highly mature, organic source rocks in this area were not identified. A recent organic reinterpretation of gas condensates from the Hudson Canyon suggests a deeper Lower Jurassic source, analogous to that of the U.S. Gulf Coast’s Smackover Formation, Late Jurassic in age. The Houston Oil Minerals 676 Well encountered salt at a depth of 3,800 meters on the eastern flank of the Schlee Dome. Reprocessed seismic data (AVO Analysis) indicate reflectors typical of widespread salt layers deposited during the Early Jurassic (60 m thick and 25 km wide) suggesting arid and restricted (anoxic) depositional climatic conditions in the Early Jurassic. Impermeable evaporites and shales, between the Lower and Upper Jurassic, may provide excellent seals explaining the lack of significant migration of hydrocarbons into porous rocks of the Upper Jurassic and Cretaceous. The Gulf Coast Smackover may be an excellent analog for this area. The Red Sea-Dead Sea-Sea of Galilee rift zone may be an important modern analog for the Baltimore Canyon Trough. Carbonates in this area have porosities that range between 30% and 60% permeabilities that range between 0.01 and 10,000 millidarcys. The thermal maturation profile (based on the Shell 273-1 well) for the Baltimore Canyon Trough indicates that Jurassic age sediments entered the early oil phase at a depth of approximately 2500 m and the main gas generation window at a depth of 5000 m. Gas generation in Early to Middle Jurassic sediments started in the Late Jurassic and continued through the Tertiary. Sediments younger than the Early Cretaceous are not thermally mature. A new exploration strategy should focus on deeper sections of the Lower and Middle Jurassic, at depths much greater than previously drilled. Drilling should be significant distances from igneous emplacements, which may have breached upper reservoir seals. Reservoirs should be in carbonates and shelf elastics. An isopach map of the Baltimore Canyon Trough indicates that a significant area of Jurassic Age sediments, greater than 6 km thick, is buried to depths of mature hydrocarbon generation. © Northeasten Science Foundation 2009 |
| abstract_unstemmed |
Abstract Hydrocarbon exploration in the Baltimore Canyon during the 1980’s targeted Upper Jurassic and younger elastics and carbonates in stratigraphic traps consisting of possibly erosionally enhanced mounds and pinnacles. Five wells encountered hydrocarbons with cumulative flow rates testing 90 mm cfg/d. Apparent discontinuity in reservoir extent resulted in project abandonment. Highly mature, organic source rocks in this area were not identified. A recent organic reinterpretation of gas condensates from the Hudson Canyon suggests a deeper Lower Jurassic source, analogous to that of the U.S. Gulf Coast’s Smackover Formation, Late Jurassic in age. The Houston Oil Minerals 676 Well encountered salt at a depth of 3,800 meters on the eastern flank of the Schlee Dome. Reprocessed seismic data (AVO Analysis) indicate reflectors typical of widespread salt layers deposited during the Early Jurassic (60 m thick and 25 km wide) suggesting arid and restricted (anoxic) depositional climatic conditions in the Early Jurassic. Impermeable evaporites and shales, between the Lower and Upper Jurassic, may provide excellent seals explaining the lack of significant migration of hydrocarbons into porous rocks of the Upper Jurassic and Cretaceous. The Gulf Coast Smackover may be an excellent analog for this area. The Red Sea-Dead Sea-Sea of Galilee rift zone may be an important modern analog for the Baltimore Canyon Trough. Carbonates in this area have porosities that range between 30% and 60% permeabilities that range between 0.01 and 10,000 millidarcys. The thermal maturation profile (based on the Shell 273-1 well) for the Baltimore Canyon Trough indicates that Jurassic age sediments entered the early oil phase at a depth of approximately 2500 m and the main gas generation window at a depth of 5000 m. Gas generation in Early to Middle Jurassic sediments started in the Late Jurassic and continued through the Tertiary. Sediments younger than the Early Cretaceous are not thermally mature. A new exploration strategy should focus on deeper sections of the Lower and Middle Jurassic, at depths much greater than previously drilled. Drilling should be significant distances from igneous emplacements, which may have breached upper reservoir seals. Reservoirs should be in carbonates and shelf elastics. An isopach map of the Baltimore Canyon Trough indicates that a significant area of Jurassic Age sediments, greater than 6 km thick, is buried to depths of mature hydrocarbon generation. © Northeasten Science Foundation 2009 |
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