Changes

  | part    = Traps, trap types, and the petroleum system

  | part    = Traps, trap types, and the petroleum system

  | chapter = Petroleum systems

  | chapter = Petroleum systems

  | frompg  = 3-1

  | frompg  = 3-15

  | topg    = 3-34

  | topg    = 3-18

  | author  = Leslie B. Magoon, Edward A. Beaumont

  | author  = Leslie B. Magoon, Edward A. Beaumont

  | link    = http://archives.datapages.com/data/specpubs/beaumont/ch03/ch03.htm

  | link    = http://archives.datapages.com/data/specpubs/beaumont/ch03/ch03.htm

  | isbn    = 0-89181-602-X

  | isbn    = 0-89181-602-X

}}

}}

The Mandal-Ekofisk(!) petroleum system in the Central Graben of the North Sea contains 21.4 billion bbl of oil and 39.4 trillion ft³ of gas in 39 fields.<ref name=ch03r3>Cornford, C., 1994, [http://archives.datapages.com/data/specpubs/methodo2/data/a077/a077/0001/0500/0537.htm The Mandal-Ekofisk(!) petroleum system in the Central Graben of the North Sea], in Magoon, L., B., Dow, W., G., eds., The Petroleum System—From Source to Trap: [http://store.aapg.org/detail.aspx?id=1022 AAPG Memoir 60], p. 537–571.</ref> The age of the reservoir rock ranges from Devonian to [[Tertiary]] age with about 85% of the petroleum in rock adjacent to the Cretaceous-Tertiary boundary, specifically the Ekofisk Formation of Late Cretaceous age. Based on geochemical evidence, the Upper Jurassic (Kimmeridgian) to Lower Cretaceous source rock is the Mandal Formation. A positive oil-source rock correlation indicates a known system.

The Mandal-Ekofisk(!) [[petroleum]] system in the Central Graben of the North Sea contains 21.4 billion bbl of oil and 39.4 trillion ft³ of gas in 39 fields.<ref name=ch03r3>Cornford, C., 1994, [http://archives.datapages.com/data/specpubs/methodo2/data/a077/a077/0001/0500/0537.htm The Mandal-Ekofisk(!) petroleum system in the Central Graben of the North Sea], in Magoon, L., B., Dow, W., G., eds., The Petroleum System—From Source to Trap: [http://store.aapg.org/detail.aspx?id=1022 AAPG Memoir 60], p. 537–571.</ref> The age of the reservoir rock ranges from Devonian to [[Tertiary]] age with about 85% of the petroleum in rock adjacent to the Cretaceous-Tertiary boundary, specifically the Ekofisk Formation of Late Cretaceous age. Based on geochemical evidence, the Upper Jurassic (Kimmeridgian) to Lower Cretaceous source rock is the Mandal Formation. A positive oil-source rock correlation indicates a known system.

==Geologic setting==

==Geologic setting==

[[file:petroleum-systems_fig3-7.png|thumb|300px|{{figure number|1}}Burial history chart. From Cornford.<ref name=ch03r3 />]]

[[file:petroleum-systems_fig3-7.png|thumb|300px|{{figure number|1}}[[Burial history chart]]. From Cornford.<ref name=ch03r3 />]]

This petroleum system formed in sedimentary rocks deposited in a failed rift system in the North Sea between Great Britain, Norway, and Denmark. The prerift rocks are mostly underburden rocks and are not involved in this petroleum system except as reservoir rocks for a minor amount of petroleum. The synrift sedimentary section contains the source rock. The reservoir rock, seal rock, and overburden rock were deposited during the postrift period of sedimentation.

This petroleum system formed in sedimentary rocks deposited in a failed rift system in the North Sea between Great Britain, Norway, and Denmark. The prerift rocks are mostly underburden rocks and are not involved in this petroleum system except as reservoir rocks for a minor amount of petroleum. The synrift sedimentary section contains the source rock. The reservoir rock, seal rock, and overburden rock were deposited during the postrift period of sedimentation.

[[file:petroleum-systems_fig3-9.png|thumb|300px|{{figure number|3}}Petroleum system cross section. Modified from Cornford.<ref name=ch03r3 />]]

[[file:petroleum-systems_fig3-9.png|thumb|300px|{{figure number|3}}Petroleum system cross section. Modified from Cornford.<ref name=ch03r3 />]]

The petroleum system [[cross section]] in [[:file:petroleum-systems_fig3-9.png|Figure 3]] shows migration pathways and the spatial relation of the active source rock to the reservoir rocks. This section trends longitudinally (see [[:file:petroleum-systems_fig3-8.png|Figure 2]] for location) along the Central Graben and shows the vertical migration path from the active source rock through the Cretaceous rocks and horizontally along the basal Paleogene reservoir rocks until it [[Accumulation|accumulates]] in various traps. The underburden rock is pre-Late Jurassic in age and is not involved in the petroleum system except as minor reservoir rocks and where the Permian salt (Zechstein Group) creates diapirs that form petroleum traps and migration paths in fractured chalk.

The petroleum system [[cross section]] in [[:file:petroleum-systems_fig3-9.png|Figure 3]] shows [[hydrocarbon migration|migration]] pathways and the spatial relation of the active source rock to the reservoir rocks. This section trends longitudinally (see [[:file:petroleum-systems_fig3-8.png|Figure 2]] for location) along the Central Graben and shows the vertical migration path from the active source rock through the Cretaceous rocks and horizontally along the basal Paleogene reservoir rocks until it [[Accumulation|accumulates]] in various traps. The underburden rock is pre-Late Jurassic in age and is not involved in the petroleum system except as minor reservoir rocks and where the Permian salt (Zechstein Group) creates diapirs that form petroleum traps and migration paths in fractured chalk.

==Oil-source rock correlation==

==Oil-source rock correlation==

[[file:petroleum-systems_fig3-10.png|300px|thumb|{{figure number|4}}Biological marker analysis by Mackenzie et al.<ref name=ch03r6 /> and Hughes et al.<ref name=ch03r5 /> from reservoirs in the Greater Ekofisk, Forties, Montrose, and Argyll fields shows that these oils originated from the Mandal Formation source rockFrom Cornford.<ref name=ch03r3 />]]

[[file:petroleum-systems_fig3-10.png|300px|thumb|{{figure number|4}}Biological marker analysis by Mackenzie et al.<ref name=ch03r6 /> and Hughes et al.<ref name=ch03r5 /> from reservoirs in the Greater Ekofisk, Forties, Montrose, and Argyll fields shows that these oils originated from the Mandal Formation source rockFrom Cornford.<ref name=ch03r3 />]]

The oil-source rock correlation is a multiparameter geochemical approach; biological markers are one parameter. Biological marker analysis by Mackenzie et al.<ref name=ch03r6>Mackenzie, A., S., Maxwell, J., R., Coleman, M., L., 1983, Biological marker and isotope studies of North Sea crude oils and sediments: Proceedings of the 11th World Petroleum Congress, London, Section PD1(4), p. 45–56.</ref> and Hughes et al.<ref name=ch03r5>Hughes, W., B., Holba, A., G., Miller, D., E., Richardson, J., S., 1985, Geochemistry of the greater Ekofisk crude oils, in Thomas, B., M., eds., Petroleum Geochemistry in the Exploration of the Norwegian Shelf: London, Graham and Trotman, p. 75–92.</ref> from reservoirs in the Greater Ekofisk, Forties, Montrose, and Argyll fields shows that these oils originated from the Mandal Formation source rock, as illustrated in [[:file:petroleum-systems_fig3-10.png|Figure 4]].

The oil-source rock correlation is a multiparameter geochemical approach; biological markers are one parameter. Biological marker analysis by Mackenzie et al.<ref name=ch03r6>Mackenzie, A., S., Maxwell, J., R., Coleman, M., L., 1983, Biological marker and isotope studies of North Sea [[crude oil]]s and sediments: Proceedings of the 11th World Petroleum Congress, London, Section PD1(4), p. 45–56.</ref> and Hughes et al.<ref name=ch03r5>Hughes, W., B., Holba, A., G., Miller, D., E., Richardson, J., S., 1985, Geochemistry of the greater Ekofisk crude oils, in Thomas, B., M., eds., Petroleum Geochemistry in the Exploration of the Norwegian Shelf: London, Graham and Trotman, p. 75–92.</ref> from reservoirs in the Greater Ekofisk, Forties, Montrose, and Argyll fields shows that these oils originated from the Mandal Formation source rock, as illustrated in [[:file:petroleum-systems_fig3-10.png|Figure 4]].

==Petroleum system events chart==

==Petroleum system events chart==

[[file:petroleum-systems_fig3-11.png|thumb|300px|{{figure number|5}}Events chart. Modified from Cornford.<ref name=ch03r3 />.]]

[[file:petroleum-systems_fig3-11.png|thumb|300px|{{figure number|5}}Events chart. Modified from Cornford.<ref name=ch03r3 />.]]

An events chart indicates when the essential elements and processes took place to form a petroleum system, the critical moment, and the preservation time. In [[:file:petroleum-systems_fig3-11.png|Figure 5]], the source rock is the Upper Jurassic to Lower Cretaceous Mandal Formation, which was deposited as the rift formed. Most overburden rock of Cretaceous to Cenozoic age was deposited after the rift formed. The seal rock ranges from Permian to Neogene and consists of halite, shale, and chalk. Based on volume of petroleum, the Permian to Jurassic reservoir rocks are least important; the most important reservoir rocks are Late Cretaceous to early Paleogene in age. Most traps were created as the rift formed and filled through structural movement and halokenesis. Petroleum generation-migration-[[accumulation]] occurred from just over 100 Ma to the present day. The critical moment, or peak generation, is at 30 Ma.

An events chart indicates when the essential elements and processes took place to form a petroleum system, the critical moment, and the preservation time. In [[:file:petroleum-systems_fig3-11.png|Figure 5]], the source rock is the Upper Jurassic to Lower Cretaceous Mandal Formation, which was deposited as the rift formed. Most overburden rock of Cretaceous to [[Cenozoic]] age was deposited after the rift formed. The seal rock ranges from Permian to Neogene and consists of [[halite]], shale, and chalk. Based on volume of petroleum, the Permian to Jurassic reservoir rocks are least important; the most important reservoir rocks are Late Cretaceous to early Paleogene in age. Most traps were created as the rift formed and filled through structural movement and halokenesis. Petroleum generation-migration-[[accumulation]] occurred from just over 100 Ma to the present day. The critical moment, or peak generation, is at 30 Ma.

==Size of the petroleum system==

==Size of the petroleum system==

! rowspan = 2 | Field name || colspan = 2 | Oil || colspan = 2 | Condensate || colspan = 2 | Gas

! rowspan = 2 | Field name || colspan = 2 | Oil || colspan = 2 | Condensate || colspan = 2 | Gas

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! (&times; 10⁶ bbl) || (&times; 10⁶ m³) || (&times; 10⁶ bbl) || (&times; 10⁶ m³) || (&times; 10⁶ ft³) || (&times; 10⁶ m³)

! (&times; 10⁶ bbl) || (&times; 10⁶ m³) || (&times; 10⁶ bbl) || (&times; 10⁶ m³) || (&times; 10⁹ ft³) || (&times; 10⁹ m³)

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