Oil and gas traps - Revision history

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	<onlyinclude>'''Oil and gas traps''', sometimes referred to as '''petroleum traps''' are below ground traps where a permeable [[oil and gas reservoir\|reservoir]] rock is covered by some low [[permeability]] cap rock. This combination of rock can take several forms, but they all prevent the upward migration of [[oil]] and [[natural gas]] up through the reservoir rock.</onlyinclude> Once oil and natural gas are in the reservoir rock, they continue to migrate upwards through the pore spaces of the rock until blocked by some sort of seal with a cap rock.<ref name="RE2">Geo Info. (December 23, 2015). ''Introduction to Petroleum Geology'' [Online]. Available: http://geoinfo.nmt.edu/faq/energy/petroleum/petroleum_geology_intro.pdf</ref> ~~The~~ low permeability cap ~~rocks~~ are generally [[shale]] or low permeability sandstones and carbonate rocks.<ref name="RE1">KAU. (December 22, 2015). ''Petroleum Traps'' [Online]. Available: http://www.kau.edu.sa/Files/0054337/Subjects/types%20of%20oil%20traps.pdf</ref>		<onlyinclude>'''Oil and gas traps''', sometimes referred to as '''petroleum traps''', are below-ground "traps" where a permeable [[oil and gas reservoir\|reservoir]] rock is covered by some low [[permeability]] cap rock. This combination of rock can take several forms, but they all prevent the upward migration of [[oil]] and [[natural gas]] up through the reservoir rock.</onlyinclude> Once oil and natural gas are in the reservoir rock, they continue to migrate upwards through the pore spaces of the rock until blocked by some sort of seal with a cap rock.<ref name="RE2">Geo Info. (December 23, 2015). ''Introduction to Petroleum Geology'' [Online]. Available: http://geoinfo.nmt.edu/faq/energy/petroleum/petroleum_geology_intro.pdf</ref> "Seal" is a more general term that refers to rock with low permeability. The "cap rock" specifically traps oil and natural gas in the reservoir rock below them, and are generally composed of [[shale]] or low permeability sandstones and carbonate rocks.<ref name="RE1">KAU. (December 22, 2015). ''Petroleum Traps'' [Online]. Available: http://www.kau.edu.sa/Files/0054337/Subjects/types%20of%20oil%20traps.pdf</ref>

	There are two major categories of traps, and are classified based on how the [[petroleum]] accumulates. The two main groups are '''structural traps''' and '''stratigraphic traps'''.<ref name="RE1"/> For a more in-depth description of the overall structure of oil and gas deposits, see [[oil and gas reservoir]].		There are two major categories of traps, and are classified based on how the [[petroleum]] accumulates. The two main groups are '''structural traps''' and '''stratigraphic traps'''.<ref name="RE1"/> For a more in-depth description of the overall structure of oil and gas deposits, see [[oil and gas reservoir]].

	[[File:oil traps.png\|800px\|center\|thumb\|Figure 1. Diagram showing the structure of several different types of oil and gas traps.<ref>Wikimedia Commons. (December 22, 2015). ''Oil Traps'' (Online). Available: https://upload.wikimedia.org/wikipedia/commons/thumb/a/af/Oil_traps.svg/2000px-Oil_traps.svg.png</ref>]]		[[File:oil traps.png\|800px\|center\|thumb\|Figure 1. Diagram showing the structure of several different types of oil and gas traps. (A) is the cap rock and (B) is the reservoir rock.<ref>Wikimedia Commons. (December 22, 2015). ''Oil Traps'' (Online). Available: https://upload.wikimedia.org/wikipedia/commons/thumb/a/af/Oil_traps.svg/2000px-Oil_traps.svg.png</ref>]]


	==Structural Traps==		==Structural Traps==
	These traps ~~are types that~~ form as a result of some structural deformation - a bend or dip - of rock. These traps take on several ~~forms and~~ shapes as a result of different types of deformation. This deformation tends to take place over tens or hundreds of millions of years after sediment that creates the seals and rocks ~~themselves have~~ been deposited.<ref name="RE2"/> In these traps, the pores of the reservoir rock contain oil, gas, or [[water]]. Gas moves up in the trap as it is the lightest, with oil below it and water at the bottom. The cap rock prevents upward migration of these [[fluid]]s.		These types of traps form as a result of some structural ''deformation'' (a bend or dip) of the rock. These traps take on several shapes as a result of different types of deformation. This deformation tends to take place over tens or hundreds of millions of years, after the sediment that creates the seals and rocks has been deposited.<ref name="RE2"/> In these traps, the pores of the reservoir rock contain oil, gas, or [[water]]. Gas moves up in the trap as it is the lightest, with oil below it and water at the bottom. The cap rock prevents upward migration of these [[fluid]]s.

	===Anticline Traps===		===Anticline Traps===
	These types of traps are formed by a folding of rock. Specifically, a sandstone bed covered with low permeability shale is folded into a trap that contains petroleum products. Hydrocarbons are trapped in the peak of this fold.<ref name="RE1"/> An anticline trap is shown in the upper-left of Figure 1. Most anticline traps are created as a result of sideways pressure, folding the layers of rock, but can also occur from sediments being compacted. For more information on anticline traps, click [[anticline\|here]].<ref name="RE3">David Oser. (December 23, 2015). ''Petroleum Geology'' [Online]. Available: http://davidosergeology.tripod.com/petroleomgeology/index.html</ref>		These types of traps are formed by a folding of rock into an upwards convex shape. Specifically, a sandstone bed covered with low permeability shale is folded into a trap that contains petroleum products. Hydrocarbons are trapped in the peak of this fold.<ref name="RE1"/> An anticline trap is shown in the upper-left corner of Figure 1. Most anticline traps are created as a result of sideways pressure, folding the layers of rock, but can also occur from sediments being compacted. For more information on anticline traps, click [[anticline\|here]].<ref name="RE3">David Oser. (December 23, 2015). ''Petroleum Geology'' [Online]. Available: http://davidosergeology.tripod.com/petroleomgeology/index.html</ref>

	===Fault Traps===		===Fault Traps===
	These types of traps are formed when reservoir rock is split along a fault line. Between the walls of the split reservoir, clay traps oil and prevents it from leaving the trap.<ref name="RE3"/> Other times there exists a pressure differential across the two sides of the fault that prevents the fluids from migrating.<ref name="RE1"/> A fault trap is shown in the upper-right of Figure 1. Although faulting is common in many petroleum fields, traps that result from faulting alone are not very common. Generally speaking, faulting creates some other type of structure that creates the main trap.<ref name="RE1"/>		These types of traps are formed when reservoir rock is split along a fault line. Between the walls of the split reservoir, clay traps oil and prevents it from leaving the trap.<ref name="RE3"/> Other times there exists a pressure differential across the two sides of the fault that prevents the fluids from migrating.<ref name="RE1"/> A fault trap is shown in the upper-right corner of Figure 1. Although faulting is common in many petroleum fields, traps that result from faulting alone are not very common. Generally speaking, faulting creates some other type of structure that creates the main trap.<ref name="RE1"/>

	===Salt Domes===		===Salt Domes===
	Salt dome traps are formed as a result of below ground salt - which is less [[density\|dense]] than the rock above it - moving upwards slowly. This upward migration of the salt can deform and break up rock along the way.<ref name="RE3"/> The process of this salt deforming rock is known as salt tectonics, and take place over hundreds of millions of years.<ref name="RE1"/> Oil and gas that flows through the reservoir rock will come to rest when it reaches the salt dome and is then trapped. A salt dome trap is shown on the lower left of Figure 1.		Salt dome traps are formed as a result of below ground salt (which is less [[density\|dense]] than the rock above it) moving upwards slowly. This upward migration of the salt can deform and break up rock along the way.<ref name="RE3"/> The process of this salt deforming rock is known as salt tectonics, and take place over hundreds of millions of years.<ref name="RE1"/> Oil and gas that flows through the reservoir rock will come to rest when it reaches the salt dome and is then trapped. A salt dome trap is shown in the lower-left corner of Figure 1.

	==Stratigraphic Traps==		==Stratigraphic Traps==
	These traps are formed as a result of the deposition in [[sedimentary rock]]s. When the sediment that creates the reservoir rock is deposited in a discontinuous layer, the seals are created beside and on top of the reservoir. In some cases, these seals are made of impermeable or low permeability shale deposited around the reservoir, blocking the oil and gas inside. The seals themselves may also be source rocks.<ref name="RE2"/> A ~~stratiographic~~ trap is shown on the bottom right of Figure 1.		These traps are formed as a result of the deposition in [[sedimentary rock]]s. When the sediment that creates the reservoir rock is deposited in a discontinuous layer, the seals are created beside and on top of the reservoir. In some cases, these seals are made of impermeable or low permeability shale deposited around the reservoir, blocking the oil and gas inside. The seals themselves may also be source rocks.<ref name="RE2"/> A stratigraphic trap is shown in the bottom-right corner of Figure 1.

			There are two main types of stratigraphic traps that are classified by ''when'' changes occur relative to the sedimentation process. '''Primary stratigraphic traps''' result from changes that develop during the sedimentation process. These are generally structural changes that arise as a result of discontinuous deposition of sediment. '''Secondary stratigraphic traps''' result from changes that develop after sedimentation has occurred. These changes can involve changes in porosity of the rock that lead to formation of a cap-like rock.<ref name="RE2"/>

			== For Further Reading ==

	There are two main types of stratigraphic traps that are classified by when changes occur relative to the sedimentation process. Primary stratigraphic traps result from changes that develop during the sedimentation process. These are generally structural changes that arise as a result of discontinuous deposition of sediment. Secondary stratigraphic traps result from changes that develop after sedimentation has occurred. These changes can involve changes in porosity of the rock ~~that lead to formation of~~ a ~~cap-like rock.<ref name="RE2"/>~~		* [[Reservoir]]
			* [[Permeability]]
			* [[Cap rock]]
			* [[Source rock]]
			* [[Density]]
			* [[Anticline]]
			* Or explore a [[Special:Random\|random page]]

	==References==		==References==
	{{reflist}}		{{reflist}}
			[[Category:Uploaded]]

Jmdonev: 1 revision imported

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Jmdonev at 19:42, 28 December 2015

2015-12-28T19:42:21Z

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[[Category:Done 2016-01-15]]
<onlyinclude>'''Oil and gas traps''', sometimes referred to as '''petroleum traps''' are below ground traps where a permeable [[oil and gas reservoir|reservoir]] rock is covered by some low [[permeability]] cap rock. This combination of rock can take several forms, but they all prevent the upward migration of [[oil]] and [[natural gas]] up through the reservoir rock.</onlyinclude> Once oil and natural gas are in the reservoir rock, they continue to migrate upwards through the pore spaces of the rock until blocked by some sort of seal with a cap rock.<ref name="RE2">Geo Info. (December 23, 2015). ''Introduction to Petroleum Geology'' [Online]. Available: http://geoinfo.nmt.edu/faq/energy/petroleum/petroleum_geology_intro.pdf</ref> The low permeability cap rocks are generally [[shale]] or low permeability sandstones and carbonate rocks.<ref name="RE1">KAU. (December 22, 2015). ''Petroleum Traps'' [Online]. Available: http://www.kau.edu.sa/Files/0054337/Subjects/types%20of%20oil%20traps.pdf</ref>

There are two major categories of traps, and are classified based on how the [[petroleum]] accumulates. The two main groups are '''structural traps''' and '''stratigraphic traps'''.<ref name="RE1"/> For a more in-depth description of the overall structure of oil and gas deposits, see [[oil and gas reservoir]].

[[File:oil traps.png|800px|center|thumb|Figure 1. Diagram showing the structure of several different types of oil and gas traps.<ref>Wikimedia Commons. (December 22, 2015). ''Oil Traps'' (Online). Available: https://upload.wikimedia.org/wikipedia/commons/thumb/a/af/Oil_traps.svg/2000px-Oil_traps.svg.png</ref>]]

==Structural Traps==
These traps are types that form as a result of some structural deformation - a bend or dip - of rock. These traps take on several forms and shapes as a result of different types of deformation. This deformation tends to take place over tens or hundreds of millions of years after sediment that creates the seals and rocks themselves have been deposited.<ref name="RE2"/> In these traps, the pores of the reservoir rock contain oil, gas, or [[water]]. Gas moves up in the trap as it is the lightest, with oil below it and water at the bottom. The cap rock prevents upward migration of these [[fluid]]s.

===Anticline Traps===
These types of traps are formed by a folding of rock. Specifically, a sandstone bed covered with low permeability shale is folded into a trap that contains petroleum products. Hydrocarbons are trapped in the peak of this fold.<ref name="RE1"/> An anticline trap is shown in the upper-left of Figure 1. Most anticline traps are created as a result of sideways pressure, folding the layers of rock, but can also occur from sediments being compacted. For more information on anticline traps, click [[anticline|here]].<ref name="RE3">David Oser. (December 23, 2015). ''Petroleum Geology'' [Online]. Available: http://davidosergeology.tripod.com/petroleomgeology/index.html</ref>

===Fault Traps===
These types of traps are formed when reservoir rock is split along a fault line. Between the walls of the split reservoir, clay traps oil and prevents it from leaving the trap.<ref name="RE3"/> Other times there exists a pressure differential across the two sides of the fault that prevents the fluids from migrating.<ref name="RE1"/> A fault trap is shown in the upper-right of Figure 1. Although faulting is common in many petroleum fields, traps that result from faulting alone are not very common. Generally speaking, faulting creates some other type of structure that creates the main trap.<ref name="RE1"/>

===Salt Domes===
Salt dome traps are formed as a result of below ground salt - which is less [[density|dense]] than the rock above it - moving upwards slowly. This upward migration of the salt can deform and break up rock along the way.<ref name="RE3"/> The process of this salt deforming rock is known as salt tectonics, and take place over hundreds of millions of years.<ref name="RE1"/> Oil and gas that flows through the reservoir rock will come to rest when it reaches the salt dome and is then trapped. A salt dome trap is shown on the lower left of Figure 1.

==Stratigraphic Traps==
These traps are formed as a result of the deposition in [[sedimentary rock]]s. When the sediment that creates the reservoir rock is deposited in a discontinuous layer, the seals are created beside and on top of the reservoir. In some cases, these seals are made of impermeable or low permeability shale deposited around the reservoir, blocking the oil and gas inside. The seals themselves may also be source rocks.<ref name="RE2"/> A stratiographic trap is shown on the bottom right of Figure 1.

There are two main types of stratigraphic traps that are classified by when changes occur relative to the sedimentation process. Primary stratigraphic traps result from changes that develop during the sedimentation process. These are generally structural changes that arise as a result of discontinuous deposition of sediment. Secondary stratigraphic traps result from changes that develop after sedimentation has occurred. These changes can involve changes in porosity of the rock that lead to formation of a cap-like rock.<ref name="RE2"/>

==References==
{{reflist}}