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[[File:Distribution of detritus.png|thumb|Distribution of detritus in a depositional system.]]
[[File:Distribution of detritus.png|thumb|Distribution of detritus in a depositional system]]


{{short description|Underwater geological structures associated with large-scale sediment deposition}}
{{short description|Underwater geological structures associated with large-scale sediment deposition}}
'''Abyssal fans''', also known as '''deep-sea fans''', '''underwater deltas''', and '''submarine fans''', are underwater geological structures associated with large-scale [[sediment deposition]] and formed by [[turbidity current]]s. They can be thought of as an underwater version of [[alluvial fans]] and can vary dramatically in size, with widths from several kilometres to several thousands of kilometres<ref>Gluyas, J. & Swarbrick, R. (2004) Petroleum Geoscience. Publ. Blackwell Publishing</ref> The largest is the [[Bengal Fan]], followed by the [[Indus River#Geology|Indus Fan]], but major fans are also found at the outlet of the [[Amazon River|Amazon]], [[Congo Deep-Sea Fan|Congo]], [[Mississippi River|Mississippi]] and elsewhere.<ref>{{cite journal | author=Clift | author2=Gaedicke | author3=Edwards | author4=Lee | author5=Hildebrand | author6=Amjad | author7=White | author8=Schlüter | name-list-style=amp | title=The stratigraphic evolution of the Indus Fan and the history of sedimentation in the Arabian Sea | year=2002 | journal=Marine Geophysical Researches | volume=23 | issue=3 | pages=223–245 | doi=10.1023/A:1023627123093 | s2cid=129735252 }}</ref><ref>{{cite journal | author=Covault, J.A. | title=Submarine Fans and Canyon-Channel Systems: A Review of Processes, Products, and Models | url=https://www.nature.com/scitable/knowledge/library/submarine-fans-and-canyon-channel-systems-a-24178428 | year=2011 | journal= Nature Education Knowledge | volume=3 | issue=10 | page=4 }}</ref><ref>{{cite journal | author=Shanmugam, G. | title=Submarine fans: A critical retrospective (1950–2015) | year=2016 | journal= Journal of Palaeogeography | volume=5 | issue=2 | pages=110–184 | doi=10.1016/j.jop.2015.08.011 | doi-access=free }}</ref>
'''Abyssal fans''', also known as '''deep-sea fans''', '''underwater deltas''', and '''submarine fans''', are underwater geological structures associated with large-scale [[sediment deposition]] and formed by [[turbidity current]]s. They can be thought of as an underwater version of [[alluvial fans]] and can vary dramatically in size, with widths from several kilometres to several thousands of kilometres.<ref>Gluyas, J. & Swarbrick, R. (2004) Petroleum Geoscience. Publ. Blackwell Publishing</ref> The largest is the [[Bengal Fan]], followed by the [[Indus River#Geology|Indus Fan]], but major fans are also found at the outlet of the [[Amazon River|Amazon]], [[Congo Deep-Sea Fan|Congo]], [[Mississippi River|Mississippi]] and elsewhere.<ref>{{cite journal | author=Clift | author2=Gaedicke | author3=Edwards | author4=Lee | author5=Hildebrand | author6=Amjad | author7=White | author8=Schlüter | name-list-style=amp | title=The stratigraphic evolution of the Indus Fan and the history of sedimentation in the Arabian Sea | year=2002 | journal=Marine Geophysical Researches | volume=23 | issue=3 | pages=223–245 | doi=10.1023/A:1023627123093 | s2cid=129735252 }}</ref><ref>{{cite journal | author=Covault, J.A. | title=Submarine Fans and Canyon-Channel Systems: A Review of Processes, Products, and Models | url=https://www.nature.com/scitable/knowledge/library/submarine-fans-and-canyon-channel-systems-a-24178428 | year=2011 | journal= Nature Education Knowledge | volume=3 | issue=10 | page=4 }}</ref><ref>{{cite journal | author=Shanmugam, G. | title=Submarine fans: A critical retrospective (1950–2015) | year=2016 | journal= Journal of Palaeogeography | volume=5 | issue=2 | pages=110–184 | doi=10.1016/j.jop.2015.08.011 | doi-access=free }}</ref>


== Formation ==
== Formation ==

Revision as of 05:15, 3 June 2023

Distribution of detritus in a depositional system

Abyssal fans, also known as deep-sea fans, underwater deltas, and submarine fans, are underwater geological structures associated with large-scale sediment deposition and formed by turbidity currents. They can be thought of as an underwater version of alluvial fans and can vary dramatically in size, with widths from several kilometres to several thousands of kilometres.[1] The largest is the Bengal Fan, followed by the Indus Fan, but major fans are also found at the outlet of the Amazon, Congo, Mississippi and elsewhere.[2][3][4]

Formation

Abyssal (or submarine) fans are formed from turbidity currents.

These currents begin when a geologic activity pushes sediments over the edge of a continental shelf and down the continental slope, creating an underwater landslide. A dense slurry of muds and sands speeds towards the foot of the slope, until the current slows. The decreasing current, having a reduced ability to transport sediments, deposits the grains it carries, thus creating a submarine fan. The slurry continues to slow as it is moved towards the continental rise until it reaches the ocean bed. Thus results a series of graded sediments of sand, silt and mud, which are known as turbidites, as described by the Bouma sequence.

See also

References

  1. ^ Gluyas, J. & Swarbrick, R. (2004) Petroleum Geoscience. Publ. Blackwell Publishing
  2. ^ Clift; Gaedicke; Edwards; Lee; Hildebrand; Amjad; White & Schlüter (2002). "The stratigraphic evolution of the Indus Fan and the history of sedimentation in the Arabian Sea". Marine Geophysical Researches. 23 (3): 223–245. doi:10.1023/A:1023627123093. S2CID 129735252.
  3. ^ Covault, J.A. (2011). "Submarine Fans and Canyon-Channel Systems: A Review of Processes, Products, and Models". Nature Education Knowledge. 3 (10): 4.
  4. ^ Shanmugam, G. (2016). "Submarine fans: A critical retrospective (1950–2015)". Journal of Palaeogeography. 5 (2): 110–184. doi:10.1016/j.jop.2015.08.011.

Sources

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