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List of fracture zones

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List of fracture zones
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Fracture zones are common features in the geology of oceanic basins. Globally most fault zones are located on divergent plate boundaries on oceanic crust. This means that they are located around mid-ocean ridges and trend perpendicular to them. The term fracture zone is used almost exclusively for features on oceanic crust; similar structures on continental crust are instead termed transform or strike slip faults. Some use the term "transform fault" to describe the seismically and tectonically active portion of a fracture zone after John Tuzo Wilson's concepts first developed with respect to the Mid-Atlantic Ridge.[1] The term fracture zone has a distinct geological meaning, but it is also used more loosely in the naming of some oceanic features. Fracture zones are much longer than wide, but may have feature complexity within their width. Not all named fracture zones are active, indeed only the central portion of those still forming usually is, in an area of active transform faulting associated with a mid-ocean ridge. Classic fracture zones remain significant ocean floor features with usually different aged rocks on either side of the fracture zone due to past tectonic processes. Some fracture zones have been created by mid-ocean ridge segments that have been subducted and that part may no longer exist.

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Approximate surface projection on oceans of named fracture zones (orange). Also shown are relevant present plate boundaries (white) and associated features (lighter orange). Click to expand to interactive map.'"`UNIQ--ref-00000001-QINU`"'
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Major active fractures zones worldwide are in the orange shaded areas perpendicular to the black lines of the mid-ocean ridges of the major oceanic plates.
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Pacific Ocean

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Major Pacific trenches (1–10) and fracture zones (11–20): 1. Kermadec 2. Tonga 3. Bougainville 4. Mariana 5. Izu–Ogasawara 6. Japan 7. Kuril–Kamchatka 8. Aleutian 9. Middle America 10. Peru–Chile 11. Mendocino 12. Murray 13. Molokai 14. Clarion 15. Clipperton 16. Challenger 17. Eltanin 18. Udintsev 19. East Pacific Rise (S-shaped) 20. Nazca Ridge

Most fracture zones in the Pacific Ocean originate from large mid-ocean ridges (also called "rises") such as the East Pacific Rise, Chile Rise and Juan de Fuca Ridge. The plates that host the fractures are Nazca, Pacific, Antarctic, Juan de Fuca and Cocos among others. Fracture zones being subducted under Southern and Central America are generally southwest–northeast oriented reflecting the relative motion of Cocos, Nazca and the Antarctic plates.

Chile Rise

The fracture zones of the Chile Rise trend in a west to east fashion with the most southern ones taking a slightly more southwest to northeast orientation. This non-perpendicular relation to Chile's coast reflects the oblique subduction of Nazca plate under southern Chile. West of Chile rise the fracture zones are hosted in the Antarctic plate. Some fracture zones such as Chile and Valdivia make up large sections of the Nazca-Antarctic plate boundary.

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Map of the Chile Rise and its fracture zones in Nazca and the Antarctic plates
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Active Pacific Ocean fracture zones are perpendicular to the mid-ocean ridges (black lines) in orange shaded region. Since the map was prepared ages not shown of south-west Pacific and north Pacific Ocean floors may have been characterised.
More information Name, Minimum length in km ...

East Pacific Rise

The East Pacific Rise includes the Pacific–Antarctic Rise (Pacific plate and Antarctic plate boundary) in some usages and in others relates only to the boundaries between the Pacific plate and the Nazca plates which includes the Juan Fernández plate and Easter microplate.

Nazca plate boundary

More information Name, Minimum length in km ...

Pacific–Antarctic Rise

More information Name, Minimum length in km ...

Cocos–Nazca spreading center

Western Pacific

Some of the fracture zones in the western Pacific Ocean are associated with the smaller plate boundaries of the active back-arc basin spreading center of the North Fiji Basin being the Hunter fracture zone and North Fiji fracture zone. The Parece Vela Rift (Parece Vela fracture zone province) is also associated with the back-arc basin of the Parece Vela Basin (West Mariana Basin) at the intersection of the Philippine Sea plate and Mariana plate.[4]:70–73

South of the Equator

North of the Equator

  • Victoria fracture zone
  • Central fracture zone
  • Parece Vela Rift (Parece Vela fracture zone province)
    • Kokugan fracture zone
    • Owashi fracture zone
    • Ojirowashi fracture zone
    • Inuwashi fracture zone
    • Konotori fracture zone
    • Toki fracture zone
    • Tancho fracture zone
    • Raicho fracture zone
  • Ortelius fracture zone
  • Waghenaer fracture zone
  • Rat fracture zone

West of East Pacific Rise and Gulf of California Rift Zone

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A map of the Juan de Fuca plate
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Age of ocean floor, with fracture zones in the north Pacific Ocean. Hawaii-Emperor seamount chain in black.

(some are inactive)[5]

Juan de Fuca and Gorda Ridges

Surveyor, Molokai, Pioneer and Murray fracture zones shown in the list were created by ridge segments that no longer exist.[5]

Northeast Pacific

  • Sedna fracture zone
  • Sila fracture zone
  • Aja fracture zone
  • Cobb fracture zone
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Atlantic Ocean

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Major fractures zones of the Atlantic can be seen on this ocean depth map
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Active Atlantic Ocean fracture zones are perpendicular to the mid-ocean ridges (black lines) in orange shaded region

In the Atlantic Ocean most fracture zones originate from the Mid-Atlantic Ridge, which runs from north to south, and are therefore west to east oriented in general. There are about 300 fracture zones, with an average north–south separation of 55 kilometres (34 mi):[6] two for each degree of latitude. Physically it makes sense to group Atlantic fracture zones into three categories:[7]

  1. Small offset: length of transform fault less than 30 kilometres (19 mi)
  2. Medium offset: offset over 30 kilometers
  3. Large offset: offset several hundreds of kilometers

Mid-Atlantic Ridge (Northern Hemisphere)

More information Name, Minimum length in km ...

Fracture zones involved in the early opening of the North Atlantic

More information American side, African side ...

Mid-Atlantic Ridge (Southern Hemisphere)

More information Name, Minimum length in km ...
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Indian Ocean

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The Indian Ocean fracture zones are mainly related to the Southwest Indian Ridge and Southeast Indian Ridge mid-ocean ridges.

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Active Indian Ocean fracture zones are perpendicular to the mid-ocean ridges (black lines) in orange shaded region

Southwest Indian Ridge

Carlsberg Ridge

Central Indian Ridge

  • Bao Chuan fracture zone
  • Mabahiss fracture zone
  • Sealark fracture zone
  • Vityaz fracture zone
  • Vema fracture zone (not to be confused with fracture zone of same name in the Atlantic)
  • Argo fracture zone
  • Mary Celeste fracture zone
  • Rodrigues fracture zone
  • Mauritius Fault Zone
  • Egeria fracture zone
  • Flinders fracture zone

Lakshadweep-Chagos Ridge

  • Vishnu Fault Zone

Southeast Indian Ridge

  • Ter Tholen fracture zone
  • Zeewolf fracture zone
  • Nieuw Amsterdam fracture zone
  • Vlamingh fracture zone
  • Geelvinck fracture zone
  • Zeehaen fracture zone
  • Heemskerck fracture zone
  • Saint Vincent fracture zone
  • Gambier fracture zone
  • Tasman fracture zone
  • Balleny fracture zone

Southern Ocean

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Active Southern Ocean fracture zones are perpendicular to the mid-ocean ridges (black lines) in orange shaded region

References

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