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ARABIAN BASIN Latitude and Longitude:

10°N 65°E / 10°N 65°E / 10; 65
From Wikipedia, the free encyclopedia
Early Jurassic breakup of Gondwana (left) and A- Early Cretaceous, B- Late Cretaceous, C- Paleocene, D- Present Day (right)

The Arabian Basin is an oceanic basin located in the southern part of the Arabian Sea between the Arabian Peninsula and India. It is centered at 10° N, 65° E. [1] The basin depth ranges from 3,400 m in the north to 4,400 m in the south, with a maximum depth of 4,652 m. [1] The floor is covered by sediments from the Indus submarine fan and is relatively smooth. [2]

The southern enclosure of this basin is formed by the Central Indian Ridge, the Carlsberg Ridge and the Chagos-Laccadive Ridge. Bottom water enters the basin through the Owen Fracture Zone to the west. [3] The Carlsberg Ridge, at a depth of 3,800 m, separates this basin from the Somali Basin to the southwest. [1] The Arabian Basin is separated from the shallow Oman Basin by the Murray Ridge. [4] Most of the northern and eastern limits are formed by the Laxmi Ridge and the Laccadive Plateau. [2]

References

  1. ^ a b c McCutcheon, Scott; McCutcheon, Bobbi (2003). The Facts on File marine science handbook. Facts on File Science Handbooks. Infobase Publishing. p.  10. ISBN  0-8160-4812-6.
  2. ^ a b Gupta, Rabin Sen; Desa, Ehrlich (2001). The Indian Ocean: a perspective. Vol. 2. Taylor & Francis. p. 715. ISBN  90-5809-224-0.
  3. ^ Tyler, Paul A. (2003). Ecosystems of the deep oceans. Ecosystems of the world. Vol. 28. Elsevier. p. 223. ISBN  0-444-82619-X.
  4. ^ Black, Kenneth D.; Shimmield, Graham B. (2003). Biogeochemistry of marine systems. Sheffield Biological Sciences. CRC Press. p. 158. ISBN  0-8493-2818-7.

10°N 65°E / 10°N 65°E / 10; 65