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. 1 2 3 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. 1 2 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


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