Eighty Five East Ridge

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Free-air gravity map of northeastern Indian Ocean showing location of 85°E Ridge

The Eighty Five East Ridge or 85°E Ridge is a near-linear, aseismic, age-progressive ridge in the northeastern Indian Ocean. It is named for its near-parallel strike along the 85th meridian.[1] It is one of two major aseismic ridges in the Bay of Bengal, the other being the Ninety East Ridge.[2] The feature extends from the Mahanadi Basin in the north, off the northeastern coast of India, shifts westwards by about 250 km around 5°N, southeast of Sri Lanka and continues south to the Afanasy Nikitin Seamount in the Central Indian Basin.[3]

No wells have been drilled on the ridge.

Cretaceous normal superchron or "Cretaceous quiet period".[1] The correlation of the magnetization pattern of the ridge and the geomagnetic polarity timescale suggests that the volcanism that created the ridge started ~80 Ma (magnetic chron time 33r) in the Mahanadi Basin and the process continued southwards, ending at ~55 Ma near the Afanasy Nikitin Seamount.[1] There are several proposals to explain the origin and development of the ridge, one of which is that the volcanism was caused by a short-lived hotspot.[1]

References

  1. ^ a b c d e f g h i Michael, Laju; K. S. Krishna (May 2011). "Dating of the 85°E Ridge (northeastern Indian Ocean) using marine magnetic anomalies". Current Science. 100 (9). Indian Academy of Sciences: 1314–1322.
  2. ^ a b c Sar, D.; M.K. Maheshwari; S. Rangarajan; C. S. Bahuguna (July 2009). "Eighty five degrees east ridge & its hydrocarbon potential" (PDF). Geohorizons. 15. Society of Petroleum Geophysicists (SPG), India.
  3. .

Further reading