Wharton Basin is the marine area of the north east quarter of the Indian Ocean. It is named after William Wharton (1843-1905), Hydrographer of the Navy. Alternative names are Cocos Basin (after the Cocos Islands) and West Australian Basin.
It is of interest in relation to Indian Ocean floor movement and adjacent fracture zones  and the relationship between the Indian and Australian plates  and is one of a number of features of the Indian Ocean that has been studied extensively. However, its floor has not been charted since the 1960s and is not well known.
- Sclater, John G.; Fisher, Robert L. "Evolution of the East: Central Indian Ocean, with Emphasis on the Tectonic Setting of the Ninetyeast Ridge". Geological Society of America Bulletin. 85 (5): 683–702. doi:10.1130/0016-7606(1974)85<683:eoteci>2.0.co;2.
- Larson, Roger L.; Carpenter, George B.; Diebold, John B. (1978). "A geophysical study of the Wharton Basin near the Investigator Fracture Zone". Journal of Geophysical Research. 83: 773. Bibcode:1978JGR....83..773L. doi:10.1029/jb083ib02p00773.
- Schlich, R., (1982). The Indian Ocean: Aseismic ridges, spreading centers and oceanic basins. In A.E.M. Nairn and F.G. Stehli , (Eds.), The Ocean Basins and Margins, vol. 6, The Indian Ocean, Plenum, New-York.
- Pearlman, Jonathan (9 April 2014). "MH370 'may be found in days' as ship picks up signals again". Telegraph.
- Science Advances, The discovery of a conjugate system of faults in the Wharton Basin intraplate deformation zone
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