Abstract
THE mid-ocean-ridge basalts (MORBs) from the Indian Ocean are isotopically distinctive. They have higher 87Sr/86Sr, 208Pb/206Pb and 207Pb/206Pb ratios than Pacific andAtlantic counterparts1,2 (see Fig. 1), suggesting that the upper mantle beneath the Indian Ocean has remained a partially isolated system2. The Australian–Antarctic discordance, a bathymetrically depressed segment of the South-East Indian Ridge, may represent a fundamental boundary between the Indian and Pacific mantle domains3. What processes are responsible for such domains? We argue here that the Kerguelen–Heard plume, which is producing Dupal-type basalts on Kerguelen and Heard Islands in the southern Indian Ocean, has contaminated large volumes of the Indian Ocean asthenosphere. This has produced the distinctive composition of Indian Ocean MORBs.
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Storey, M., Saunders, A., Tarney, J. et al. Contamination of Indian Ocean asthenosphere by the Kerguelen–Heard mantle plume. Nature 338, 574–576 (1989). https://doi.org/10.1038/338574a0
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DOI: https://doi.org/10.1038/338574a0
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