Tracing the Indian Ocean Mantle Domain Through Time: Isotopic Results from Old West Indian, East Tethyan, and South Pacific Seafloor

The isotopic difference between modern Indian Ocean and Pacific or North Atlantic Ocean ridge mantle (e.g. variably lower 206Pb/204Pb for a given ε Nd and 208Pb/204Pb) could reflect processes that occurred within a few tens of millions of years preceding the initial breakup of Gondwana. Alternativel...

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Bibliographic Details
Published in:Journal of Petrology
Main Authors: Mahoney, J. J., Frei, R., Tejada, M. L. G., Mo, X. X., Leat, P. T., NäGler, T. F.
Format: Text
Language:English
Published: Oxford University Press 1998
Subjects:
Online Access:http://petrology.oxfordjournals.org/cgi/content/short/39/7/1285
https://doi.org/10.1093/petroj/39.7.1285