The geochemical structure of the South-East Indian Ridge

Physics

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Scientific paper

Isotopic (Sr, Nd, Pb) and trace element data are reported for samples dredged along the South-East Indian Ridge (SEIR). They confirm the existence of a geochemical province under the Indian Ocean which is distinct from the provinces observed under the North Atlantic and Pacific Oceans. This province is characterized by the association of Sr and Nd isotopic enrichment features with a depleted Pb signature and of magmaphile element depletion features (low (La/Sm)N, (Nb/Zr)N, Rb/Sr with high Sm/Nd ratios).
On a regional scale, the data emphasize the strong relationship existing between the physical structure of the ridge system and its chemical characteristics. It is suggested that these chemical characteristics are the result of contribution of different mantle sources corresponding to different structures of the ridge system:
-``normal ridge'' segments,
-the ridge segment located on an immediately north of the St. Paul-Amsterdam massif,
-off-axis structures located on the structural link between Broken Ridge and Kerguelen.
In a model of ocean differentiation from Bulk Earth, it is suggested that SEIR mantle sources are the result of separate episodes of differentiation, all taking place more recently than the differentiation of the Atlantic and Pacific oceans.

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