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Evidence for heterogenes primary MORB and mantle sources, NW Indian Ocean

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Abstract

Basalts from 5 Deep Sea Drilling Project (DSDP) sites in the northwest Indian Ocean (Somali Basin and Arabian Sea) have general geochemical features consistent with a spreading origin at the ancient Carlsberg Ridge. However, compared to most MORBS from other oceans they have low normative olivine, TiO2, and Zr contents. There is no evidence that the mantle source of these northwest Indian Ocean basalts was enriched in incompatible elements relative to the Atlantic and Pacific ocean mantles. In detail, incompatible element abundances in these DSDP basalts establish that they evolved from several compositionally distinct parental magmas. In particular, basalts from site 236 in the Somali Basin have relatively high SiO2 and low Na, P, Ti, and Zr contents. These compositional features along with low normative olivine contents are similar to those proposed for melts derived by two-stage (or dynamic) melting. Published data also indicate there is no enrichment in incompatible elements at the southwest Indian Ocean triple junction, although southwest Indian Ocean basalts have slightly higher 87Sr/86Sr than “normal” Atlantic MORB. The data suggest that there are significant subtle geochemical variations in the Indian Ocean mantle sources, but are insufficient to show whether these variations have a systematic temporal or geographic distribution.

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Authors and Affiliations

  1. Department of Earth and Planetary Sciences, Massachusetts Institute of Technology, 02139, Cambridge, MA, USA

    Fred A. Frey & John S. Dickey Jr.

  2. Woods Hole Oceanographic Institution, 02543, Woods Hole, MA, USA

    Geoffrey Thompson & Wilfred B. Bryan

  3. Geological Survey, Port Moresby, Papua, New Guinea

    Hugh L. Davies

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  1. Fred A. Frey
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  2. John S. Dickey Jr.
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  3. Geoffrey Thompson
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  4. Wilfred B. Bryan
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  5. Hugh L. Davies
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Frey, F.A., Dickey, J.S., Thompson, G. et al. Evidence for heterogenes primary MORB and mantle sources, NW Indian Ocean. Contr. Mineral. and Petrol. 74, 387–402 (1980). https://doi.org/10.1007/BF00518119

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