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dc.contributor.authorMurty, P.S.N.
dc.contributor.authorCronan, D.S.
dc.contributor.authorRao, Ch.M.
dc.contributor.authorParopkari, A.L.
dc.contributor.authorTopgi, R.S.
dc.contributor.authorGuptha, M.V.S.
dc.contributor.authorColley, N.
dc.date.accessioned1995-05-13T10:00:57Z
dc.date.accessioned2017-09-29T13:48:36Z
dc.date.available1995-05-13T10:00:57Z
dc.date.available2017-09-29T13:48:36Z
dc.date.issued1983
dc.identifier.citationMahasagar, vol.16(1); 1983; 9-30
dc.identifier.issn0542-0938
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6524
dc.description.abstractGeochemical investigations including partition analysis have been carried out on nine sediment cores from the western equatorial Indian Ocean. The results show that a core from the Arabian Sea exhibits a greater terrigenous influence than cores from the Somali Basin, and that among the Somali Basin cores depth appears to influence the variable distributions of metals in them. Iron, aluminium and titanium appear to be mainly supplied from terrigenous sources, manganese from authigenic sources, and the remaining elements from a variety of sources including submarine volcanic activity
dc.languageen
dc.publisherIndian Association for Limnology and Oceanography
dc.relation.ispartofMahasagar
dc.relation.isreferencedbyNON-SCI
dc.subjectGeology and Geophysics
dc.subject.othersediments
dc.subject.othercores
dc.subject.othergeochemistry
dc.subject.otherISW, Equatorial Indian Ocean
dc.titleGeochemistry of Sediment cores of the Western Equatorial Indian Ocean
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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