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dc.contributor.authorPattan, J.N.
dc.contributor.authorBanakar, V.K.
dc.date.accessioned2009-01-12T09:18:23Z
dc.date.available2009-01-12T09:18:23Z
dc.date.issued1997
dc.identifier.citationIndian Journal of Marine Sciences, Vol.26; 341-344p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/2050
dc.description.abstractRare earth elements (REE) distribution in a 36 cm long sediment box core from the Central Indian Basin is studied. REE concentration is generally higher in the upper oxic zone than in intermediate suboxic zone suggesting REE diffusion upwards the sediment column and subsequent incorporation in the oxyhydroxide phase. The similarity in depth distribution of bulk REE concentration solid Mn phase and micronodule abundance from the coarse fraction suggest that micronodules are one of the major component controlling the REE distribution in a sediment column.
dc.language.isoen
dc.publisherNISCAIR, CSIR
dc.rightsCopyright [1997]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subjectrare earths
dc.subjectdiagenesis
dc.subjectsediments
dc.subjectoxic conditions
dc.titleDiagenetic remobilization of rare earth elements in a sediment core from the central Indian Basin
dc.typeJournal Article


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