Diagenetic remobilization of rare earth elements in a sediment core from the central Indian Basin

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dc.contributor.author Pattan, J.N.
dc.contributor.author Banakar, V.K.
dc.date.accessioned 2009-01-12T09:18:23Z
dc.date.available 2009-01-12T09:18:23Z
dc.date.issued 1997
dc.identifier.citation Indian Journal of Marine Sciences, Vol.26; 341-344p.
dc.identifier.uri http://drs.nio.org/drs/handle/2264/2050
dc.description.abstract Rare 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.iso en
dc.publisher NISCAIR, CSIR
dc.rights Copyright [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.subject rare earths
dc.subject diagenesis
dc.subject sediments
dc.subject oxic conditions
dc.title Diagenetic remobilization of rare earth elements in a sediment core from the central Indian Basin
dc.type Journal Article


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