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

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Title Diagenetic remobilization of rare earth elements in a sediment core from the central Indian basin
 
Creator Pattan, J N
Banakar, V K
 
Description 341-344
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.
 
Date 2016-10-27T09:09:58Z
2016-10-27T09:09:58Z
1997-12
 
Type Article
 
Identifier 0975-1033 (Online); 0379-5136 (Print)
http://nopr.niscair.res.in/handle/123456789/36334
 
Language en_US
 
Rights CC Attribution-Noncommercial-No Derivative Works 2.5 India
 
Publisher NISCAIR-CSIR, India
 
Source IJMS Vol.26(4) [December 1997]