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dc.contributor.authorBanerjee, R.
dc.contributor.authorIyer, S.D.
dc.contributor.authorDutta, P.
dc.date.accessioned2009-05-12T10:25:30Z
dc.date.available2009-05-12T10:25:30Z
dc.date.issued1991
dc.identifier.citationGeo-Marine Letters, Vol.11; 103-107p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/3252
dc.description.abstractBuried nodules from siliceous sediments in the central Indian Basin are morphologically variable and mineralogically consist of d-MnO2 incipient todorokite. Compositionally they are weakly diagenetic. The sediment coarse fractions ( 63 mu m) at different depths show variable abundances of micronodules, volcanic glass shards and biodebris. Dissolution of biodebris increases and abundance of micronodules decreases with increasing depth. Enrichment in Mn, Fe, Cu, Ni, Co, together with a decrease in organic carbon in the sediment column, may result from diagenetic metal remobilization. Diagenetically remobilized trace metals might have been utilized for the growth of micronodules over the buried nodules.
dc.language.isoen
dc.publisherSpringer
dc.rightsCopyright [1991]. 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.titleBuried nodules and associated sediments from the central Indian Basin
dc.typeJournal Article


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