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dc.contributor.authorBanakar, V.K.
dc.contributor.authorBorole, D.V.
dc.date.accessioned1995-06-22T10:01:47Z
dc.date.accessioned2017-09-30T01:29:55Z
dc.date.available1995-06-22T10:01:47Z
dc.date.available2017-09-30T01:29:55Z
dc.date.issued1989
dc.identifier.citationJournal of the Geological Society of India, vol.33; 1989; 253-258
dc.identifier.issn0016-7622
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/7203
dc.description.abstractmhe ferro-manganese nodule collected in EEZ of Seychelles yields a growth rate of 1.5 mm/10 6Y 230Th (ex)/ and 230Th (ex)/ 232Th activity ratio methods indicating very slow growth of ferro-manganese nodules. The Mn/Fe and U/Th ratios suggest that the genesis of the studied nodule is of hydrogenetic origin
dc.languageen
dc.publisherGeological Society of India
dc.relation.ispartofJ Geol Soc India
dc.relation.isreferencedbySCI
dc.subjectGeology and Geophysics
dc.subject.othergrowth
dc.subject.othergeochemistry
dc.subject.otherexclusive economic zone
dc.subject.otherferromanganese nodules
dc.subject.otherISW, Seychelles
dc.titleGrowth rate and chemical composition of a manganese nodule from the EEZ of Seychelles
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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