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dc.contributor.authorBanakar, V.K.
dc.contributor.authorSudhakar, M.
dc.date.accessioned1995-08-14T10:01:42Z
dc.date.accessioned2017-09-30T01:29:45Z
dc.date.available1995-08-14T10:01:42Z
dc.date.available2017-09-30T01:29:45Z
dc.date.issued1988
dc.identifier.citationIndian Journal of Marine Sciences, vol.17; 1988; 265-269
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/7016
dc.description.abstractStudy of ferro-manganese oxide growth on apatitic substrates like shark teeth enamel from siliceous sediment environment (lat. 10 degrees S and long. 75 degrees E) suggests the changes in depositional environments within the sediment layer through the growth history of these oxides. Though the nature of substrates does not have any control over the mineralogy and chemistry of Fe-Mn oxides, an active sink like loose sediment or altered basaltic coat appears to be the primary requirement before ferric hydroxide coat on hard nucleating agent
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectGeology and Geophysics
dc.subject.otherteeth
dc.subject.otherferromanganese oxides
dc.subject.othersubstrata
dc.subject.othersedimentary environments
dc.subject.otherISW, Central Indian Ocean
dc.titleFerro-manganese oxide growth on shark teeth from cenral Indian Ocean basin
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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