Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38570
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dc.contributor.authorBanakar, V K-
dc.contributor.authorSudhakar, M-
dc.date.accessioned2016-12-13T12:05:30Z-
dc.date.available2016-12-13T12:05:30Z-
dc.date.issued1988-12-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38570-
dc.description265-269en_US
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.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.17(4) [December 1988]en_US
dc.titleFerro-Manganese Oxide Growth on Shark Teeth from Central Indian Ocean Basinen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.17(4) [December 1988]

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