Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38315
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dc.contributor.authorRao, P S-
dc.contributor.authorPattan, J N-
dc.date.accessioned2016-12-08T09:59:23Z-
dc.date.available2016-12-08T09:59:23Z-
dc.date.issued1989-03-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38315-
dc.description11-15en_US
dc.description.abstractMineralogical and chemical investigations show that todorokite is the only Mn mineral in the Mid-Indian Ridge ferromanganese, coatings, delta δ MnO2 in the seamount crusts, and well crystallised todorokite and minor amounts of delta δ MnO2 in the abyssal nodules. Enrichment of Mn, Cu, Ni and Mn/Fe ratio is in the sequence, abyssal nodules > seamount crusts > Mid-Indian Ridge samples. Fe is highest in the Mid-Indian Ridge samples followed by seamount crusts and abyssal nodules. Co is enriched (up to 0.47 %) in the seamount crusts. The ferromanganese oxides from the Mid-Indian Ridge, seamount crusts and abyssal nodules appear to be of hydrothermal, hydrogenous and early-diagenetic in origin respectively.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.18(1) [March 1989]en_US
dc.titleFerromanganese oxides from Mid-Indian Ridge, seamounts and abyssal plains from the Indian Oceanen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.18(1) [March 1989]

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