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dc.contributor.authorGlasby, G.P.
dc.date.accessioned2010-06-14T10:05:09Z
dc.date.available2010-06-14T10:05:09Z
dc.date.issued2010
dc.identifier.citationResource Geology, vol.60(2); 212-215
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/3628
dc.description.abstractOf the 12 elements enriched in Co-rich Mn crusts from the Afanasiy-Nikitin Seamount in the Equatorial S Indian Ocean, Mn, Fe and Co are enriched by a factor of approx. 10 sup(9) compared to their concentrations in seawater whereas Ni and Cu are enriched by a factor of approx. 10 sup(7) and the PGE and Au by a factor of approx.10 sup(5) to 10 sup(7) compared to their concentrations in seawater. The relatively high concentration of Pt in the crusts reflects its occurrence as fine-grained particles in the crusts rather than adsorption of the elements from seawater
dc.language.isoen
dc.publisherThe Society of Resource Geology
dc.rights© 2010 The Author. 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.subjectplatinum group elements
dc.subjectIndian Ocean
dc.titleIncorporation of transition and platinum group elements (PGE) in Co-rich Mn crusts at Afanasiy-Nikitin Seamount (AFS) in the equatorial S Indian Ocean
dc.typeJournal Article


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