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dc.contributor.authorIyer, S.D.
dc.contributor.authorFernandes, G.Q.
dc.contributor.authorMahender, K.
dc.date.accessioned2015-11-06T06:13:19Z
dc.date.available2015-11-06T06:13:19Z
dc.date.issued2012
dc.identifier.citationJournal Indian Association of Sedimentologists, vol.31(1&2); 2012; 123-135.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/4866
dc.description.abstractCoarse Fractions Components of a sediment core (268 cm from a water depth of 5120 m) collected at 18 degrees S and 80 degrees E from the red clay domain in the Central Indian Ocean Basin (CIOB), comprises mineral grains, basaltic fragments, phillipsite, ferromanganese micronodules, glass shards, small pumices, microtektites and biogenic material. This paper describes the provenance of these coarse fraction components that have resulted from multiple sources- both in situ and derived products.
dc.language.isoen
dc.publisherIndian Association of Sedimentologists
dc.rightsCopyright [2012]. An edited version of this paper was published by Indian Association of Sedimentologists. 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.subjectAQUATIC RESOURCES
dc.subjectGEOLOGY AND GEOPHYSICS
dc.subjectGEOLOGY AND GEOPHYSICS
dc.titleCoarse fraction components in a red-clay sedimemt core, Central Indian Ocean Basin: Their occurrence and significance
dc.typeJournal Article


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