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dc.contributor.authorValsangkar, A.B.
dc.date.accessioned2017-09-27T13:03:32Z
dc.date.available2017-09-27T13:03:32Z
dc.date.issued2010
dc.identifier.citationVaigyanik, vol.42(2-3); 2010; 39-44.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/5138
dc.description.abstractThe sediment coverage in the Carlsberg Ridge is similar in appearance to those in the Mid-Atlantic Ridge. The Carlsberg Ridge sediments show that their sources are continental, biogenic and diagenetic. The sedimentation rate determined by Th232 decay is 3 cm/ ka. The sediments are dominant in CaCO3 % and illite mineral, and low Cu, Fe and Mn %. They do not show enrichment of Fe, Mn and magnetic susceptibility.
dc.language.isoen
dc.rightsCopyright [2010]. 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.titleकार्ल्सवर्ग पर्वतश्रेणी के तलछट की विशेषता
dc.title.alternativeCharacteristics of sediments of Carlsberg Ridge
dc.typeJournal Article


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