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dc.contributor.authorRao, P.S.
dc.contributor.authorRao, Ch.M.
dc.contributor.authorReddy, N.P.C.
dc.date.accessioned1995-06-21T10:01:39Z
dc.date.accessioned2017-09-30T01:29:50Z
dc.date.available1995-06-21T10:01:39Z
dc.date.available2017-09-30T01:29:50Z
dc.date.issued1988
dc.identifier.citationDeep Sea Research, vol.35; 1988; 1215-1221
dc.identifier.issn0198-0149
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/7082
dc.description.abstractPyritized ooids in association with turbidites were observed in a box core collected at a depth of 3627 m from the Arabian Sea Basin. Ooids having a shallow water origin were transported to the present depth by turbidity currents or slumping. Occurrence of pyrite at turbidite intervals suggests that pyritization in high organic carbon and H2S abundant environments was mainly controlled by the supply of reactive iron. From the distribution of pyrite in the core it is inferred that reactive iron necessary for pyritization was transported as colloidal oxyhydroxides from the shelf region along with the ooids
dc.languageen
dc.publisherElsevier
dc.relation.ispartofDeep-Sea Res
dc.relation.isreferencedbySCI
dc.subjectGeology and Geophysics
dc.subject.otherconcretions
dc.subject.otherooids
dc.subject.otherabundance
dc.subject.otherparticle distribution
dc.subject.othersuspended organic matter
dc.subject.otherturbidity currents
dc.subject.othersediment sampling
dc.subject.othercore analysis
dc.subject.otherpyrite
dc.subject.otherminerals
dc.subject.othermineralogy
dc.subject.otherISW, Arabian Sea
dc.titlePyritized ooids from the Arabian Sea basin
dc.typeJournal Article


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