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dc.contributor.authorNaqvi, S.W.A.
dc.contributor.authorKureishy, T.W.
dc.date.accessioned1995-06-15T10:01:21Z
dc.date.accessioned2017-09-29T13:48:18Z
dc.date.available1995-06-15T10:01:21Z
dc.date.available2017-09-29T13:48:18Z
dc.date.issued1986
dc.identifier.citationIndian Journal of Marine Sciences, vol.15; 1986; 48-49
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6175
dc.description.abstractHydro chemical studies at a station (10 degrees 34.l'N,56 degrees 31,7'E) in the Owen Fracture zone reveal an active movement of bottom water as approx 75 m thick, cold, low-salinity layer. Silicate profile exhibits a broad maximum coinciding with a salinity maximum at about 3 km depth in conformity with earlier results. Within the benthic layer, an increase in AOU is observed associated with minor increases in nutrients, presumably due to the oxidation of particulate organic matter sinking from the surface layer
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.otherparticulate organic matter
dc.subject.otheroxidation
dc.subject.othernutrients (mineral)
dc.subject.otherbenthic boundary layer
dc.subject.otherdeep-water masses
dc.subject.otherbottom water
dc.subject.othersubmarine features
dc.subject.otherfracture zones
dc.subject.otherISW, Arabian Sea
dc.titleDeep and bottom water characteristics in the Owen Fracture Zone, Western Arabian Sea
dc.typeJournal Article


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