Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38591
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dc.contributor.authorRao, A T-
dc.contributor.authorRaman, C V-
dc.date.accessioned2016-12-14T05:40:23Z-
dc.date.available2016-12-14T05:40:23Z-
dc.date.issued1986-03-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38591-
dc.description20-23en_US
dc.description.abstractRed sediments, characterised by badland like topography, found along the Visakhapatnam - Bhimunipatnam coast and associated with khondalite hill ranges comprise 60-70% (quartz + heavies), 20% silt and 10% ferruginous clay. Kaolinite and illite proportions are dominant in the clays of the red sediments and compare fairly with the clays from the offshore region. The similar concentration of elements - K, Fe, Ti, Cr,Co, Ba, Sr and Pb - supports the clay input from the red sediments into the shelf region, Ti, V, Mn, Cr with Fe and Sr, Ba, Pb with K show positive relationship, which reflects alteration of detrital magnetite and ilmenite and orthoclase in the source rocks.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.15(1) [March 1986]en_US
dc.titleGeochemical studies of clays from red sediments of Visakhapatnam coast, east coast of Indiaen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.15(1) [March 1986]

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