Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/39170
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dc.contributor.authorRao, A T-
dc.contributor.authorRaman, C V-
dc.date.accessioned2016-12-26T06:28:21Z-
dc.date.available2016-12-26T06:28:21Z-
dc.date.issued1979-03-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/39170-
dc.description38-40en_US
dc.description.abstractRed sediments of recent age are commonly seen in association with the khondalite hill ranges and also found towards the coast in Visakhapatnam District, Andhra Pradesh, India. These red sediments comprise sand (quartz + heavies), silt and clay. X-ray data on clays reveal that kaolinite (70-94%) and illite (6-22%) are the dominant types in the red sediments. Smectite and chlorite are rare. Variation of clay mineral percentages in the red sediments is due to varying amounts of altered detrital sillimanite and orthoclase derived from the khondalites. The clays from the inner shelf have considerable proportion of illite and kaolinite along Visakhapatnam Coast, which indicates that the fluvial input of clays from the red sediments and lateritic soils is significant.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.08(1) [March 1979]en_US
dc.titleClay input from the red sediments of Visakhapatnam Coasten_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.08(1) [March 1979]

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