Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38348
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dc.contributor.authorReddy, N P C-
dc.contributor.authorRao, K Mohan-
dc.date.accessioned2016-12-09T04:59:28Z-
dc.date.available2016-12-09T04:59:28Z-
dc.date.issued1989-06-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38348-
dc.description128-130en_US
dc.description.abstractForty eight sediment samples, collected from 50-100m depth, have been analysed for their clay mineral composition and distribution. Kaolinite with chlorite (K + C) is the predominant mineral followed by illite and montmorillonite. K + C and illite appear to originate from the coastal red sediments and from the nearby Precambrian khondalites while montmorillonite is supplied by river Godavari from its drainage basin (Basaltic Deccan Traps) dispersed towards north by NE directed SW monsoon currents.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.18(2) [June 1989]en_US
dc.titleClay mineral distribution from Bhimunipatnam to Pudimadaka along central eastern continental shelf of Indiaen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.18(2) [June 1989]

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