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Clay minerals in identification of provenance of sediments of Mandovi estuary, Goa, west coast of India

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Title Clay minerals in identification of provenance of sediments of Mandovi estuary, Goa, west coast of India
 
Creator Bukhari, S. S.
Nayak, G. N.
 
Description 341-345
Relative abundance and spatial distribution of the clay minerals show considerable variation with changing seasons all along the length of the Mandovi estuary. Kaolinite, illite, montmorillonite and gibbsite have been identified as chief clay minerals in both the suspended sediments and the surface bed sediments. Of all the minerals, kaolinite is the most dominant. Kaolinite and gibbsite predominantly have their origin in the laterites and lateritic soil. Illite originates basically from the metasediments, while majority of montmorillonite is brought in from the offshore.
 
Date 2016-11-18T11:30:29Z
2016-11-18T11:30:29Z
1996-12
 
Type Article
 
Identifier 0975-1033 (Online); 0379-5136 (Print)
http://nopr.niscair.res.in/handle/123456789/37148
 
Language en_US
 
Rights CC Attribution-Noncommercial-No Derivative Works 2.5 India
 
Source IJMS Vol.25(4) [December 1996]