Clay mineral distribution on tropical shelf: an example from the western shelf of India
DRS at CSIR-National Institute of Oceanography
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Title |
Clay mineral distribution on tropical shelf: an example from the western shelf of India
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Creator |
Hashimi, N.H.
Nair, R.R. |
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Subject |
Geology and Geophysics
grain size x-ray diffraction analysis distribution sediments continental slope continental shelves clay minerals ISW, India, Kerala |
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Description |
Seventy-five sediment samples collected from the Kerala continental shelf and slope during the 17th and 71st Cruises of RV Gaveshani were analysed by X-ray diffraction for clay mineral content. The distribution of total clay ( 4 mu fraction) indicates low percentages ( 10%) on the outer shelf and high percentages on the inner shelf (20 to 50%) and upper continental slope (11 to 47%). The clay minerals are composed of montmorillonite (smectite), kaolinite, illite and gibbsite and the non clay minerals are quartz and feldspar. Kaolinite and gibbsite have low values on the outer shelf and high values on the inner shelf and slope, while illite increases in the offshore direction. However, montmorillonite behaves differently from others in having high values on the outer shelf and low values on the inner shelf and slope. These variations in the clay mineral distribution have been attributed to differences in the energy of the various environments and due to size segregation of the minerals
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Date |
1995-12-15T10:01:55Z
2017-09-30T01:29:54Z 1995-12-15T10:01:55Z 2017-09-30T01:29:54Z 1989 |
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Type |
Journal Article
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Identifier |
Journal of Indian Association of Sedimentologists, vol.8; 1989; 17-27
0970-3268 http://drs.nio.org/drs/handle/2264/7163 |
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Language |
en
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Relation |
J Indian Assoc Sedimentol
Proc. 5 Convention; 1985 NON-SCI |
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Publisher |
Indian Association of Sedimentology
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