Clay mineral distribution on the Kerala continental shelf and slope
DRS at CSIR-National Institute of Oceanography
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Title |
Clay mineral distribution on the Kerala continental shelf and slope
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Creator |
Rao, V.P.
Nair, R.R. Hashimi, N.H. |
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Subject |
Geology and Geophysics
clay minerals continental shelves continental slope sediments distribution X ray diffraction analysis grain size 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 @iRV gaveshani@@ were analysed by X-ray diffraction for clay mineral cntent. The distribution of total clay (< 4~k 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 montomorillonite (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 |
1997-11-28T10:01:00Z
2017-09-29T13:48:35Z 1997-11-28T10:01:00Z 2017-09-29T13:48:35Z 1983 |
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Type |
Journal Article
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Identifier |
Journal of the Geological Society of India, vol.24; 1983; 540-546
0016-7622 http://drs.nio.org/drs/handle/2264/6509 |
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Language |
en
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Relation |
J Geol Soc India
SCI |
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Publisher |
Geological Society of India
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