Mineralogy of the carbonate sediments - western continental shelf of India
DRS at CSIR-National Institute of Oceanography
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Title |
Mineralogy of the carbonate sediments - western continental shelf of India
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Creator |
Nair, R.R.
Hashimi, N.H. |
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Subject |
Geology and Geophysics
continental shelves carbonates sediments mineralogy ISW, India, West Coast |
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Description |
An X-ray diffraction study of forty-six sediment samples and three oolitic limestone samples from the western continental shelf of India shows that aragonite is the dominant carbonate mineral (99% maximum), followed by low-magnesium calcite (77% maximum), and high-magnesium calcite (39% maximum). MgCO3 in the high-magnesium calcite ranges from 5 to 21% (maximum in the limestone) with the most prominent mode at 13%, followed by lesser modes at 16, 9 and 6.5%. These modes are attributed to the presence of various organic constituents in the sediments and rocks. The sediments and the limestones are similar in mineralogy. Thus we conclude that no diagenetic change has taken place in the limestones after their formation
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Date |
1995-05-07T09:57:14Z
2017-09-29T13:48:44Z 1995-05-07T09:57:14Z 2017-09-29T13:48:44Z 1981 |
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Type |
Journal Article
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Identifier |
Marine Geology, vol.41; 1981; 309-319
0025-3227 http://drs.nio.org/drs/handle/2264/6729 |
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Language |
en
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Relation |
Mar Geol
SCI |
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Publisher |
Elsevier
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