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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
 
Creator Nair, R.R.
Hashimi, N.H.
 
Subject Geology and Geophysics
continental shelves
carbonates
sediments
mineralogy
ISW, India, West Coast
 
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
 
Date 1995-05-07T09:57:14Z
2017-09-29T13:48:44Z
1995-05-07T09:57:14Z
2017-09-29T13:48:44Z
1981
 
Type Journal Article
 
Identifier Marine Geology, vol.41; 1981; 309-319
0025-3227
http://drs.nio.org/drs/handle/2264/6729
 
Language en
 
Relation Mar Geol
SCI
 
Publisher Elsevier