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Reddening of dune sands—evidence from southeast India

✍ Scribed by Rita A. M. Gardner


Book ID
102838428
Publisher
John Wiley and Sons
Year
1981
Tongue
English
Weight
874 KB
Volume
6
Category
Article
ISSN
0360-1269

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✦ Synopsis


Abstract

Thin section, SEM, and TEM analyses have indicated that the red ‘teri’ sands of southeast India have formed from weathering in situ of coastal dune sands. The data does not support a detrital origin for the red sands. C^14^ dates indicate that dune deposition and weathering, to a maximum depth of 10 m, leading to the formation of a hematite, koalinite and illite rich matrix has taken place rapidly over the past 25,000 years. It is postulated that garnet was a major source of hematite (ferric oxide).


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