Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

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The Continental Quaternary deposits of semi-arid central Gujarat consist of layered sequences of sediments of fluvio-marine, fluvial and aeolian origin. The deposits occupy structural depressions which are bounded by basement faults and provide an interesting record of neotectonism and climatic changes.

Keywords

Lithostratigraphy, Quaternary, Gujarat.
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