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Arid-Humid Cycles in Mainland Gujarat over the Past 300 Ka: Evidence from the Mahi River Basin, India


Affiliations
1 Department of Geology, M.S. University of Baroda, Vadodara - 390 002, India
 

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A more or less complete conformable succession of sediments of Quaternary age is documented from the Mahl river basin. A description of the lithostratigraphy is accompanied by the palaeoclimatic inferences drawn on the basis of deduced depositional environments, which shows a remarkable broad correspondance with global climatic fluctuations.
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  • Arid-Humid Cycles in Mainland Gujarat over the Past 300 Ka: Evidence from the Mahi River Basin, India

Abstract Views: 163  |  PDF Views: 171

Authors

A. S. Khadkikar
Department of Geology, M.S. University of Baroda, Vadodara - 390 002, India
L. S. Chamyal
Department of Geology, M.S. University of Baroda, Vadodara - 390 002, India
J. N. Malik
Department of Geology, M.S. University of Baroda, Vadodara - 390 002, India
D. M. Maurya
Department of Geology, M.S. University of Baroda, Vadodara - 390 002, India
S. S. Merh
Department of Geology, M.S. University of Baroda, Vadodara - 390 002, India

Abstract


A more or less complete conformable succession of sediments of Quaternary age is documented from the Mahl river basin. A description of the lithostratigraphy is accompanied by the palaeoclimatic inferences drawn on the basis of deduced depositional environments, which shows a remarkable broad correspondance with global climatic fluctuations.