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

Authors

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

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.

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Issue

Volume 47, Issue 3, March 1996

Section

Short Communications

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Published

1996-03-01

How to Cite

Khadkikar, A. S., Chamyal, L. S., Malik, J. N., Maurya, D. M., & Merh, S. S. (1996). Arid-Humid Cycles in Mainland Gujarat over the Past 300 Ka: Evidence from the Mahi River Basin, India. Journal of Geological Society of India, 47(3), 383–388. Retrieved from http://www.geosocindia.com/index.php/jgsi/article/view/68215

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