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A Note on the Structure of the Area Around Dughda, Chhotaudepur Taluka, Baroda District, Gujarat


Affiliations
1 Department of Geology, M. S. University of Baroda, Baroda 390002, India
 

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Bagh beds and Deccan Traps are the main formations exposed in Dughda area. These exposures are controlled by numerous fractures formed due to tectonic activity along the Narmada lineament. The contact between Bagh beds and Deccan Traps is characterised by pyroclastic rocks and tuffaceous beds.
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  • A Note on the Structure of the Area Around Dughda, Chhotaudepur Taluka, Baroda District, Gujarat

Abstract Views: 165  |  PDF Views: 203

Authors

R. V. Karanth
Department of Geology, M. S. University of Baroda, Baroda 390002, India
A. G. Rao
Department of Geology, M. S. University of Baroda, Baroda 390002, India
J. M. Patel
Department of Geology, M. S. University of Baroda, Baroda 390002, India

Abstract


Bagh beds and Deccan Traps are the main formations exposed in Dughda area. These exposures are controlled by numerous fractures formed due to tectonic activity along the Narmada lineament. The contact between Bagh beds and Deccan Traps is characterised by pyroclastic rocks and tuffaceous beds.