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

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Geology of Karara Volcanic Vent, Rajasthan


Affiliations
1 Department of Geology, University of Rajasthan, Udaipur 313 001, India
2 Department of Mines & Geology, Government of Rajasthan, Udaipur 313 001, India
     

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Fluorspar veins in Karara area occur in a variety of pyroclastic and flow rocks. represented by volcanic breccias, lapilli tuffs, and welded tuffs including ignimbrite. Lavas produced are of the nature of basalt. andesite, trachyte, dacite, and rhyolite along with their border line varieties.
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  • Geology of Karara Volcanic Vent, Rajasthan

Abstract Views: 153  |  PDF Views: 5

Authors

P. S. Ranawat
Department of Geology, University of Rajasthan, Udaipur 313 001, India
R. S. Dashora
Department of Mines & Geology, Government of Rajasthan, Udaipur 313 001, India

Abstract


Fluorspar veins in Karara area occur in a variety of pyroclastic and flow rocks. represented by volcanic breccias, lapilli tuffs, and welded tuffs including ignimbrite. Lavas produced are of the nature of basalt. andesite, trachyte, dacite, and rhyolite along with their border line varieties.