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Authors
Affiliations
1 Department of Geology, University of Rajasthan, Udaipur 313 001, IN
2 Department of Mines & Geology, Government of Rajasthan, Udaipur 313 001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 25, No 11 (1984), Pagination: 728-734
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.