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Mineralogy and Genesis of Fluorite Deposits of Chandidongri, Madhya Pradesh


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1 Geology Section, Indian Institute of TechnoIogy, Bombay 400 076, India
     

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Fluorite occurs as replacement and cavity filling type in a shear zone traversing the Dongargarh granites where basic rocks' are encountered. This region is different in two ways: 1. presence of basic rocks in the shear zone and 2. absence of any calcareous type of rocks as compared to other fluorite occurrences like Ambadongar in Gujarat and Kahela-Mandokipal in Rajasthan. Fluorite, tysonite, borofluorite and yittrofluorite are the minerals identified. Geochemical studies combined with thermodynamic data throw a better light on the genesis of the fluorite deposits of this area which can be classified as low temperature hydrothermal.
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  • Mineralogy and Genesis of Fluorite Deposits of Chandidongri, Madhya Pradesh

Abstract Views: 176  |  PDF Views: 2

Authors

K. S. Balasubramaniam
Geology Section, Indian Institute of TechnoIogy, Bombay 400 076, India
J. S. Bhosale
Geology Section, Indian Institute of TechnoIogy, Bombay 400 076, India

Abstract


Fluorite occurs as replacement and cavity filling type in a shear zone traversing the Dongargarh granites where basic rocks' are encountered. This region is different in two ways: 1. presence of basic rocks in the shear zone and 2. absence of any calcareous type of rocks as compared to other fluorite occurrences like Ambadongar in Gujarat and Kahela-Mandokipal in Rajasthan. Fluorite, tysonite, borofluorite and yittrofluorite are the minerals identified. Geochemical studies combined with thermodynamic data throw a better light on the genesis of the fluorite deposits of this area which can be classified as low temperature hydrothermal.