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

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Fluid Inclusion Studies on Fluorite from Chumathang, Ladakh Himalaya


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1 Wadia Institute of Himalayan Geology, Dehra Dun 248001, India
 

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Study indicates low salinity and moderate density for the ore forming fluids responsible for the fluorite. The temperature of homogenisation (120°C to 150°C) in different coloured fluorites indicate that the mineralization is of epithermal type.
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  • Fluid Inclusion Studies on Fluorite from Chumathang, Ladakh Himalaya

Abstract Views: 189  |  PDF Views: 137

Authors

R. R. Patil
Wadia Institute of Himalayan Geology, Dehra Dun 248001, India
Vinay M. Choubey
Wadia Institute of Himalayan Geology, Dehra Dun 248001, India
Kewal K. Sharma
Wadia Institute of Himalayan Geology, Dehra Dun 248001, India

Abstract


Study indicates low salinity and moderate density for the ore forming fluids responsible for the fluorite. The temperature of homogenisation (120°C to 150°C) in different coloured fluorites indicate that the mineralization is of epithermal type.