Fluid Inclusion Studies on Fluorite from Chumathang, Ladakh Himalaya

Authors

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

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.

Downloads

Download data is not yet available.

Metrics

Metrics Loading ...

Issue

Volume 24, Issue 6, June 1983

Section

Research Notes

Downloads

Published

1983-06-01

How to Cite

Patil, R. R., Choubey, V. M., & Sharma, K. K. (1983). Fluid Inclusion Studies on Fluorite from Chumathang, Ladakh Himalaya. Journal of Geological Society of India, 24(6), 311–313. Retrieved from https://geosocindia.com/index.php/jgsi/article/view/65362