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

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Fluid inclusion studies were carried out on the milky white vein qurtz intimately associated with Kolihan sulphide assemblage. The studies reveal that the deposition should have taken place at a temperature higher than 350°C and the ore-bearing solutions could have had a very high degree of salinity approaching the condition of a 'hydrosaline melt' with 33% NaCI and 17% KCl by weight.
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