Gold-bearing quartz (+/- calcite +/- scheelite) stringers and veins up to 4 m thick. The sulphide content of the lode is very low; sulphide grains are rarely of visually observable dimensions.
References
- Mishra, B., and Panigrahi, M.K. (1999): Fluid evolution in the Kolar Gold Field: evidence from fluid inclusion studies. Mineralium Deposita 34, 173-181.
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