Massive sulphide deposit, hosted in serpentinites and talc-carbonate metasomatic rocks replacing them.
Located about 20 km west of Gay.
References:
- Zaikov, V.V., and Melekestseva, I.Y. (2006): The Ishkinino Co-Cu Massive Sulfide Deposit Hosted in Ultramafic Rocks of the Main Ural Fault Zone, the Southern Urals. Geology of Ore Deposits 48(3), 151-174.
Mineral List:34 entries listed. 28 valid minerals.
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