(Zinkwand, Obertal, Schladminger Tauern, Schladming, Steiermark, Österreich)
Polygene deposit with vein-type Bi-Co-Ni mineralizations near the intersection of fault zones in amphibolites, gneisses and micaschists with sulphide- and arsenide-bearing strata. The deposit was worked from both the Styrian and the Salzburgian side, and the material on the dumps on both sides originates from both provinces as well.
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Map Reference: 47°16'N , 13°41'E
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54 entries listed. 48 valid minerals.
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