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.
References
- Pribitzer, F. (1956): Die Minerallagerstätte Zinkwand bei Schladming in Steiermark (Österreich). Aufschluss, 7 (3), 59-63.
- A. Strasser: Die Minerale Salzburgs (1989)
- Taucher, J. & Hollerer, C.E. (1994): Phaunouxit und Rauenthalit von der Co-Ni-Lagerstätte Zinkwand-Vöttern, Schladminger Tauern, Steiermark. Matrixx 3, 69-72.
- Kolitsch, U. & Brandstätter, F. (2008): 1557: Ullmannit von der Zinkwand, Schladminger Tauern, Steiermark. In: Niedermayr, G. et al. (2008): Neue Mineralfunde aus Österreich LVII. Carinthia II, 198/118, 262.
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