Flirscher Skihütte, Flirsch, Stanzer Tal, Nordtirol, Tirol, Österreich
Minor hydrothermal fahlore mineralisation in alpine sandstone/quartzite ('Alpiner Buntsandstein') about 30 m above the Flirsch ski hut.
Small, 3 m long adit and outcrop (high rock wall).
References
- KRAINER, K. (1982): Zur Sedimentologie und Vererzung der "Hangendquarzite" im Stanzer Tal / Arlberg (Tirol). Geol. Paläontol. Mitteilungen, Innsbruck, 12, 81-94.
- MOSTLER, H., KRAINER, K. & STINGL, V. (1982): Erzlagerstätten in der postvariszischen Trangressionsserie im Arlberggebiet. Arch. f. Lagerstättenforsch. Geol. B.-A., 2, 131-136.
- STINGL, V. (1982): Sedimentologie und Vererzung des Alpinen Verrucano im Stanzertal (Tirol). Geol. Paläont. Mitt. Innsbruck, 12, 71-80.
- HADITSCH, J. G. & KRAINER, K. (1993): Permoskytische Sandsteinvererzungen aus den Ost- und Südalpen Österreichs. Arch. f. Lagerstättenforsch. Geol. B.-A., 16, 13-28.
- J. Gröbner, U. Kolitsch, R. Poeverlein & M. Strasser (2009): Ein ungewöhnliches Fahlerzvorkommen bei der Flirscher Schihütte im Stanzer Tal, Tirol. Lapis 34, 13-19; 58.
Mineral List
38 entries listed. 36 valid minerals.
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