Berggießhübel (Berggiesshübel), Bad Gottleuba-Berggießhübel, Erzgebirge, Sachsen, Deutschland
Magnetite-sulphide skarns, hosted in hornblende schists and andalusite-micaschists formed at the contact between a granite intrusion (Markersbach granite) and Silurian to Devonian clay schists and diabase tuffs. The lens-shaped skarn orebodies occur in NE- to WNW-trending swarms that can be traced over a distance of 3 km. In the past, they were worked by several mines.
References
- Palache, C., Berman, H., & Frondel, C. (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume II: 1084.
- Baumann, L., Kuschka, E., and Seifert, T. (2000): Lagerstätten des Erzgebirges. Enke (Stuttgart), 300 pp.
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