Čierna Lehota, okres Bánovce nad Bebravou, Trenčiansky kraj, Slovenská republika
The Ni-Bi-As mineralization is situated approximately 2 km SSE from the village Čierna Lehota. Mineralization is situated in a narrow zone of black shales and intensively graphitized rocks (graphitic-biotitic gneisses, graphitic metaquartzite).
References
- Mikuš T., Pršek J., Chovan M., Makovicky E., 2002: New type of hydrothermal mineralization in the Tatric tectonic unit (Western Carpathians): Ni-Bi-As mineral assemblage in the black shales. Geol. Carpath., 53, special issue. Proceedings of the XVII Congress of CBGA, Bratislava.
- Pršek J., Mikuš T., Makovicky E., Chovan M., 2005: Cuprobismutite, kupčíkite, hodrushite and associated sulfosalts from the black shale hosted Ni-Bi-As mineralization at Čierna Lehota, Slovakia. Eur. J. Mineral., 17, 155-162.
- Mikuš T. & Chovan M., 2007: Retgersit z Čiernej Lehoty(Strážovské vrchy). Mineralia Slovaca, 39, 3, 197-203.
External Links
http://www.schweizerbart.de/resources/downloads/paper_previews/56603.pdfMineral List
30 entries listed. 29 valid minerals.
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