Uranium deposit in Karlovarský (Carlsbad) Massif. The mineralization is connected with short ruptures filled with rock breccia, limonite, hematite and rarely quartz. Thickness of those zones was usually 5-20 cm, close to surface up to 1 m. No primary U-mineralization is known. The deposit was found in 1962 and mining activities ceased after the upper 35 m of the deposit were exhausted.
Uranium mineralization.
References
- Černý, P.: Ložisko uranu Nový Fojtov. Minerál, 2004, roč. 12, č. 6, s. 435-437.
Mineral List
6 entries listed. 5 valid minerals.
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