Uraninite veins in red Permian clay schists, deposit situated around 7 km SSE of Lodève.
Heavy concentrations of massive pitchblende at the intersection of fractures affecting Saxonian red pelites, or in impregnations of sediments near the faults.
Refs.: (in part):
- Min.Rec.: 24:463-467 (1993).
- Eur. J. Mineral., 1993, 5, 873-877.
- Caubel A. (1997), Minéralogie du gisement d'uranium de Rabejac (Hérault), Le Règne Minéral, n° 13, 5-18
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Map Reference: 43°44'N , 3°19'E
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