Vein-type lead-zinc deposit, consisting of (1) several large NE-SW trending sulphide-dominated veins, up to 40 m thick and 13 km long, and (2) smaller baryte-fluorite dominated veins, up to 10 m thick, trending NE-SW and E-W. The veins are mainly hosted in Paleozoic rocks.
Photo: Zbynek Burival
This deposit has been operated by several french compagnies from 1923 to 1960.
32 entries listed. 27 valid minerals.
The above list contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.
- Jébrak, M., Marcoux, E., Masloubi, M., and Zaharaoui, M. (1998): From sandstone- to carbonate-hosted stratabound deposits: an isotope study of galena in the Upper-Moulouya District (Morocco). Mineralium Deposita 33, 406-415.
This page is currently not sponsored. To sponsor this page click here.