Rameauite
| Rameauite | |
|---|---|
| General | |
| Category | Radioactive |
| References | [2][3][4] |
Rameauite is a hydrated complex
Crystallography
Rameauite has four observed forms which are {010}, {100}, {001} and {110}. The angles between these faces are {100}^{001} = 58°40' and {010}^{110} = 49° 50'. The crystals are always twinned on {100} and they are flattened parallel to {010}, and elongated parallel to {001}. The mineral rameauite is an example of a
monoclinic mineral and appears pseudo-hexagonal. I has unit cell dimensions of: a= 13.97, b= 14.26, c= 14.22 with β = 121.02°.[4][6]
Occurrence
It was first described in 1972 for an occurrence in the
Limousin, France and named after Jacques Rameau (1926–1960), French prospector at the "Commissariat à l'Energie Atomique", who discovered the deposit where the mineral occurs.[4][5]
In addition to the type locality in France it has been reported from the Orphan Mine on the south rim of the Grand Canyon in Arizona and on Rhyolite Ridge, Esmeralda County, Nevada.[5]
References
- S2CID 235729616.
- ^ "Rameauite Mineral Data".
- ^ "ATHENA - Pierre Perroud".
- ^ a b c d Handbook of Mineralogy
- ^ a b c Mindat.org
- ^ Cesbron, F., W.L. Brown, P. Bariand, and J. Geffroy (1972) Rameauite and agrinierite, two new hydrated complex uranyl oxides from Margnac, France. Mineralogical Magazine, 38, 781–789.