Florencite-(Sm)
Florencite-(Sm) is a very rare mineral of the plumbogummite group (alunite supergroup) with simplified formula SmAl3(PO4)2(OH)6.[2] Samarium in florencite-(Sm) is substituted by other rare earth elements, mostly neodymium. It does not form separate crystals, but is found as zones in florencite-(Ce),[1] which is cerium-dominant member of the plumbogummite group.[3] Florencite-(Sm) is also a samarium-analogue of florencite-(La) (lanthanum-dominant) and waylandite (bismuth-dominant), both being aluminium-rich minerals.[2]
Florencite-(Sm) | |
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General | |
Category | Phosphate mineral |
Formula (repeating unit) | SmAl3(PO4)2(OH)6 |
Crystal system | Trigonal |
Crystal class | Hexagonal scalenohedral (3m) H-M symbol: (3 2/m) |
Space group | R3m |
Unit cell | a = 6.972, c = 16.182 [Å]; Z = 3 |
Identification | |
Color | Colorless, pale pink, pale yellow |
Crystal habit | Sub-mm zones in florencite-(Ce) crystals |
Cleavage | {0001}, distinct |
Fracture | Uneven |
Mohs scale hardness | 5.5-6 |
Luster | Vitreous to greasy |
Streak | White |
Density | 3.6 (measured) |
Optical properties | Uniaxal(+) |
Refractive index | nω=1.70, nε=1.71 |
References | [1]"Florencite-(Sm) - Handbook of Mineralogy" (PDF). Handbookofmineralogy.org. Retrieved 2016-03-08.[2] |
Occurrence and association
Florencite-(Sm) was revealed in quartz veins in the Maldynyrd Range, Subpolar Urals, Russia. It associates with xenotime-(Y).[1]
Notes on chemistry
Florencite-(Sm) has admixtures of neodymium, and small amounts of cerium, gadolinium, sulfur, strontium, praseodymium, calcium, lanthanum, europium, and silicon.[1]
References
- Repina, S.A., Popova, V.I., Churin, E.I., Belogub, E.V., and Khiller, V.V., 2014. Florencite-(Sm)—(Sm,Nd)Al3(PO4)2(OH)6: A new mineral species of the alunite-jarosite group from the Subpolar Urals. Geology of Ore Deposits 53(7), 564-574
- "Florencite-(Sm): Florencite-(Sm) mineral information and data". Mindat.org. Retrieved 2016-03-04.
- "Florencite-(Ce): Florencite-(Ce) mineral information and data". Mindat.org. Retrieved 2016-03-09.l