| Feklichevite | |
|---|---|
| General | |
| Category | Cyclosilicate |
|
Formula (repeating unit) | Na11Ca9(Fe3+,Fe2+)2Zr3Nb[Si25O73](OH,H2O,Cl,O)5 (original form) |
| IMA symbol | Fek [1] |
| Strunz classification | 9.CO.10 |
| Dana classification | 64.1.7. |
| Crystal system | Trigonal |
| Crystal class | Ditrigonal pyramidal (3m) H-M symbol: (3m) |
| Space group | R3m |
| Unit cell | a = 14.26, c = 30.17 [Å] (approximated); Z = 3 |
| Identification | |
| Color | Dark brown |
| Crystal habit | Isometric, thick-tabular; grains |
| Cleavage | (001), perfect |
| Tenacity | Brittle |
| Mohs scale hardness | 5.5 |
| Luster | Vitreous |
| Streak | Brownish |
| Diaphaneity | Transparent or translucent |
| Density | 2.87 (approximated) |
| Optical properties | Uniaxial (+) |
| Refractive index | nω = 1.61, nε = 1.61 (approximated) |
| Pleochroism | None |
| Ultraviolet fluorescence | No |
| Common impurities | Mn, F |
| References | [2] [3] |
Feklichevite is a rare mineral of the eudialyte group with the formula Na11Ca9(Fe3+,Fe2+)2Zr3NbSi(Si3O9)2(Si9O27)2. [3] [2] The original formula was extended to show the presence of cyclic silicate groups and presence of silicon at the M4 site, according to the nomenclature of eudialyte group. [4] When compared to other minerals of the group, feklichevite characterizes in the presence of ferric iron (thus similar to ikranite, mogovidite and fengchengite [2]) and dominance of calcium at the N4 site. Calcium is ordered in the structure and is also present at the M1 site. [3] [4] Other iron-bearing minerals of the group are eudialyte, ferrokentbrooksite, georgbarsanovite, khomyakovite, labyrinthite, oneillite and rastsvetaevite, but they rather contain ferrous iron [2] Feklichevite name honors Russian mineralogist and crystallographer, V. G. Feklichev. [3]
Occurrence and association
Feklichevite was found in cancrinite syenite vein of pegmatoid type, that occurs in the Kovdor alkaline massif, Kola Peninsula, Russia. Feklichevite coexists with aegirine- diopside, cancrinite, potassic feldspar, pectolite, titanite, hematite, and руrrhоtitе. [3]
Notes on chemistry
Feklichevite has quite high admixtures of manganese and fluorine, with minor hafnium, strontium, titanium, cerium, and lanthanum. [3]
References
- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode: 2021MinM...85..291W. doi: 10.1180/mgm.2021.43. S2CID 235729616.
- ^ a b c d Mindat, Feklichevite, http://www.mindat.org/min-11029.html
- ^ a b c d e f Pekov, I.V., Ekimenkova, I.A., Chukanov, N.V., Rastsvetaeva, R.K., Kononkova, N.N., Pekova, N.A., and Zadov, A.E., 2001. Feklichevite Na11Ca9(Fe3+,Fe2+)2Zr3Nb[Si25O73](OH,H2O,Cl,O)5, a new mineral of the eudialyte group from Kovdor Massif, Kola peninsula. Zapiski Vserossijskogo Mineralogicheskogo Obshchestva 130(3), 55–65
- ^ a b Johnsen, O., Ferraris, G., Gault, R.A., Grice, D.G., Kampf, A.R., and Pekov, I.V., 2003. The nomenclature of eudialyte-group minerals. The Canadian Mineralogist 41, 785–794
 | This article about a specific silicate mineral is a stub. You can help Wikipedia by expanding it. |
| Feklichevite | |
|---|---|
| General | |
| Category | Cyclosilicate |
|
Formula (repeating unit) | Na11Ca9(Fe3+,Fe2+)2Zr3Nb[Si25O73](OH,H2O,Cl,O)5 (original form) |
| IMA symbol | Fek [1] |
| Strunz classification | 9.CO.10 |
| Dana classification | 64.1.7. |
| Crystal system | Trigonal |
| Crystal class | Ditrigonal pyramidal (3m) H-M symbol: (3m) |
| Space group | R3m |
| Unit cell | a = 14.26, c = 30.17 [Å] (approximated); Z = 3 |
| Identification | |
| Color | Dark brown |
| Crystal habit | Isometric, thick-tabular; grains |
| Cleavage | (001), perfect |
| Tenacity | Brittle |
| Mohs scale hardness | 5.5 |
| Luster | Vitreous |
| Streak | Brownish |
| Diaphaneity | Transparent or translucent |
| Density | 2.87 (approximated) |
| Optical properties | Uniaxial (+) |
| Refractive index | nω = 1.61, nε = 1.61 (approximated) |
| Pleochroism | None |
| Ultraviolet fluorescence | No |
| Common impurities | Mn, F |
| References | [2] [3] |
Feklichevite is a rare mineral of the eudialyte group with the formula Na11Ca9(Fe3+,Fe2+)2Zr3NbSi(Si3O9)2(Si9O27)2. [3] [2] The original formula was extended to show the presence of cyclic silicate groups and presence of silicon at the M4 site, according to the nomenclature of eudialyte group. [4] When compared to other minerals of the group, feklichevite characterizes in the presence of ferric iron (thus similar to ikranite, mogovidite and fengchengite [2]) and dominance of calcium at the N4 site. Calcium is ordered in the structure and is also present at the M1 site. [3] [4] Other iron-bearing minerals of the group are eudialyte, ferrokentbrooksite, georgbarsanovite, khomyakovite, labyrinthite, oneillite and rastsvetaevite, but they rather contain ferrous iron [2] Feklichevite name honors Russian mineralogist and crystallographer, V. G. Feklichev. [3]
Occurrence and association
Feklichevite was found in cancrinite syenite vein of pegmatoid type, that occurs in the Kovdor alkaline massif, Kola Peninsula, Russia. Feklichevite coexists with aegirine- diopside, cancrinite, potassic feldspar, pectolite, titanite, hematite, and руrrhоtitе. [3]
Notes on chemistry
Feklichevite has quite high admixtures of manganese and fluorine, with minor hafnium, strontium, titanium, cerium, and lanthanum. [3]
References
- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode: 2021MinM...85..291W. doi: 10.1180/mgm.2021.43. S2CID 235729616.
- ^ a b c d Mindat, Feklichevite, http://www.mindat.org/min-11029.html
- ^ a b c d e f Pekov, I.V., Ekimenkova, I.A., Chukanov, N.V., Rastsvetaeva, R.K., Kononkova, N.N., Pekova, N.A., and Zadov, A.E., 2001. Feklichevite Na11Ca9(Fe3+,Fe2+)2Zr3Nb[Si25O73](OH,H2O,Cl,O)5, a new mineral of the eudialyte group from Kovdor Massif, Kola peninsula. Zapiski Vserossijskogo Mineralogicheskogo Obshchestva 130(3), 55–65
- ^ a b Johnsen, O., Ferraris, G., Gault, R.A., Grice, D.G., Kampf, A.R., and Pekov, I.V., 2003. The nomenclature of eudialyte-group minerals. The Canadian Mineralogist 41, 785–794
|
| This article about a specific silicate mineral is a stub. You can help Wikipedia by expanding it. |