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词条 Feklichevite
释义

  1. Occurrence and association

  2. Notes on chemistry

  3. References

{{infobox mineral
| name = Feklichevite
| category = Cyclosilicate
| image =
| imagesize =
| alt =
| caption =
| formula = Na11Ca9(Fe3+,Fe2+)2Zr3Nb[Si25O73](OH,H2O,Cl,O)5 (original form)
| strunz = 9.CO.10
| dana = 64.1.7.
| system = Trigonal
| class = Ditrigonal pyramidal (3m)
H-M symbol: (3m)
| symmetry = R3m
| unit cell = a = 14.26, c = 30.17 [Å] (approximated); Z = 3
| color = Dark brown
| colour =
| habit = isometric, thick-tabular; grains
| twinning =
| cleavage = (001), perfect
| fracture =
| tenacity = Brittle
| mohs = 5.5
| luster = Vitreous
| streak = Brownish
| diaphaneity = Transparent or Translucent
| gravity =
| density = 2.87 (approximated)
| polish =
| opticalprop = Uniaxial (+)
| refractive = nω=1.61, nε=1.61 (approximated)
| birefringence =
| pleochroism = None
| 2V =
| dispersion =
| extinction =
| length fast/slow =
| fluorescence = No
| absorption =
| melt =
| fusibility =
| diagnostic =
| solubility =
| impurities = Mn, F
| alteration =
| other =
| references = [1][2]
}}Feklichevite is a rare mineral of the eudialyte group with the formula Na11Ca9(Fe3+,Fe2+)2Zr3NbSi(Si3O9)2(Si9O27)2.[1][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.[3] 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.[1][3] 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.[1]

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.[1]

Notes on chemistry

Feklichevite has quite high admixtures of manganese and fluorine, with minor hafnium, strontium, titanium, cerium, and lanthanum.[1]

References

1. ^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
2. ^Mindat, Feklichevite, http://www.mindat.org/min-11029.html
3. ^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
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7 : Cyclosilicates|Sodium minerals|Calcium minerals|Iron minerals|Zirconium minerals|Niobium minerals|Trigonal minerals

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