[Newest Minerals] [Minerals for Sale] [Educational Articles] [About Us] [Image Gallery] John Betts - Fine Minerals Classic minerals, out-of-print books & magazines, plus informative articles for collectors General Kuzmenkoite-Zn InformationK2Zn(Ti,Nb)4(Si4O12)2(OH,O)4•6-8(H2O) |
Molecular Weight = 1,214.76 gm |
|
Potassium 4.76 % K 5.74 % K2O |
|
Barium 1.81 % Ba 2.02 % BaO |
|
Sodium 0.36 % Na 0.48 % Na2O |
|
Strontium 0.14 % Sr 0.17 % SrO |
|
Calcium 1.58 % Ca 2.22 % CaO |
|
Magnesium 0.02 % Mg 0.03 % MgO |
|
Titanium 10.68 % Ti 17.82 % TiO2 |
|
Manganese 1.63 % Mn 2.10 % MnO |
|
Niobium 8.87 % Nb 12.69 % Nb2O5 |
|
Aluminum 0.04 % Al 0.08 % Al2O3 |
|
Zinc 3.01 % Zn 3.75 % ZnO |
|
Iron 0.41 % Fe 0.53 % FeO |
|
Silicon 18.22 % Si 38.98 % SiO2 |
|
Hydrogen 1.56 % H 13.93 % H2O |
|
Oxygen 46.89 % O |
|
______ ______ |
|
100.00 % 100.55 % = TOTAL OXIDE |
K1.48Ca0.48Na0.19Ba0.16Sr0.02Zn0.56Mn2+0.36Fe2+0.09Mg0.01Ti2.71Nb1.162(Si3.94)2(Al0.01)
2(O11.85)(OH)2.19O1.41·8.3(H2O) |
Hydrothermal product in 3 pegmatites. May form pseudomorphs after murmanite. (labuntosovite group; structure) |
Approved IMA 2002 (Dana # Added) |
Mount Kedydverpakhk and Mount Krrnasurt, Lovozero massif, Kola Peninsula, Russia. Link to MinDat.org Location Data. |
Named for the Russian geochemist and mineralogist Maria V. Kuz'menko (1918-1995) and the Zn content. |
IMA2001-037 |
| | Search for Kuzmenkoite-Zn Images
|
|
| | Kuzmenkoite-Zn Crystallographya:b:c =1.0396:1:0.5617 |
a = 14.4, b = 13.851, c = 7.781, Z = 2; beta = 117.33° V = 1,378.72 Den(Calc)= 2.93 |
Monoclinic - DomaticH-M Symbol (m) Space Group: Cm |
By Intensity(I/Io): 3.19(1)(400,421,402), 3.09(0.91)(041,022), 6.92(0.75)(020,001),
6.4(0.5)(201,200), 2.49(0.35)(441,403), 2.58(0.35)(241), |
| Physical Properties of Kuzmenkoite-ZnNone |
Colorless, White, Grayish white, Pale pink, Light brown. |
2.78 - 2.87, Average = 2.82 |
Transparent to Translucent |
Brittle - Uneven - Very brittle fracture producing uneven fragments. |
Prismatic - Crystals Shaped like Slender Prisms (e.g. tourmaline). |
Pseudomorphous - Occurs in the form of another mineral. |
Vitreous (Glassy) |
white |
| Optical Properties of Kuzmenkoite-ZnCI meas= 0.035 (Excellent) - where the CI = (1-KPDmeas/KC) |
CI calc= 0.07 (Fair) - where the CI = (1-KPDcalc/KC) KPDcalc= 0.245,KPDmeas= 0.2541,KC= 0.2635 Ncalc = 1.73 - 1.77 Biaxial (+), a=1.68-1.683, b=1.686-1.688, g=1.783-1.787, bire=0.1030-0.1040, 2V(Calc)=28-30, 2V(Meas)=25. Dispersion dispersion not observed. |
| Calculated Properties of Kuzmenkoite-ZnBulk Density (Electron Density)=2.79 gm/cc |
note: Specific Gravity of Kuzmenkoite-Zn =2.83 gm/cc. Fermion Index = 0.02 |
Boson Index = 0.98 PEKuzmenkoite-Zn = 25.37 barns/electron |
U=PEKuzmenkoite-Zn x relectron= 70.70 barns/cc. |
GRapi = 67.78 (Gamma Ray American Petroleum Institute Units)
Estimated Radioactivity from Kuzmenkoite-Zn | Kuzmenkoite-Zn Classification60.01.03c.02 (60)Cyclosilicate Four-Membered Rings |
|
(60.01)as Titanosilicates |
|
(60.01.03c)Labuntsovite Group (Kuzmenkoite subgroup Monoclinic [C2/m]) |
|
|
|
|
09.CE.30c 09 - SILICATES (Germanates) |
|
09.C - Cyclosilicates |
|
09.CE -[Si4O12]8- 4-membered single rings (vierer-Einfachringe), |
|
|
|
|
|
|
|
|
|
| Other Kuzmenkoite-Zn InformationNAME( AmMin, v 88, p 932) PHYS. PROP.(AmMin, v 88, p 932) OPTIC PROP.(AmMin, v 88, p 932) |
Links to other databases for Kuzmenkoite-Zn : |
1 - Am. Min. Crystal Structure Database 2 - Athena 3 - GeoScienceWorld 4 - Google Images 5 - Google Scholar 6 - MinDAT 7 - Mineralienatlas (Deutsch) 8 - Online Mineral Museum 9 - QUT Mineral Atlas 10 - Ruff.Info Search for Kuzmenkoite-Zn using: Visit our Advertisers for Kuzmenkoite-Zn : B & L Fine MineralsDan Weinrich Fine Minerals Dan Weinrich Auctions Dakota Matrix Excalibur Minerals Exceptional Minerals Fabre Minerals John Betts Fine Minerals Lapis Mineral Journal Mineral News UV Tools Wrights Rock Shop Translate Kuzmenkoite-Zn Mineral Data : Ask about Kuzmenkoite-Zn here : Print or Cut-and-Paste your Kuzmenkoite-Zn Specimen Label here :
| |
|
| | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||