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Kukisvumite

A valid IMA mineral species
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About KukisvumiteHide

Formula:
Na6ZnTi4(Si8O24)O4 · 4H2O
Colour:
White to colorless, some grains with a silver tint
Lustre:
Vitreous
Hardness:
5½ - 6
Specific Gravity:
2.90
Crystal System:
Orthorhombic
Name:
Named for Mount Kukisvumchorr, Russia, the type locality.
The Zn analogue of manganokukisvumite and (the Zn0.5-analogue of) lintisite. AM-4 family of natural titanosilicates.

Compare the other two group members: eliseevite and punkaruaivite.


Unique IdentifiersHide

Mindat ID:
2283
Long-form identifier:
mindat:1:1:2283:1

IMA Classification of KukisvumiteHide

Classification of KukisvumiteHide

9.DB.20

9 : SILICATES (Germanates)
D : Inosilicates
B : Inosilicates with 2-periodic single chains, Si2O6; Pyroxene-related minerals
65.1.6.2

65 : INOSILICATES Single-Width,Unbranched Chains,(W=1)
1 : Single-Width Unbranched Chains, W=1 with chains P=2

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
KkiIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of KukisvumiteHide

Vitreous
Transparency:
Transparent
Colour:
White to colorless, some grains with a silver tint
Streak:
White
Hardness:
5½ - 6 on Mohs scale
Hardness:
VHN20=517 - 571 kg/mm2 - Vickers
Tenacity:
Elastic
Cleavage:
None Observed
Parting:
{010}
Fracture:
Irregular/Uneven, Splintery
Comment:
Crushes into thin fibers along the elongation
Density:
2.90 g/cm3 (Measured)    2.95 g/cm3 (Calculated)

Optical Data of KukisvumiteHide

Type:
Biaxial (-)
RI values:
nα = 1.676(3) nβ = 1.746(3) nγ = 1.795(3)
2V:
Measured: 77° , Calculated: 76°
Max. Birefringence:
δ = 0.119
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
weak
Pleochroism:
Non-pleochroic

Chemistry of KukisvumiteHide

Mindat Formula:
Na6ZnTi4(Si8O24)O4 · 4H2O
Element Weights:
Element% weight
O44.930 %
Si19.718 %
Ti16.803 %
Na12.105 %
Zn5.738 %
H0.708 %

Calculated from ideal end-member formula.
O
Si
Ti
Na
Zn
H
Common Impurities:
Nb,Fe,F

Crystallography of KukisvumiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Pccn
Setting:
Pccn
Cell Parameters:
a = 28.889(4) Å, b = 8.604(4) Å, c = 5.215(3) Å
Ratio:
a:b:c = 3.358 : 1 : 0.606
Unit Cell V:
1,296.25 ų (Calculated from Unit Cell)
Z:
2
Morphology:
Elongate [001], flattened [100], up to 7 mm long and 0.1 mm thick (type material)

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0011086KukisvumiteMerlino S, Pasero M, Ferro O (2000) The crystal structure of kukisvumite, Na6ZnTi4(Si2O6)4O4*4H2O Zeitschrift fur Kristallographie 215 352-3562000Kukisvumtschorr deposit, Khibiny alkaline massif, Kola peninsula, Russia0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
14.49 Å(90)
6.42 Å(60)
4.815 Å(80)
3.722 Å(65)
3.009 Å(100)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 4b: Highly evolved igneous rocks>3.0
35 : Ultra-alkali and agpaitic igneous rocks

Type Occurrence of KukisvumiteHide

General Appearance of Type Material:
Fan-shaped intergrowths of long prismatic crystals.
Place of Conservation of Type Material:
Fersman Mineralogical Museum, Moscow, Russia.
Mining Museum, St. Petersburg, Russia.
Geological Setting of Type Material:
Arfvedsonite-microcline pegmatite vein that cuts ijolitic/urtitic rocks.
Associated Minerals at Type Locality:

Synonyms of KukisvumiteHide

Other Language Names for KukisvumiteHide

German:Kukisvumit
Simplified Chinese:羟硅锌钛钠石
Spanish:Kukisvumita
Traditional Chinese:羥矽鋅鈦鈉石

Common AssociatesHide

Associations Based on Photo Data:
2 photos of Kukisvumite associated with ManganokukisvumiteNa6MnTi4(Si8O24)O4 · 4H2O
2 photos of Kukisvumite associated with ArfvedsoniteNaNa2(Fe2+4Fe3+)Si8O22(OH)2
2 photos of Kukisvumite associated with Labuntsovite Supergroup
1 photo of Kukisvumite associated with Nenadkevichite(Na,◻)8Nb4(Si4O12)2(O,OH)4 · 8H2O
1 photo of Kukisvumite associated with AegirineNaFe3+Si2O6

Related Minerals - Strunz-mindat GroupingHide

9.DB.05PotassiccarpholiteK(Mn2+,Li)2Al4Si4O12(OH,F)8Orth. mmm(2/m2/m2/m) : Ccca
9.DB.05CarpholiteMn2+Al2(Si2O6)(OH)4Orth. mmm(2/m2/m2/m) : Ccca
9.DB.05VanadiocarpholiteMn2+V3+Al(Si2O6)(OH)4Orth. mmm(2/m2/m2/m) : Ccca
9.DB.05MagnesiocarpholiteMgAl2Si2O6(OH)4Orth. mmm(2/m2/m2/m) : Ccca
9.DB.05FerrocarpholiteFe2+Al2Si2O6(OH)4Orth. mmm(2/m2/m2/m) : Ccca
9.DB.05BalipholiteBaLiMg2Al3(Si2O6)2(OH)4Orth. mmm(2/m2/m2/m) : Ccca
9.DB.10LorenzeniteNa2Ti2(Si2O6)O3Orth. mmm(2/m2/m2/m) : Pbcn
9.DB.15PunkaruaiviteLiTi2(HSi4O12)(OH)2 · H2OMon. 2/m : B2/b
9.DB.15LintisiteLiNa3Ti2(Si2O6)2O2 · 2H2OMon. 2/m : B2/b
9.DB.17EliseeviteLiNa1.5Ti2(H1.5Si4O12)O2 · 2H2OMon. 2/m : B2/b
9.DB.20ManganokukisvumiteNa6MnTi4(Si8O24)O4 · 4H2OOrth. mmm(2/m2/m2/m) : Pccn
9.DB.25VinogradoviteNa4Ti4(Si2O6)2[(Si,Al)4O10]O4 · (H2O,Na,K)3Mon. 2/m : B2/b
9.DB.25ParavinogradoviteNa1-2(Ti,Fe3+)4(Si2O6)2(AlSi3O10)(OH)4 · H2OTric. 1 : P1
9.DB.30NchwaningiteMn2+2(SiO3)(OH)2 · H2OOrth. mm2 : Pca21
9.DB.40ShattuckiteCu5(Si2O6)2(OH)2Orth. mmm(2/m2/m2/m)
9.DB.40'UM2005-31-SiO:CuH'Cu11(SiO4)(OH)18 · 9H2O (?)
9.DB.45Aerinite(Ca5.1Na0.5)(Fe3+,Al,Fe2+,Mg)4(Al,Mg)6[HSi12O36(OH)12][(CO3)1.2(H2O)12]Trig. 3m : P3c1
9.DB.50CapranicaiteKCaNaAl4B4Si2O18Mon. 2/m : P21/m

Other InformationHide

Notes:
Yellow-green luminescence in the electron microprobe beam
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for KukisvumiteHide

References for KukisvumiteHide

Localities for KukisvumiteHide

Showing 4 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
Russia
 
  • Murmansk Oblast
Min.Zhurnal (1991)
Pekov (1998)
Yakovenchuk et al. (2005)
...
 
and/or  
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