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Punkaruaivite

A valid IMA mineral species
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About PunkaruaiviteHide

Formula:
LiTi2(HSi4O12)(OH)2 · H2O
Colour:
brownish yellow to colorless
Lustre:
Vitreous
Hardness:
Specific Gravity:
2.60
Crystal System:
Monoclinic
Name:
Named for Mt. Punkaruaiv, the type locality in the Lovozero massif, Kola Peninsula, Russia.
Related to lintisite, eliseevite; and kukisvumite and manganokukisvumite.

AM-4 family of natural titanosilicates.


Unique IdentifiersHide

Mindat ID:
38697
Long-form identifier:
mindat:1:1:38697:9

IMA Classification of PunkaruaiviteHide

Classification of PunkaruaiviteHide

9.DB.15

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

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

Physical Properties of PunkaruaiviteHide

Vitreous
Transparency:
Transparent, Translucent
Colour:
Brownish yellow to colorless
Streak:
White
Hardness:
4½ on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
{100}
Fracture:
Step-Like
Density:
2.60(5) g/cm3 (Measured)    2.55 g/cm3 (Calculated)

Optical Data of PunkaruaiviteHide

Type:
Biaxial (-)
RI values:
nα = 1.658(2) nβ = 1.696(2) nγ = 1.726(5)
2V:
Measured: 85° (5), Calculated: 82°
Max. Birefringence:
δ = 0.068
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:
none
Pleochroism:
Weak
Comments:
Y light brownish yellow, X brownish yellow

Chemistry of PunkaruaiviteHide

Mindat Formula:
LiTi2(HSi4O12)(OH)2 · H2O
Element Weights:
Element% weight
O52.167 %
Si24.420 %
Ti20.810 %
Li1.509 %
H1.096 %

Calculated from ideal end-member formula.
O
Si
Ti
Li
H

Crystallography of PunkaruaiviteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/b
Setting:
C2/c
Cell Parameters:
a = 26.68 Å, b = 8.75 Å, c = 5.24 Å
β = 91.2°
Ratio:
a:b:c = 3.049 : 1 : 0.599
Unit Cell V:
1,223.01 ų (Calculated from Unit Cell)
Z:
4

X-Ray Powder DiffractionHide

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 PunkaruaiviteHide

General Appearance of Type Material:
well-shaped prismatic crystals flattened on (100) and elongate along [001] arranged in
sheaf-like and radiating aggregates.
Place of Conservation of Type Material:
Mineralogical Museum of the St. Petersburg State University (Russia) and the Geological and the Mineralogical Museum of the Geological Institute of the Kola Science Centre of the Russian Academy of Sciences (Apatity, Russia, No. 6441).
Geological Setting of Type Material:
ussingite - aegirine - microcline vein in nepheline syenite.
Rare late-stage hydrothermal minerals formed as a result of the alteration of earlier titanosilicates
Associated Minerals at Type Locality:

Synonyms of PunkaruaiviteHide

Other Language Names for PunkaruaiviteHide

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.15LintisiteLiNa3Ti2(Si2O6)2O2 · 2H2OMon. 2/m : B2/b
9.DB.17EliseeviteLiNa1.5Ti2(H1.5Si4O12)O2 · 2H2OMon. 2/m : B2/b
9.DB.20KukisvumiteNa6ZnTi4(Si8O24)O4 · 4H2OOrth. mmm(2/m2/m2/m) : Pccn
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

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 PunkaruaiviteHide

References for PunkaruaiviteHide

Localities for PunkaruaiviteHide

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 (TL)
 
  • Murmansk Oblast
Yakovenchuk et al. (2010) +1 other reference
    • Lovozersky District
Yakovenchuk et al. (2010)
IMA website - Proposals approved in ... +1 other reference
Pekov et al. (2013)
 
and/or  
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