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Telyushenkoite

A valid IMA mineral species
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About TelyushenkoiteHide

Formula:
(Cs,Na,K)Na6[Be2Al3Si15O39]F2
Colour:
Colourless to white
Lustre:
Vitreous
Hardness:
6
Specific Gravity:
2.73
Crystal System:
Trigonal
Member of:
Name:
Honouring Tamara Matveyevna Telyushenko (Тамара Матвеевна Телюшенко) (1930 - 19 January 1997), Professor of Petrography in the Ashkhabad School of Geology.
Leifite Group.
The cesium analogue of leifite and eirikite.


Unique IdentifiersHide

Mindat ID:
25600
Long-form identifier:
mindat:1:1:25600:3

IMA Classification of TelyushenkoiteHide

Classification of TelyushenkoiteHide

9.EH.25

9 : SILICATES (Germanates)
E : Phyllosilicates
H : Transitional structures between phyllosilicate and other silicate units

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

Physical Properties of TelyushenkoiteHide

Vitreous
Transparency:
Transparent
Colour:
Colourless to white
Streak:
White
Hardness:
Hardness:
VHN100=696 - 737 kg/mm2 - Vickers
Cleavage:
Distinct/Good
Density:
2.73 g/cm3 (Measured)    2.73 g/cm3 (Calculated)

Optical Data of TelyushenkoiteHide

Type:
Uniaxial (+)
RI values:
nω = 1.526(2) nε = 1.531(2)
Max. Birefringence:
δ = 0.005
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:
None to Very Low
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 uniaxial interference figure - the conoscopic (convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis centred and vertical. The coloured rings are isochromatics, computed with the same physics as the Michel-Lévy bar above; the dark cross is the isogyre.

For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.

Chemistry of TelyushenkoiteHide

Mindat Formula:
(Cs,Na,K)Na6[Be2Al3Si15O39]F2
Element Weights:
Element% weight
O42.942 %
Si28.993 %
Na9.493 %
Cs9.147 %
Al5.571 %
F2.615 %
Be1.240 %

Calculated from ideal end-member formula.
O
Si
Na
Cs
Al
F
Be
Common Impurities:
Zn

Crystallography of TelyushenkoiteHide

Crystal System:
Trigonal
Class (H-M):
3m(32/m) - Hexagonal Scalenohedral
Space Group:
P31m
Setting:
P31m
Cell Parameters:
a = 14.377 Å, c = 4.878 Å
Ratio:
a:c = 1 : 0.339
Unit Cell V:
873.19 ų (Calculated from Unit Cell)
Z:
1
Morphology:
Equant grains to 2 cm.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0005761TelyushenkoiteSokolova E V, Huminicki D M C, Hawthorne F C, Agakhanov A A, Pautov L A, Grew E S (2002) The crystal chemistry of telyushenkoite and leifite, A Na6[Be2Al3Si15O39F2], A = Cs, Na The Canadian Mineralogist 40 183-19220020293
CIF Raw Data - click here to close

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 TelyushenkoiteHide

General Appearance of Type Material:
Angular grains to 2 cm.
Place of Conservation of Type Material:
A.E. Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia.
Geological Setting of Type Material:
Inclusions in coarse-grained blocks consisting mainly of reedmergnerite.
Associated Minerals at Type Locality:

Synonyms of TelyushenkoiteHide

Other Language Names for TelyushenkoiteHide

Simplified Chinese:氟铍硅铯钠石
Traditional Chinese:氟鈹矽銫鈉石

Relationship of Telyushenkoite to other SpeciesHide

Member of:
Other Members of Leifite Group:
EirikiteKNa6Be2(Si15Al3)O39F2Trig. 3m(32/m) : P3m1
Leifite(Na,H2O)Na6[Be2Al2(Al,Si)Si15O39]F2Trig. 3m : P3m1

Common AssociatesHide

Associations Based on Photo Data:
6 photos of Telyushenkoite associated with ReedmergneriteNaBSi3O8
5 photos of Telyushenkoite associated with ShibkoviteK(◻K)Ca2Zn3[Si12O30]
1 photo of Telyushenkoite associated with Moskvinite-(Y)Na2KYSi6O15
1 photo of Telyushenkoite associated with MiseriteK1.5-x(Ca,Y,REE)5(Si6O15)(Si2O7)(OH,F)2 · yH2O
1 photo of Telyushenkoite associated with PectoliteNaCa2Si3O8(OH)
1 photo of Telyushenkoite associated with AegirineNaFe3+Si2O6

Related Minerals - Strunz-mindat GroupingHide

9.EH.05ManganoneptuniteKNa2Li(Mn2+)2Ti2[Si4O12]2Mon. m : Bb
9.EH.05MagnesioneptuniteKNa2Li(Mg)2Ti2[Si4O12]2Mon. 2/m : B2/b
9.EH.05NeptuniteKNa2Li(Fe2+)2Ti2[Si4O12]2Mon. m : Bb
9.EH.05WatatsumiiteKNa2Li(Mn2+)2V4+2[Si4O12]2Mon. m : Bb
9.EH.05RotherkopfiteKNa2Fe2+(Fe2+)2(Ti1.5Fe2+0.5)[Si4O12]2Mon. 2/m : B2/b
9.EH.10GrumantiteNa(HSi2O5) · H2OOrth. mm2 : Fdd2
9.EH.15SarcoliteNa4Ca12Al8Si12O46(SiO4,PO4)(OH,H2O)4(CO3,Cl)Tet. 4/m : I4/m
9.EH.20UssingiteNa2AlSi3O8OHTric. 1 : P1
9.EH.25Leifite(Na,H2O)Na6[Be2Al2(Al,Si)Si15O39]F2Trig. 3m : P3m1
9.EH.25EirikiteKNa6Be2(Si15Al3)O39F2Trig. 3m(32/m) : P3m1
9.EH.30NafertisiteNa3Fe2+10Ti2(Si6O17)2O2(OH)6F(H2O)2Mon. 2/m
9.EH.35VebleniteKNa(Fe2+5Fe3+4Mn7)Nb4(Si2O7)2(Si8O22)2O6(OH)10(H2O)3 Tric. 1 : P1

Fluorescence of TelyushenkoiteHide

Weak lilac fluorescence in short-wave UV light.

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 TelyushenkoiteHide

References for TelyushenkoiteHide

Localities for TelyushenkoiteHide

Showing 1 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.
Tajikistan (TL)
 
  • Districts of Republican Subordination
Agakhanov et al. (2003) +1 other reference
 
and/or  
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