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Odintsovite

A valid IMA mineral species
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About OdintsoviteHide

02419230017271928945100.jpg
Prof. M. M. Odintsov
Formula:
K2Na4Ca3Ti2Be4Si12O38
Colour:
Colorless, light pink, pink with a brownish hue, tan colored
Lustre:
Vitreous
Hardness:
5 - 5½
Specific Gravity:
2.94 - 2.98
Crystal System:
Orthorhombic
Name:
Named in honor of Mikhail Mikhailovich Odintsov (Михаил Михайлович Одинцов) (23 October (5 November) 1911, Irkutsk, Russian Empire - 12 March 1980, Irkutsk, USSR), geologist, director of the Institute of the Earth's Crust in Irkutsk, and a participant in the discovery of the Siberian Diamond Province.
Unique combination of elements. Also one of very few mineral species known to combine titanium and beryllium.

The Na analogue of nakkaalaaqite.


Unique IdentifiersHide

Mindat ID:
7200
Long-form identifier:
mindat:1:1:7200:3

IMA Classification of OdintsoviteHide

Classification of OdintsoviteHide

9.CJ.50

9 : SILICATES (Germanates)
C : Cyclosilicates
J : [Si6O18]12- 6-membered single rings (sechser-Einfachringe), without insular complex anions
61.1.5.1

61 : CYCLOSILICATES Six-Membered Rings
1 : Six-Membered Rings with [Si6O18] rings; possible (OH) and Al substitution

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

Physical Properties of OdintsoviteHide

Vitreous
Transparency:
Transparent, Translucent
Colour:
Colorless, light pink, pink with a brownish hue, tan colored
Hardness:
5 - 5½ on Mohs scale
Cleavage:
None Observed
Density:
2.94 - 2.98 g/cm3 (Measured)    2.91 g/cm3 (Calculated)

Optical Data of OdintsoviteHide

Type:
Biaxial (+)
RI values:
nα = 1.630(3) nβ = 1.644 nγ = 1.675(3)
2V:
Measured: 70°
Max. Birefringence:
δ = 0.045
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:
Moderate
Dispersion:
r > v

Chemistry of OdintsoviteHide

Mindat Formula:
K2Na4Ca3Ti2Be4Si12O38
Element Weights:
Element% weight
O44.470 %
Si24.651 %
Ca8.794 %
Ti7.002 %
Na6.726 %
K5.720 %
Be2.637 %

Calculated from ideal end-member formula.

Chemical AnalysisHide

Oxide wt%:
 12
Na2O6.33 %8.57 %
K2O6.83 %6.86 %
Li2O0.98 %0.10 %
CaO12.93 %11.51 %
BeO7.15 %6.75 %
Al2O30.15 %0.11 %
Fe2O32.27 %
TiO27.06 %11.42 %
SiO251.02 %52.56 %
Nb2O53.73 %
FeO0.42 %
SrO1.21 %
MnO0.05 %
Total:98.45 %99.56 %
Empirical formulas:
Sample IDEmpirical Formula
1K2.03Li0.92(Na2.85Ca1.23)Σ4.08Ca2(Ti1.24Fe3+0.40Nb0.39)Σ2.03Be4(Si11.88Al0.04)Σ11.92O38

Crystallography of OdintsoviteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Fddd
Setting:
Fddd
Cell Parameters:
a = 12.778(4) Å, b = 14.343(3) Å, c = 33.69(1) Å
Ratio:
a:b:c = 0.891 : 1 : 2.349
Unit Cell V:
6174 ų
Z:
8
Morphology:
Flat fanshaped, wheelshaped arrgegates.
Platy on {001}.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0012499OdintsoviteRastsvetaeva R K, Evsyunin V G, Kashaev A A (1995) Crystal structure of a new representative of ring silicates Doklady Chemistry 340 49-5119950293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
9.23 Å(90)
4.15 Å(10)
3.30 Å(100)
3.16 Å(100)
2.53 Å(100)
2.42 Å(100)
1.668 Å(80)
1.6 32 Å(80)
1.582 Å(90)
1.309 Å(80)

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 OdintsoviteHide

Synonyms of OdintsoviteHide

Other Language Names for OdintsoviteHide

Common AssociatesHide

Associations Based on Photo Data:
5 photos of Odintsovite associated with AegirineNaFe3+Si2O6
2 photos of Odintsovite associated with MicroclineK(AlSi3O8)
2 photos of Odintsovite associated with KalsiliteKAlSiO4
1 photo of Odintsovite associated with TitaniteCaTiO(SiO4)
1 photo of Odintsovite associated with K Feldspar

Related Minerals - Strunz-mindat GroupingHide

9.CJ.ZolotareviteNa5Zr[Si6O15(OH)3] · 3H2OTrig. 3m(32/m) : R3m
9.CJ.'Avdeevite'NaAl4(Be5Li)(Si6O18)2(H2O)1-2Hex. 6/mmm(6/m2/m2/m) : P63/mmc
9.CJ.'Beryllocordierite-Na'NaMg4(Al5Be)(AlSi5O18)2 · 2H2OOrth. mmm(2/m2/m2/m) : Cccm
9.CJ.SachanbińskiiteNaMn4(Al5Be)(AlSi5O18)2 · 2H2OOrth. mmm(2/m2/m2/m) : Cccm
9.CJ.NakkaalaaqiteK2[Na3Ca]LiCa2Ti2Be4Si12O38Orth. mmm(2/m2/m2/m) : Fddd
9.CJ.05Johnkoivulaite-(Cs)Cs[Be2B]Mg2Si6O18Hex. 6/mmm(6/m2/m2/m) : P6/mcc
9.CJ.05BerylBe3Al2(Si6O18)Hex. 6/mmm(6/m2/m2/m) : P6/mcc
9.CJ.05BazziteBe3Sc2(Si6O18)Hex. 6/mmm(6/m2/m2/m) : P6/mcc
9.CJ.05Ferroindialite(Fe2+,Mg)2Al4Si5O18Hex. 6/mmm(6/m2/m2/m) : P6/mcc
9.CJ.05 va'Vorobyevite'Be3Al2(Si6O18)
9.CJ.05StoppaniiteBe3Fe3+2(Si6O18) · H2OHex. 6/mmm(6/m2/m2/m) : P6/mcc
9.CJ.05IndialiteMg2Al3(AlSi5O18)Hex. 6/mmm(6/m2/m2/m) : P6/mcc
9.CJ.10SekaninaiteFe2+2Al4Si5O18Orth. mmm(2/m2/m2/m) : Cccm
9.CJ.10CordieriteMg2Al4Si5O18Orth. mmm(2/m2/m2/m) : Cccm
9.CJ.15aZirsinaliteNa6(Ca,Mn2+,Fe2+)Zr(Si6O18)Trig. 3m(32/m) : R3m
9.CJ.15aKapustiniteNa6ZrSi6O16(OH)2Mon. 2/m : B2/m
9.CJ.15aTownenditeNa8ZrSi6O18Trig. 3m(32/m) : R3m
9.CJ.15aCombeiteNa4.5Ca3.5Si6O17.5(OH)0.5Trig. 3m(32/m) : R3m
9.CJ.15aKazakoviteNa6Mn2+Ti(Si6O18)Trig. 3m(32/m) : R3m
9.CJ.15aTisinaliteNa3H3(Mn,Ca,Fe)TiSi6(O,OH)18 · 2H2OTrig. 3m(32/m)
9.CJ.15aLovozeriteNa2Ca(Zr,Ti)(Si6O12)[(OH)4O2] · H2OTrig. 3 : R3
9.CJ.15aLitvinskiteNa2(◻,Na,Mn)ZrSi6O12(OH,O)6Mon. m : Bm
9.CJ.15cKoashviteNa6(Ca,Mn)(Ti,Fe)Si6O18 · H2OOrth. mmm(2/m2/m2/m)
9.CJ.15bImandriteNa12Ca3Fe3+2(Si6O18)2Orth. mmm(2/m2/m2/m)
9.CJ.25BaratoviteKCa7(Ti,Zr)2Li3Si12O36F2Mon. 2/m : B2/b
9.CJ.25AleksandroviteKCa7Sn2Li3Si12O36F2Mon. 2/m : B2/b
9.CJ.25KatayamaliteKLi3Ca7Ti2(SiO3)12(OH)2Mon. 2/m : B2/b
9.CJ.30DioptaseCuSiO3 · H2OTrig. 3 : R3
9.CJ.35KostyleviteK2Zr(Si3O9) · H2OMon. 2/m : P21/b
9.CJ.40PetarasiteNa5Zr2(Si6O18)(Cl,OH) · 2H2OMon. 2/m : P21/m
9.CJ.45Gerenite-(Y)(Ca,Na)2(Y,REE)3Si6O18 · 2H2OTric. 1 : P1
9.CJ.55MathewrogersitePb7FeAl3GeSi12O36(OH,H2O)6Trig.
9.CJ.60Pezzottaite-(Cs)Cs(Be2Li)Al2(Si6O18)Trig. 3 : R3

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 0.0000% 0 α, β, γ
Thorium (Th) 0.0000% 0 α, β, γ
Potassium (K) 5.7196% 1,773 β, γ

For comparison:

  • Banana: ~15 Bq per fruit
  • Granite: 1,000–3,000 Bq/kg
  • EU exemption limit: 10,000 Bq/kg

Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.

Interactive Simulator:

Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!

Activity:

DistanceDose rateRisk
1 cm
10 cm
1 m

The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).

D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield

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 OdintsoviteHide

References for OdintsoviteHide

Reference List:

Localities for OdintsoviteHide

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.
Greenland
 
  • Kujalleq
Petersen (2001)
Petersen et al. (2001)
Russia (TL)
 
  • Irkutsk Oblast
Konev A A et al. (1995) +1 other reference
  • Murmansk Oblast
PEKOV et al. (2013)
 
and/or  
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