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Baratovite

A valid IMA mineral species
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About BaratoviteHide

05515250017271921356893.jpg
Rauf B. Baratov
Formula:
KCa7(Ti,Zr)2Li3Si12O36F2
Colour:
White, colorles, pink
Lustre:
Vitreous, Pearly
Hardness:
5 - 6
Specific Gravity:
2.92
Crystal System:
Monoclinic
Name:
Named in honor of Rauf Baratovich Baratov (Рауф Баратович Баратов) (10 October 1921, Pulatan, Turkestan (now Tajikistan) - 15 January 2013, Kazan, Russia), petrologist, Institute of Geology, Dushanbe, Tajikistan.
Note: Some mineralogists consider baratovite to be OH-dominant, which would make katayamalite the same species, with the name baratovite having priority.

The Ti analogue of Aleksandrovite.




Unique IdentifiersHide

Mindat ID:
512
Long-form identifier:
mindat:1:1:512:6

IMA Classification of BaratoviteHide

Classification of BaratoviteHide

9.CJ.25

9 : SILICATES (Germanates)
C : Cyclosilicates
J : [Si6O18]12- 6-membered single rings (sechser-Einfachringe), without insular complex anions
61.1.4.2

61 : CYCLOSILICATES Six-Membered Rings
1 : Six-Membered Rings with [Si6O18] rings; possible (OH) and Al substitution
14.9.32

14 : Silicates not Containing Aluminum
9 : Silicates of Ti

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

Pronunciation of BaratoviteHide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Physical Properties of BaratoviteHide

Vitreous, Pearly
Comment:
Pearly on cleavage
Colour:
White, colorles, pink
Hardness:
5 - 6 on Mohs scale
Hardness:
VHN100=615 kg/mm2 - Vickers
Comment:
615 on basal plane 715 to to 620 on cleavage planes. Original description of Mohs hardness was 3-3.5
Tenacity:
Brittle
Cleavage:
Perfect
Two directions crossing basal plane.
Density:
2.92(2) g/cm3 (Measured)    2.91 g/cm3 (Calculated)

Optical Data of BaratoviteHide

Type:
Biaxial (+)
RI values:
nα = 1.674 nβ = 1.671 nγ = 1.666
2V:
Measured: 60°
Max. Birefringence:
δ = 0.000
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 strong
Optical Extinction:
X ∧ ⊥ (001) ≃ 50°.

Chemistry of BaratoviteHide

Mindat Formula:
KCa7(Ti,Zr)2Li3Si12O36F2
Element Weights:
Element% weight
O41.521 %
Si24.295 %
Ca20.224 %
Ti6.901 %
K2.819 %
F2.739 %
Li1.501 %

Calculated from ideal end-member formula.
Common Impurities:
Fe,Nb,Mn,Na

Crystallography of BaratoviteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/b
Setting:
C2/c
Cell Parameters:
a = 16.94 Å, b = 9.74 Å, c = 20.9 Å
β = 112.5°
Ratio:
a:b:c = 1.739 : 1 : 2.146
Unit Cell V:
3,185.91 ų (Calculated from Unit Cell)

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006461BaratoviteBaur W H, Kassner D (1992) Katayamalite and baratovite are structurally identical European Journal of Mineralogy 4 839-84119920293
0000712BaratoviteMenchetti S, Sabelli C (1979) The crystal structure of baratovite American Mineralogist 64 383-38919790293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.22 Å(100)
2.41 Å(20)
1.92 Å(17)
3.02 Å(5)
3.54 Å(4)
1.60 Å(4)
1.49 Å(4)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Type Occurrence of BaratoviteHide

General Appearance of Type Material:
Off-white platy deposits up to 5 x 2 x 0.5 cm in size.
Place of Conservation of Type Material:
Mineralogical Museum, University of St. Petersburg, St. Petersburg, Russia, 16250-16252.
Institute of Mineralogy and Geochemistry of Rare Elements, Moscow, Russia.
A.E. Fersman Mineralogical Museum, Academy of Sciences, Moscow, Russia, 76077, 77839, vis5062.
Geological Setting of Type Material:
In quartz-albite-aegirine veinlets and in albitites in syenite.
Associated Minerals at Type Locality:

Synonyms of BaratoviteHide

Other Language Names for BaratoviteHide

German:Baratovit
Simplified Chinese:硅钛锂钙石
Spanish:Baratovita
Traditional Chinese:矽鈦鋰鈣石

Common AssociatesHide

Associations Based on Photo Data:
11 photos of Baratovite associated with AegirineNaFe3+Si2O6
5 photos of Baratovite associated with AgrelliteNaCa2Si4O10F
3 photos of Baratovite associated with QuartzSiO2
2 photos of Baratovite associated with AlbiteNa(AlSi3O8)
2 photos of Baratovite associated with MicroclineK(AlSi3O8)
2 photos of Baratovite associated with MiseriteK1.5-x(Ca,Y,REE)5(Si6O15)(Si2O7)(OH,F)2 · yH2O
1 photo of Baratovite associated with OrloviteKLi2Ti(Si4O10)OF
1 photo of Baratovite associated with FluoriteCaF2
1 photo of Baratovite associated with Pyrochlore GroupA2Nb2(O,OH)6Z

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.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.50OdintsoviteK2Na4Ca3Ti2Be4Si12O38Orth. mmm(2/m2/m2/m) : Fddd
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) 2.8185% 874 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

Fluorescence of BaratoviteHide

bright blue fluorescent response under short wave UV
see for example https://www.mindat.org/photo-852637.html

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 BaratoviteHide

References for BaratoviteHide

Localities for BaratoviteHide

Showing 3 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.
Japan
 
  • Ehime Prefecture
    • Ochi District
Murakami et al. (1983) +2 other references
Kyrgyzstan
 
  • Batken Region
    • Batken District
Pavel M. Kartashov (n.d.) +1 other reference
Tajikistan (TL)
 
  • Districts of Republican Subordination
Dusmatov et al. (1975) +5 other references
 
and/or  
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