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Kalyuzhnyite-(Ce)

A valid IMA mineral species
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Formula:
NaKCaSrCeTi(Si8O21)OF(H2O)3
Colour:
colourless
Lustre:
Vitreous
Specific Gravity:
3.120 (Calculated)
Crystal System:
Monoclinic
Name:
to honour Vasily Avksentievich Kalyuzhny (1899–1993) due to his contributions to the geology of ore deposits of Komi Republic (Russia) and mineralogy of granitic pegmatites of Tajikistan
New structure type. Unique combination of elements (at the upload time).

Structuredetails:
* heteropolyhedral Na–Sr–Ce–Ti sheet, [NaSrCeTiOF]7+ composition;
* double (Si8O21)10– sheet || (010) (unique among the all mineral species known at the upload time);
* the Si tetrahedra form tenmembered rings
* the framework is built via merging of 2 sheets (via common vertices of M polyhedra and silicate tetrahedra)
* the interstices within the Si–O sheet are occupied so that the ideal composition of the intra-sheet space is [(CaK)(H2O)3]3+.


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Unique IdentifiersHide

Mindat ID:
470699
Long-form identifier:
mindat:1:1:470699:7

IMA Classification of Kalyuzhnyite-(Ce)Hide

Approved
IMA Formula:
NaKCaSrCe3+Ti4+(Si8O21)OF(H2O)3
Approval year:
2023
Approval history:
IMA No. 2022-133
Type description reference:

Classification of Kalyuzhnyite-(Ce)Hide

9.HA.

9 : SILICATES (Germanates)
H : Unclassified silicates
A : With Alkali and Alkali-earth Elements

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

Physical Properties of Kalyuzhnyite-(Ce)Hide

Vitreous
Transparency:
Transparent
Colour:
Colourless
Streak:
White
Tenacity:
Brittle
Cleavage:
Perfect
{010}
Parting:
none
Fracture:
Irregular/Uneven
Comment:
grain too small for hardness testing
Density:
3.120 g/cm3 (Calculated)

Chemistry of Kalyuzhnyite-(Ce)Hide

Mindat Formula:
NaKCaSrCeTi(Si8O21)OF(H2O)3
Element Weights:
Element% weight
O38.929 %
Si21.867 %
Ce13.637 %
Sr8.528 %
Ti4.659 %
Ca3.901 %
K3.805 %
Na2.238 %
F1.849 %
H0.589 %

Calculated from ideal end-member formula.
O
Si
Ce
Sr
Ti
Ca
K
Na
F
H

Chemical AnalysisHide

Oxide wt%:
 1
Nb2O50.53 %
TiO20.16 %
SiO243.85 %
Er2O30.13 %
Ho2O30.10 %
Gd2O30.09 %
Sm2O30.47 %
Nd2O36.22 %
Pr2O31.21 %
Ce2O36.34 %
La2O30.82 %
PbO4.90 %
BaO0.85 %
SrO11.39 %
CaO1.86 %
Cs2O3.80 %
K2O1.59 %
Na2O2.99 %
H2O5.24 %
F1.55 %
O=F-0.65 %
Total:93.44 %
Empirical formulas:
Sample IDEmpirical Formula
1Na1.07K0.37Cs0.30Sr1.21Ca0.37Pb0.24Ba0.06(Ce0.43Nd0.41Pr0.08La0.06Sm0.03Gd0.01Er0.01Ho0.01)Σ1.04(Ti0.97Nb0.04)Σ1.01Si8.06O25.21F0.90H6.42

Crystallography of Kalyuzhnyite-(Ce)Hide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P2/b
Setting:
P2/c
Cell Parameters:
a = 18.647(4) Å, b = 11.214(2) Å, c = 14.642(3) Å
β = 129.55(3)°
Ratio:
a:b:c = 1.663 : 1 : 1.306
Unit Cell V:
2360.9 ų
Z:
4
Twinning:
none visible

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.978 Å(24)
3.423 Å(22)
3.332 Å(33)
3.026 Å(100)
2.963 Å(40)
2.895 Å(24)
2.591 Å(28)
2.344 Å(33)
Reference:

Type Occurrence of Kalyuzhnyite-(Ce)Hide

General Appearance of Type Material:
grains, up to 0.05 x 0.07 mm
Place of Conservation of Type Material:
collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 119071, Russia, registration number 5923/1
How to
Geological Setting of Type Material:
found within a quartz-pectolite aggregate of a silexite-like peralkaline pegmatite
Associated Minerals at Type Locality:
Reference:

Other Language Names for Kalyuzhnyite-(Ce)Hide

Related Minerals - Strunz-mindat GroupingHide

9.HA.ShinichengiteCa5[BSi2O7(OH)2]2 · 6H2OTric. 1 : P1
9.HA.MoragiteCa3TiSi2(Al2Si)O14Trig. 32 : P321
9.HA.05ErtixiiteNa2Si4O9Iso.
9.HA.10KenyaiteNa2Si22O41(OH)8 · 6H2OMon.
9.HA.20WawayandaiteCa6Mn2BBe9Si6O23(OH,Cl)15Mon.
9.HA.25MagbasiteKBaFe3+Mg7Si8O22(OH)2F6Orth. mmm(2/m2/m2/m) : Cmma
9.HA.35DemagistrisiteBaCa2Mn3+4(Si3O10)(Si2O7)(OH)4 · 3H2OOrth. mm2 : Amm2
9.HA.37DonwilhelmsiteCaAl4Si2O11Hex. 6/mmm(6/m2/m2/m) : P63/mmc
9.HA.40KasatkiniteBa2Ca8B5Si8O32(OH)3 · 6H2O Mon.
9.HA.40'Igumnovite'Ca3Al2[SiO4]2[◻Cl4]Iso.
9.HA.42PaqueiteCa3TiSi2(Al,Ti,Si)3O14Trig. 32 : P321
9.HA.42QeltiteCa3TiSi2(Fe3+2Si)O14Trig. 32 : P321
9.HA.45RippiteK2(Nb,Ti)2(Si4O12)O(O,F)Tet.
9.HA.47ZagamiiteCaAl2Si3.5O11Hex. 6/mmm(6/m2/m2/m) : P63/mmc
9.HA.50RudenkoiteSr3(Al3.5Si3.5)O10(OH,O)8Cl2 · H2OMon.
9.HA.50'α-Carnegieite'NaAlSiO4
9.HA.52'Atheriastite'near Ca5MgFeAl6Si8O32 · 5H2O
9.HA.55'Foshallasite'Ca3[Si2O7] · 3H2O(?)
9.HA.57'Bhreckite'
9.HA.60NagelschmidtiteCa7(SiO4)2(PO4)2Hex. 6 : P61
9.HA.65Caryochroite[Na(Sr0.5Ca0.5)Mg]3[Fe3+8Mn(Fe2+0.5◻0.5)]10(Ti2Si12O37)(OH)14(H2O)3 Mon. 2/m
9.HA.70JuaniteCa10Mg4Al2Si11O39 · 4H2O or nearOrth.
9.HA.75TacharaniteCa12Al2Si18O33(OH)36Mon.
9.HA.80OyeliteCa10Si8B2O29 · 12.5H2OTric. 1 : P1
9.HA.85DenisoviteK14+x(Ca,Na,Mn,Fe)48[Si60O162]F16(Ox,OH4-x) · 2H2OMon.
9.HA.90TiettaiteK4Na12Fe3+Si16O41(OH)4 · 2H2OOrth. mmm(2/m2/m2/m) : Cmcm

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) 3.8052% 1,180 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 Kalyuzhnyite-(Ce)Hide

does not fluoresce under cathode waves or ultraviolet 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 Kalyuzhnyite-(Ce)Hide

References for Kalyuzhnyite-(Ce)Hide

Localities for Kalyuzhnyite-(Ce)Hide

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
Bosi et al. (2023) +1 other reference
 
and/or  
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