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Bonshtedtite

A valid IMA mineral species
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About BonshtedtiteHide

09650680017271921704891.jpg
Russian mineralogist Elsa Maximilianovna Bonshtedt-Kupletskaya.
Formula:
Na3Fe2+(CO3)(PO4)
Colour:
Colorless, with rose, yellowish, or greenish tint
Lustre:
Vitreous
Hardness:
4
Specific Gravity:
2.95 - 3.16
Crystal System:
Monoclinic
Name:
Named in 1982 by Alexander Petrovich Khomyakov, V. B. Aleksandrov, N. I. Krasnova, et al. in honour of Elsa Maximilianovna Bonshtedt-Kupletskaya (Эльза Максимилиановна Бонштедт-Куплетская) (18(30) October 1897, St. Petersburg, Russian Empire - 10 July 1974, Moscow, USSR), mineralogist and professor at the Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM) of the Academy of Sciences of the USSR. The mineral kupletskite is also named, in part, in her honour.
Structurally related to bradleyite.


Unique IdentifiersHide

Mindat ID:
719
Long-form identifier:
mindat:1:1:719:7

IMA Classification of BonshtedtiteHide

Classification of BonshtedtiteHide

5.BF.10

5 : CARBONATES (NITRATES)
B : Carbonates with additional anions, without H2O
F : With (Cl), SO4, PO4, TeO3
43.2.1.3

43 : COMPOUND PHOSPHATES, ETC.
2 : Anhydrous Normal Compound Phosphates, etc·
22.4.11

22 : Phosphates, Arsenates or Vanadates with other Anions
4 : Phosphates, arsenates or vanadates with carbonate

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

Physical Properties of BonshtedtiteHide

Vitreous
Transparency:
Transparent
Comment:
Pearly on cleavages.
Colour:
Colorless, with rose, yellowish, or greenish tint
Streak:
White
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
{010}, {100}
Density:
2.95 - 3.16 g/cm3 (Measured)    2.95 g/cm3 (Calculated)

Optical Data of BonshtedtiteHide

Type:
Biaxial (-)
RI values:
nα = 1.52 nβ = 1.568 nγ = 1.591
2V:
Measured: 68° , Calculated: 66°
Max. Birefringence:
δ = 0.071
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:
relatively strong
Optical Extinction:
X = b; Y = c; Z = a.

Chemistry of BonshtedtiteHide

Mindat Formula:
Na3Fe2+(CO3)(PO4)
Element Weights:
Element% weight
O40.028 %
Na24.650 %
Fe19.959 %
P11.070 %
C4.293 %

Calculated from ideal end-member formula.

Crystallography of BonshtedtiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/m
Setting:
P21/m
Cell Parameters:
a = 8.92 Å, b = 6.63 Å, c = 5.15 Å
β = 90.25°
Ratio:
a:b:c = 1.345 : 1 : 0.777
Unit Cell V:
304.57 ų (Calculated from Unit Cell)

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0020683BonshtedtiteKrivovichev S V, Chernyatieva A Y, Britvin S N, Yakovenchuk V N, Krivovichev V G (2013) Refinement of the crystal structure of bonshtedtite Na3Fe(PO4)(CO3) Zapiski Rossiiskogo Mineralogicheskogo Obshchetstva 142 46-542013Khibiny Massif, Kola Peninsula, Russia0293
0018485BonshtedtiteTjy C T L, Nadezhina T N, Pobedimskaya E A, Khomyakov A P (1984) Crystal chemical characteristics of bradleyite, sidorenkite and bonshtedtite Mineralogiceskij Zhurnal 6 79-8419840293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.318 Å(100)
2.662 Å(30)
8.923 Å(20)
2.578 Å(20)
2.146 Å(18)
1.658 Å(18)
1.851 Å(15b)
Comments:
Vuonnemiok River valley, Russia. Data from the type description.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 4b: Highly evolved igneous rocks>3.0
35 : Ultra-alkali and agpaitic igneous rocks
36 : Carbonatites, kimberlites, and related igneous rocks
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
50 : Coal and/or oil shale minerals<0.36

Type Occurrence of BonshtedtiteHide

General Appearance of Type Material:
Fine grained aggregates in shortite and as crystals up to 0.5x2x5 mm showing eleven forms.
Place of Conservation of Type Material:
Mining Institute, St. Petersburg, Russia, 1198/1.
Geology Museum, Kola Branch, Academy of Sciences, Apatity, Russia, 5713/5, 5723/1.
A.E. Fersman Mineralogical Museum, Academy of Sciences, Moscow, Russia, 81589.

Synonyms of BonshtedtiteHide

Other Language Names for BonshtedtiteHide

Russian (transliterated):Bonshtedtite
Spanish:Bonshtedtita

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Bonshtedtite associated with SidorenkiteNa3Mn2+(CO3)(PO4)
1 photo of Bonshtedtite associated with 'Titanium-bearing Aegirine'Na(Fe,Ti)Si2O6

Related Minerals - Strunz-mindat GroupingHide

5.BF.05NorthupiteNa3Mg(CO3)2ClIso. m3(2/m3) : Fd3
5.BF.05ManganotychiteNa6Mn2(CO3)4(SO4)Iso. m3(2/m3) : Fd3
5.BF.05TychiteNa6Mg2(CO3)4(SO4)Iso. m3(2/m3) : Fd3
5.BF.05FerrotychiteNa6(Fe,Mn,Mg)2(CO3)4(SO4)Iso. m3(2/m3) : Fd3
5.BF.10SidorenkiteNa3Mn2+(CO3)(PO4)Mon.
5.BF.10CrawforditeNa3Sr(CO3)(PO4)Mon. 2 : P21
5.BF.10BradleyiteNa3Mg(CO3)(PO4)Mon. 2/m : P21/m
5.BF.15Daqingshanite-(Ce)(Sr,Ca,Ba)3(Ce,La)(CO3)3-x(PO4)(OH,F)2xTrig.
5.BF.20Reederite-(Y)(Na,Mn)15Y2(CO3)9(FSO3)ClHex. 6 : P6
5.BF.25Mineevite-(Y)Na25Ba(Y,Gd,Dy)2(CO3)11(HCO3)4(SO4)2F2ClHex. 6/m : P63/m
5.BF.30BrianyoungiteZn3(CO3,SO4)(OH)4Mon. 2/m : P21/m
5.BF.35PhilolithitePb12Mn2+(Mg,Mn2+)2(Mn2+,Mg)4(CO3)4(SO4)O6(OH)12Cl4Tet. 4/mmm(4/m2/m2/m)
5.BF.40LeadhillitePb4(CO3)2(SO4)(OH)2Mon. 2/m : P21/b
5.BF.40MacphersonitePb4(CO3)2(SO4)(OH)2Orth. mmm(2/m2/m2/m)
5.BF.40SusannitePb4(CO3)2(SO4)(OH)2Trig. 3 : P3
5.BF.45Peatite-(Y)Li4Na12Y12(PO4)12(CO3)4(F,OH)8Orth. 222 : P222
5.BF.50Ramikite-(Y)Li4(Na,Ca)12Y6Zr6(PO4)12(CO3)4O4[(OH),F]4Tric. 1 : P1

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 BonshtedtiteHide

References for BonshtedtiteHide

Localities for BonshtedtiteHide

Showing 11 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.
Canada
 
  • Québec
    • Montérégie
      • La Vallée-du-Richelieu RCM
        • Mont Saint-Hilaire
HORVÁTH et al. (2000)
Russia
 
  • Murmansk Oblast
    • Carbonatite Stock in the vicinity of Tul'ilukht Bay
Pekov (1998)
PEKOV et al. (2013)
Khomyakov et al. (2002)
    • Kovdorsky District
Khomyakov et al. (1982) +2 other references
    • Kukisvumchorr Mt
[World of Stones 95:5-6
    • Lovozersky District
      • Alluaiv Mountain
        • Umbozero mine
Pekov (2000)
      • Suoluaiv Mountain
Khomyakov et al. (1982)
Khomyakov et al. (1982)
Khomyakov et al. (1982) +1 other reference
Khomyakov et al. (1982) +1 other reference
 
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