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Imandrite

A valid IMA mineral species
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About ImandriteHide

06975520017271923966496.jpg
Lake Imandra, Russia
Formula:
Na12Ca3Fe3+2(Si6O18)2
Colour:
Honey-yellow
Lustre:
Vitreous
Hardness:
5 - 5½
Specific Gravity:
2.93
Crystal System:
Orthorhombic
Name:
Named by A.P. Khomyakov, N.M. Chernitsova, S.M. Sandomirskaya, and G.L. Vasil’eva for Lake Imanda, Kola Peninsula, Russia, near the type locality. It is the largest lake on the peninsula at 812 km2.

Unique IdentifiersHide

Mindat ID:
2017
Long-form identifier:
mindat:1:1:2017:2

IMA Classification of ImandriteHide

Classification of ImandriteHide

9.CJ.15b

9 : SILICATES (Germanates)
C : Cyclosilicates
J : [Si6O18]12- 6-membered single rings (sechser-Einfachringe), without insular complex anions
61.1.2b.1

61 : CYCLOSILICATES Six-Membered Rings
1 : Six-Membered Rings with [Si6O18] rings; possible (OH) and Al substitution
14.25.8

14 : Silicates not Containing Aluminum
25 : Silicates of Fe, Ca and alkalis and of Fe, Mg, Ca and alkalis

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

Physical Properties of ImandriteHide

Vitreous
Transparency:
Translucent
Colour:
Honey-yellow
Hardness:
5 - 5½ on Mohs scale
Density:
2.93 g/cm3 (Measured)    2.92 g/cm3 (Calculated)

Optical Data of ImandriteHide

Type:
Biaxial (+)
RI values:
nα = 1.605 nβ = 1.608 nγ = 1.612
2V:
Measured: 75° , Calculated: 82°
Max. Birefringence:
δ = 0.007
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:
High (positive)
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 biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
r > v

Chemistry of ImandriteHide

Mindat Formula:
Na12Ca3Fe3+2(Si6O18)2
Element Weights:
Element% weight
O40.539 %
Si23.721 %
Na19.417 %
Ca8.462 %
Fe7.861 %

Calculated from ideal end-member formula.
O
Si
Na
Ca
Fe
Common Impurities:
Ti,Zr,Mn,Mg

Crystallography of ImandriteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Cell Parameters:
a = 7.426(4) Å, b = 10.546(1) Å, c = 10.331(1) Å
Ratio:
a:b:c = 0.704 : 1 : 0.98
Unit Cell V:
809.07 ų (Calculated from Unit Cell)
Z:
1
Comment:
Space Group: Pmnn

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0012468ImandriteChernitsova N M, Pudovkina Z V, Voronkov A A, Ilyukhin V V, Pyatenko Y A (1980) Imandrite Na12Ca3Fe2[Si6O18]2 - a representative of a new branch in the lovozerite structural family Doklady Akademii Nauk SSSR 252 618-62119800293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.73 Å(50)
3.33 Å(60)
2.63 Å(100)
1.853 Å(70)
1.520 Å(50)

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 ImandriteHide

General Appearance of Type Material:
Anhedral grains, 1-3 mm
Place of Conservation of Type Material:
Geology Museum, Kola Branch, Academy of Sciences, Apatity,5530; Mining Institute, St. Petersburg, 1298/1; A.E. Fersman Mineralogical Museum, Academy of Sciences, Moscow, Russia, 80181; The Natural History Museum, London, England, 1994,10.
Geological Setting of Type Material:
Pegmatitic alkalic rocks
Associated Minerals at Type Locality:

Synonyms of ImandriteHide

Other Language Names for ImandriteHide

Dutch:Imandriet
German:Imandrit
Spanish:Imandrita

Relationship of Imandrite to other SpeciesHide

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Imandrite associated with EudialyteNa15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2

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.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.50OdintsoviteK2Na4Ca3Ti2Be4Si12O38Orth. mmm(2/m2/m2/m) : Fddd
9.CJ.55MathewrogersitePb7FeAl3GeSi12O36(OH,H2O)6Trig.
9.CJ.60Pezzottaite-(Cs)Cs(Be2Li)Al2(Si6O18)Trig. 3 : R3

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 ImandriteHide

References for ImandriteHide

Localities for ImandriteHide

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.
China
 
  • Shaanxi
    • Baoji
      • Taibai County
Yang et al. (2022)
Russia
 
  • Murmansk Oblast
Excalibur Mineral Corp. - Mineral News
Khomyakov et al. (1979) +1 other reference
 
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