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Mongolite

A valid IMA mineral species
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About MongoliteHide

09511080017271925244428.jpg
The typical Mongolian landscape.

Khovd Province, Mongolia
Formula:
Ca4Nb6Si5O24(OH)10 · nH2O
Colour:
Pale lilac or grayish lilac
Lustre:
Silky
Hardness:
2
Specific Gravity:
3.147
Crystal System:
Tetragonal
Name:
Named after the country of origin.
This page provides mineralogical data about Mongolite.


Unique IdentifiersHide

Mindat ID:
2756
Long-form identifier:
mindat:1:1:2756:0

Similar NamesHide

CongoliteA valid IMA mineral speciesFe32+B7O13Cl
MonroliteA synonym of Sillimanite

IMA Classification of MongoliteHide

Classification of MongoliteHide

9.HF.05

9 : SILICATES (Germanates)
H : Unclassified silicates
F : With Nb, Ta, Zr
56.2.4.15

56 : SOROSILICATES Si2O7 Groups, With Additional O, OH, F and H2O
2 : Si2O7 Groups and O, OH, F, and H2O with cations in [4] and/or >[4] coordination
17.8.5

17 : Silicates Containing other Anions
8 : Silicates with niobate or tantalate

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

Pronunciation of MongoliteHide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Physical Properties of MongoliteHide

Silky
Transparency:
Translucent
Colour:
Pale lilac or grayish lilac
Hardness:
Cleavage:
Distinct/Good
One direction, good
Density:
3.147 g/cm3 (Measured)    3.53 g/cm3 (Calculated)

Optical Data of MongoliteHide

Type:
Uniaxial (-)
RI values:
nω = 1.80 nε = 1.74
Max. Birefringence:
δ = 0.060
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:
Very 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 uniaxial interference figure - the conoscopic (convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis centred and vertical. The coloured rings are isochromatics, computed with the same physics as the Michel-Lévy bar above; the dark cross is the isogyre.

For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.

Chemistry of MongoliteHide

Mindat Formula:
Ca4Nb6Si5O24(OH)10 · nH2O
Element Weights:
Element% weight
O39.153 %
Nb38.975 %
Ca11.209 %
Si9.818 %
H0.846 %

Calculated from ideal end-member formula.
O
Nb
Ca
Si
H
Common Impurities:
Ti,Al,Mn,Zn,Mg,Sr,Ba,Na,K

Crystallography of MongoliteHide

Crystal System:
Tetragonal
Cell Parameters:
a = 7.00(5) Å, c = 29.0(1) Å
Ratio:
a:c = 1 : 4.143
Unit Cell V:
1,421.00 ų (Calculated from Unit Cell)
Z:
2
Comment:
Point Group: n.d.; Space Group: n.d.

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.163 Å(100)
2.974 Å(70)
3.087 Å(65)
9.67 Å(45)
5.82 Å(45)
2.664 Å(40)
2.901 Å(35)
Comments:
Dorozhnyi pegmatite, Mongolia. Data from 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
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]

Type Occurrence of MongoliteHide

General Appearance of Type Material:
Mica-like aggregate of fine scales.
Place of Conservation of Type Material:
A.E. Fersman Mineralogical Museum, Academy of Sciences, Moscow, Russia.
Geological Setting of Type Material:
A late alteration product of an unknown niobium silicate, in the quartz-rich core zone of an alkalic pegmatite.
Associated Minerals at Type Locality:

Synonyms of MongoliteHide

Other Language Names for MongoliteHide

Dutch:Mongoliet
German:Mongolit
Spanish:Mongolita

Common AssociatesHide

Associations Based on Photo Data:
7 photos of Mongolite associated with QuartzSiO2
5 photos of Mongolite associated with 'Kovalenkoite'(K,Sr,Ba)2Ca5Nb12[Si8O52(O,OH)] · 15H2O
1 photo of Mongolite associated with ArfvedsoniteNaNa2(Fe2+4Fe3+)Si8O22(OH)2

Related Minerals - Strunz-mindat GroupingHide

9.HF.10LoudouniteNaCa5Zr4Si16O40(OH)11 · 8H2O

Other InformationHide

Thermal Behaviour:
The DTA curve shows a broad endothermic effect between 100 and 350°C, (loss of water), and an exothermic effect at 700°C. The mineral does not melt below 1100°C.
Notes:
The mineral is insoluble in acid except HF.
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 MongoliteHide

References for MongoliteHide

Localities for MongoliteHide

Showing 5 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.
Mongolia
 
  • Ömnögovi Province
    • Khanbogd District
Vladykin (ed.) +7 other references
Zapiski Vserossiyskogo Mineralogicheskogo Obshchestva (Proceedings of the Russian Mineralogical Society)
Russia
 
  • Chelyabinsk Oblast
    • Ilmen Mountains
Makagonov et al. (2017)
  • Murmansk Oblast
Pekov et al. (2004)
  • Republic of Karelia
    • Loukhsky District
Sorokhtina et al. (2018)
 
and/or  
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