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Ussingite

A valid IMA mineral species - grandfathered
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About UssingiteHide

05257030017271927447018.jpg
Niels Viggo Ussing
Formula:
Na2AlSi3O8OH
Colour:
Pale to medium violet, reddish violet, colourless, white, purple
Lustre:
Sub-Vitreous
Hardness:
6 - 7
Specific Gravity:
2.48
Crystal System:
Triclinic
Name:
Named after Niels Viggo Ussing (14 June 1864, Copenhagen, Denmark - 23 July 1911, Copenhagen, Denmark), Professor of Mineralogy, University of Copenhagen, Denmark.
The structure is a unique, interrupted framework with strong H bonding. It is based on 4-, 6- and 8-membered rings of silicate tetrahedra, somewhat like these in feldspars but, as opposed to the latter, partially depolymerized.


Unique IdentifiersHide

Mindat ID:
4122
Long-form identifier:
mindat:1:1:4122:1

IMA Classification of UssingiteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Na2AlSi3O8(OH)

Classification of UssingiteHide

9.EH.20

9 : SILICATES (Germanates)
E : Phyllosilicates
H : Transitional structures between phyllosilicate and other silicate units
76.3.3.1

76 : TECTOSILICATES Al-Si Framework
3 : Al-Si Framework with other Be/Al/Si frameworks
16.2.3

16 : Silicates Containing Aluminum and other Metals
2 : Aluminosilicates of Na

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

Physical Properties of UssingiteHide

Sub-Vitreous
Transparency:
Transparent, Translucent
Colour:
Pale to medium violet, reddish violet, colourless, white, purple
Streak:
White
Hardness:
6 - 7 on Mohs scale
Tenacity:
Brittle
Fracture:
Irregular/Uneven
Density:
2.48 g/cm3 (Measured)    2.51 g/cm3 (Calculated)

Optical Data of UssingiteHide

Type:
Biaxial (+)
RI values:
nα = 1.504 nβ = 1.509 nγ = 1.545
2V:
Measured: 32° to 39°, Calculated: 42°
Birefringence:
0.041
Max. Birefringence:
δ = 0.041
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:
Low (negative)
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:
none
Optical Extinction:
Z angle b = 3˚

Chemistry of UssingiteHide

Mindat Formula:
Na2AlSi3O8OH
Element Weights:
Element% weight
O47.646 %
Si27.879 %
Na15.214 %
Al8.928 %
H0.334 %

Calculated from ideal end-member formula.
O
Si
Na
Al
H
Common Impurities:
Ca,K,Cl,H2O,S

Crystallography of UssingiteHide

Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 7.256 Å, b = 7.686 Å, c = 8.683 Å
α = 90.75°, β = 99.75°, γ = 122.48°
Ratio:
a:b:c = 0.944 : 1 : 1.13
Unit Cell V:
399.44 ų (Calculated from Unit Cell)
Z:
2
Morphology:
Crystals uncommon; blocky to tabular with dominant pinacoidal forms {100}, {010}, and {001}
Twinning:
{010}
Comment:
Williams & Weller (2012) data: a=7.2474(1), b=7.6813(1), c=8.6423(1), α=90.8351(1), β=99.771(1), γ=122.581(1)

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0000399UssingiteRossi G, Tazzoli V, Ungaretti L (1974) The crystal structure of ussingite American Mineralogist 59 335-3401974Lovozero alkali massif, Russia0293
0019374UssingiteWilliams E R, Weller M T (2012) A variable-temperature neutron diffraction study of ussingite; a strong asymmetric hydrogen bond in an aluminosilicate framework Physics and Chemistry of Minerals 39 471-4782012Nakalaq, Ilimaussaq complex, Greenland04
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
6.88 Å(70)
6.35 Å(90)
4.92 Å(70)
4.18 Å(70)
3.84 Å(70)
3.47 Å(70)
2.95 Å(100)
2.69 Å(100)
Comments:
14-426

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 3a: Earth’s earliest Hadean crust>4.50
9 : Lava/xenolith minerals (hornfels, sanidinite facies)
Stage 4b: Highly evolved igneous rocks>3.0
35 : Ultra-alkali and agpaitic igneous rocks

Type Occurrence of UssingiteHide

Geological Setting of Type Material:
Syenite pegmatite, also sodalite-bearing xenoliths

Other Language Names for UssingiteHide

Dutch:Ussingiet
German:Ussingit
Simplified Chinese:紫脆石
紫脆云母
Spanish:Ussingita
Traditional Chinese:紫脆石
紫脆雲母

Common AssociatesHide

Associations Based on Photo Data:
61 photos of Ussingite associated with SeranditeNaMn2+2Si3O8(OH)
56 photos of Ussingite associated with VuonnemiteNa11Ti4+Nb2(Si2O7)2(PO4)2O3(F,OH)
43 photos of Ussingite associated with SodaliteNa4(Si3Al3)O12Cl
39 photos of Ussingite associated with ChkaloviteNa2BeSi2O6
33 photos of Ussingite associated with AegirineNaFe3+Si2O6
28 photos of Ussingite associated with UmbozeriteNa3Sr4Th[Si(O,OH)3-4]8
27 photos of Ussingite associated with Steenstrupine-(Ce)Na14Mn2+2Fe3+2Ce6Zr(Si6O18)2(PO4)6(PO3OH)(OH)2 · 2H2O
21 photos of Ussingite associated with Tugtupite(BeAlSi)Na4(SiO4)3Cl
19 photos of Ussingite associated with ManganoneptuniteKNa2Li(Mn2+)2Ti2[Si4O12]2
17 photos of Ussingite associated with SphaleriteZnS

Related Minerals - Strunz-mindat GroupingHide

9.EH.05ManganoneptuniteKNa2Li(Mn2+)2Ti2[Si4O12]2Mon. m : Bb
9.EH.05MagnesioneptuniteKNa2Li(Mg)2Ti2[Si4O12]2Mon. 2/m : B2/b
9.EH.05NeptuniteKNa2Li(Fe2+)2Ti2[Si4O12]2Mon. m : Bb
9.EH.05WatatsumiiteKNa2Li(Mn2+)2V4+2[Si4O12]2Mon. m : Bb
9.EH.05RotherkopfiteKNa2Fe2+(Fe2+)2(Ti1.5Fe2+0.5)[Si4O12]2Mon. 2/m : B2/b
9.EH.10GrumantiteNa(HSi2O5) · H2OOrth. mm2 : Fdd2
9.EH.15SarcoliteNa4Ca12Al8Si12O46(SiO4,PO4)(OH,H2O)4(CO3,Cl)Tet. 4/m : I4/m
9.EH.25Telyushenkoite(Cs,Na,K)Na6[Be2Al3Si15O39]F2Trig. 3m(32/m) : P31m
9.EH.25Leifite(Na,H2O)Na6[Be2Al2(Al,Si)Si15O39]F2Trig. 3m : P3m1
9.EH.25EirikiteKNa6Be2(Si15Al3)O39F2Trig. 3m(32/m) : P3m1
9.EH.30NafertisiteNa3Fe2+10Ti2(Si6O17)2O2(OH)6F(H2O)2Mon. 2/m
9.EH.35VebleniteKNa(Fe2+5Fe3+4Mn7)Nb4(Si2O7)2(Si8O22)2O6(OH)10(H2O)3 Tric. 1 : P1

Fluorescence of UssingiteHide

Not fluorescent

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 UssingiteHide

References for UssingiteHide

Localities for UssingiteHide

Showing 38 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
 
  • Newfoundland and Labrador
    • Labrador
      • Seal Lake alkaline complex (Letitia Lake)
GSC locality database +1 other reference
  • Québec
    • Montérégie
      • La Vallée-du-Richelieu RCM
        • Mont Saint-Hilaire
Grice (1989) +2 other references
      • Lajemmerais RCM
        • Varennes & St-Amable
          • Saint-Amable sill
HORVÁTH (2010)
Greenland
 
  • Kujalleq
Petersen (2001) +1 other reference
Bøggild (1953)
Sørensen et al. (2001)
Karup-Møller (1976)
          • Lilleelv
Pavel Karthasov photo (photo-203416)
Karup-Møller et al. (1974) +1 other reference
Sørensen et al. (1970)
Makovicky et al. (1980)
Pekov et al. (2001)
Amer. Mineral. et al. (abs. ref. 1) +2 other references
Semenov et al. (1968)
Karup-Møller et al. (2001) +2 other references
MinerShop.com photo-Photo ID: 100976
Jesse Crawford photo & collection +1 other reference
        • Nunasaarnaq
Cran Cowan photo
Andersen et al. (1969)
Russia
 
  • Murmansk Oblast
Pekov et al. (2004)
Mikhailova et al. (2022)
    • Lovozersky District
Pekov (2000) +2 other references
Pekov (1998)
Ju et al. (1997) +1 other reference
Pavel M. Kartashov (n.d.)
Pekov (1998)
Pekov et al. (2001)
Pekov (1998)
Pekov (1998)
Pekov (1998) +1 other reference
        • Karnasurt mine
Pekov et al. (2004) +2 other references
        • Second Eastern Stream
Pekov (1998)
Kotrly et al. (1996)
Pekov (1998)
Pekov (1998) +2 other references
Ermolaeva et al. (2007) +1 other reference
Ermolaeva et al. (2007)
Haas (n.d.)
 
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