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Kvanefjeldite

A valid IMA mineral species
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About KvanefjelditeHide

Formula:
Na4(Ca,Mn)(Si3O7)2(OH)2
Colour:
Pink with a distinct violet hue
Lustre:
Vitreous, Pearly
Hardness:
5½ - 6
Specific Gravity:
2.55
Crystal System:
Orthorhombic
Name:
Named after the type locality, Kvanefjeld mountain, Greenland.
This page provides mineralogical data about Kvanefjeldite.


Unique IdentifiersHide

Mindat ID:
2302
Long-form identifier:
mindat:1:1:2302:9

IMA Classification of KvanefjelditeHide

Classification of KvanefjelditeHide

9.DP.30

9 : SILICATES (Germanates)
D : Inosilicates
P : Transitional ino-phyllosilicate structures
72.5.3.1

72 : PHYLLOSILICATES Two-Dimensional Infinite Sheets with Other Than Six-Membered Rings
5 : Two-Dimensional Infinite Sheets with Other Than Six-Membered Rings with corrugated and complex layers
14.18.28

14 : Silicates not Containing Aluminum
18 : Silicates of Mn and Na, K, Mg, Ca or Fe

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

Physical Properties of KvanefjelditeHide

Vitreous, Pearly
Transparency:
Transparent
Comment:
almost pearly on the {010} cleavage
Colour:
Pink with a distinct violet hue
Hardness:
5½ - 6 on Mohs scale
Cleavage:
Distinct/Good
Good on f010g; poor on {101}
Density:
2.55 g/cm3 (Measured)    2.53 g/cm3 (Calculated)

Optical Data of KvanefjelditeHide

Type:
Biaxial (+)
RI values:
nα = 1.522(1) nβ = 1.522(1) nγ = 1.543(1)
Max. Birefringence:
δ = 0.021
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:
None to Very Low
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.

No measured or calculated 2V is on file for this mineral, so the value used here (0°) is estimated from its recorded refractive indices and optic sign, not from a direct 2V measurement.
Dispersion:
r < v distinct

Chemistry of KvanefjelditeHide

Mindat Formula:
Na4(Ca,Mn)(Si3O7)2(OH)2
Element Weights:
Element% weight
O45.831 %
Si30.169 %
Na16.464 %
Ca7.175 %
H0.361 %

Calculated from ideal end-member formula.
O
Si
Na
Ca
H
Common Impurities:
Ti,Al,Y,Fe,Mg,K

Crystallography of KvanefjelditeHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Cell Parameters:
a = 10.213(2) Å, b = 15.878(4) Å, c = 9.058(1) Å
Ratio:
a:b:c = 0.643 : 1 : 0.57
Unit Cell V:
1,468.86 ų (Calculated from Unit Cell)
Z:
4
Comment:
Space Group: Pcab

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0014783KvanefjelditeJohnsen O, Leonardsen E S, Falth L, Annehed H (1983) Crystal structure of kvanefjeldite: The introduction of [Si3O7OH] layers with eight-membered rings Neues Jahrbuch fur Mineralogie, Monatshefte 1983 505-5121983Ilimaussaq alkaline intrusion, South Greenland0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.117 Å(10)
4.355 Å(7)
3.880 Å(7)
4.447 Å(6)
3.388 Å(6)
3.313 Å(5)
2.576 Å(5)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
22 : Hydration and low-? subsurface aqueous alteration (see also #23)

Type Occurrence of KvanefjelditeHide

General Appearance of Type Material:
Streaks and veinlets
Place of Conservation of Type Material:
University of Copenhagen, Copenhagen, Denmark, 1983.136, GGU 47887; Harvard University, Cambridge, Massachusetts, 127475; National Museum of Natural History, Washington, D.C., USA, 162234.
Geological Setting of Type Material:
Alkaline intrusive complex
Associated Minerals at Type Locality:

Synonyms of KvanefjelditeHide

Other Language Names for KvanefjelditeHide

Common AssociatesHide

Associations Based on Photo Data:
2 photos of Kvanefjeldite associated with VilliaumiteNaF

Related Minerals - Strunz-mindat GroupingHide

9.DP.05Meliphanite(Ca,Na)2(Be,Al)[Si2O6(OH,F)]Tet. 4 : I4
9.DP.15LeucospheniteBaNa4Ti2B2Si10O30Mon. 2/m : B2/m
9.DP.20FerriprehniteCa2Fe3+(Si3AlO10)(OH)2Orth. mm2 : Pma2
9.DP.20PrehniteCa2Al2Si3O10(OH)2Orth. mm2
9.DP.25AmstalliteCaAl[(Al,Si)4O8(OH)2](OH)2 · (H2O,Cl)Mon. 2/m : B2/b
9.DP.35Lemoynite(Na,K)2CaZr2Si10O26 · 5H2OMon. 2/m : B2/b
9.DP.35Hogarthite(Na,K)2CaTi2Si10O26 · 8H2OMon. 2/m : B2/m
9.DP.35NatrolemoyniteNa4Zr2Si10O26 · 9H2OMon. 2/m : B2/m
9.DP.40AltisiteNa3K6Ti2Al2Si8O26Cl3Mon. 2/m : B2/m
9.DP.45Chiappinoite-(Y)Y2Mn(Si3O7)4Orth. mmm(2/m2/m2/m) : Ibam
9.DP.50EsquireiteBaSi6O13 · 7H2OMon. 2 : B2
9.DP.55LavinskyiteK(LiCu)Cu6(Si4O11)2(OH)4Orth.
9.DP.55PlancheiteCu8(Si8O22)(OH)4 · H2OOrth. mmm(2/m2/m2/m)

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 KvanefjelditeHide

References for KvanefjelditeHide

Localities for KvanefjelditeHide

Showing 2 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.
Greenland
 
  • Kujalleq
Petersen (2001)
      • Kuannersuit Plateau (Kvanefjeld)
        • Kvanefjeld deposit
- (n.d.) +1 other reference
 
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