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Grumantite

A valid IMA mineral species
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About GrumantiteHide

02070080017271923568297.jpg
Grumant
Formula:
Na(HSi2O5) · H2O
Colour:
white
Lustre:
Vitreous, Silky, Dull
Hardness:
4 - 5
Specific Gravity:
2.21
Crystal System:
Orthorhombic
Name:
From an old Russian name for the Spitzbergen Archipelago.
This page provides mineralogical data about Grumantite.


Unique IdentifiersHide

Mindat ID:
1757
Long-form identifier:
mindat:1:1:1757:8

IMA Classification of GrumantiteHide

Classification of GrumantiteHide

9.EH.10

9 : SILICATES (Germanates)
E : Phyllosilicates
H : Transitional structures between phyllosilicate and other silicate units
78.4.5.1

78 : Unclassified Silicates
4 :
14.1.7

14 : Silicates not Containing Aluminum
1 : Silicates of the alkali metals

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

Physical Properties of GrumantiteHide

Vitreous, Silky, Dull
Transparency:
Transparent
Comment:
Aggregates dull to silky, single crystals vitreous
Colour:
White
Streak:
White
Hardness:
4 - 5 on Mohs scale
Hardness Data:
Measured
Cleavage:
Perfect
on {100}
Fracture:
Step-Like
Density:
2.21 g/cm3 (Measured)    2.26 g/cm3 (Calculated)

Optical Data of GrumantiteHide

Type:
Biaxial (+)
RI values:
nα = 1.494(2) nβ = 1.507(2) nγ = 1.523(2)
2V:
Measured: 83° to 87°, Calculated: 84.9°
Max. Birefringence:
δ = 0.029
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:
weak, r > v
Optical Extinction:
X = a, Y = c, Z = b

Chemistry of GrumantiteHide

Mindat Formula:
Na(HSi2O5) · H2O
Element Weights:
Element% weight
O53.876 %
Si31.525 %
Na12.903 %
H1.697 %

Calculated from ideal end-member formula.

Crystallography of GrumantiteHide

Crystal System:
Orthorhombic
Class (H-M):
mm2 - Pyramidal
Space Group:
Fdd2
Cell Parameters:
a = 15.979 Å, b = 18.25 Å, c = 7.169 Å
Ratio:
a:b:c = 0.876 : 1 : 0.393
Unit Cell V:
2,090.60 ų (Calculated from Unit Cell)
Z:
16

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.505 Å(100)
3.006 Å(100)
6.20 Å(50)
6.05 Å(50)
4.46 Å(50)
3.087 Å(50)
3.346 Å(25)

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 GrumantiteHide

General Appearance of Type Material:
irregular crystals, compact massive
Place of Conservation of Type Material:
Geology Museum, Kola Branch, Academy of Sciences, Apatity, Russia.
Mineralogical Museum, St. Petersberg, Russia.
A.E.Fersman Mineralogical Museum, Moscow, Russia.
Geological Setting of Type Material:
in veins cutting alkalic feldspathoid-bearing pegmatites in a differentiated alkalic massif
Associated Minerals at Type Locality:

Synonyms of GrumantiteHide

Other Language Names for GrumantiteHide

Common AssociatesHide

Associations Based on Photo Data:
3 photos of Grumantite associated with AegirineNaFe3+Si2O6
2 photos of Grumantite associated with KazakoviteNa6Mn2+Ti(Si6O18)
2 photos of Grumantite associated with UssingiteNa2AlSi3O8OH
1 photo of Grumantite associated with SodaliteNa4(Si3Al3)O12Cl

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.15SarcoliteNa4Ca12Al8Si12O46(SiO4,PO4)(OH,H2O)4(CO3,Cl)Tet. 4/m : I4/m
9.EH.20UssingiteNa2AlSi3O8OHTric. 1 : P1
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 GrumantiteHide

Weak, bluish white

Other InformationHide

Thermal Behaviour:
The DTA curve exhibits marked endothermal effects at 280°C (dehydration), 700°C (phase transition), and 760°C (melting).
Notes:
Insoluble in cold water and cold 10% HCl, readily
soluble in hot 10% HCl giving a silicic residue.
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 GrumantiteHide

References for GrumantiteHide

Localities for GrumantiteHide

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.
Russia
 
  • Murmansk Oblast
    • Lovozersky District
ZVMO (1987)
Pekov (1998)
    • Rasvumchorr Mt
      • Rasvumchorr Mine
Pekov I.V. et al. (2010)
 
and/or  
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