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Gerasimovskite

A valid IMA mineral species - grandfathered
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About GerasimovskiteHide

06002860017271923554599.jpg
Gerasimovsky, Vasily Ivanovich
Formula:
Mn2+(Nb,Ti)5O12 · 9H2O (?)
Colour:
brown to gray or light gray
Lustre:
Pearly
Hardness:
2
Specific Gravity:
2.52 - 2.58
Crystal System:
Amorphous
Name:
Named in 1957 by Evgeny Ivanovich Semenov in honor of Vasilii Ivanovich Gerasimovsky (Василий Иванович Герасимовский) (20 June 1907, village of Artemyevskaya, Vologda province - 11 August 1979, Transbaikalia) in 1934, discovered (together with O.A. Vorobyova) industrial deposits of loparite ore on the Kola Peninsula.
This page provides mineralogical data about Gerasimovskite.


Unique IdentifiersHide

Mindat ID:
1678
Long-form identifier:
mindat:1:1:1678:6

IMA Classification of GerasimovskiteHide

Classification of GerasimovskiteHide

4.FM.25

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
F : Hydroxides (without V or U)
M : Hydroxides with H2O +- (OH); unclassified
8.7.8.3

8 : MULTIPLE OXIDES CONTAINING NIOBIUM,TANTALUM OR TITANIUM
7 : Miscellaneous
18.1.37

18 : Niobates and Tantalates
1 : Niobates and tantalates containing neither rare earths nor U

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

Physical Properties of GerasimovskiteHide

Pearly
Colour:
Brown to gray or light gray
Hardness:
Cleavage:
Perfect
In one direction
Density:
2.52 - 2.58 g/cm3 (Measured)    

Optical Data of GerasimovskiteHide

Type:
Biaxial (-)
RI values:
nα = 1.74 nβ = 1.81 nγ = 1.81
2V:
Measured: 18°
Max. Birefringence:
δ = 0.070
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:
r > v moderate
Optical Extinction:
Parallel extinction, elongation positive.

Chemistry of GerasimovskiteHide

Mindat Formula:
Mn2+(Nb,Ti)5O12 · 9H2O (?)

Crystallography of GerasimovskiteHide

Crystal System:
Amorphous
Comment:
diffuse lines at 2.60, 1.85, and 1.64 A.

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
1.89 Å(100)
3.70 Å(80)
3.18 Å(60)
2.10 Å(40)
1.64 Å(20)
Comments:
Lovozero massif, Russia. Data collected after heating the sample at 900°C.

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 GerasimovskiteHide

General Appearance of Type Material:
Platy masses up to 1.5x1x0.3 cm.
Geological Setting of Type Material:
In ussingite-bearing pegmatites. Thought to have formed by the hydrothermal alteration of minerals of the murmanite-lomonosovite series.

Synonyms of GerasimovskiteHide

Other Language Names for GerasimovskiteHide

Relationship of Gerasimovskite to other SpeciesHide

Common AssociatesHide

Associations Based on Photo Data:
3 photos of Gerasimovskite associated with AegirineNaFe3+Si2O6
3 photos of Gerasimovskite associated with UssingiteNa2AlSi3O8OH
2 photos of Gerasimovskite associated with Birnessite(Na,Ca)0.5(Mn4+,Mn3+)2O4 · 1.5H2O
1 photo of Gerasimovskite associated with Manganonordite-(Ce)Na3SrCeMn2+Si6O17
1 photo of Gerasimovskite associated with AlbiteNa(AlSi3O8)
1 photo of Gerasimovskite associated with PectoliteNaCa2Si3O8(OH)

Related Minerals - Strunz-mindat GroupingHide

4.FM.CharleshatchettiteCaNb4O10(OH)2 · 8H2OMon. 2/m : B2/b
4.FM.15FranconiteNa(Nb2O5)(OH) · 3H2OMon.
4.FM.15Hochelagaite(Ca,Na,Sr)(Nb,Ti,Si,Al)4O11 · 8H2OMon.
4.FM.15Ternovite(Mg,Ca)Nb4O11 · nH2OMon.
4.FM.25BelyankiniteCa1-2(Ti,Zr,Nb)5O12 · 9H2O (?)Amor.
4.FM.25ManganbelyankiniteMn2+(Ti,Nb)5O12 · 9H2O
4.FM.30SilhydriteSi3O6 · H2OOrth.
4.FM.35CuzticiteFe3+2(TeO6) · 3H2OHex.
4.FM.50QatranaiteCaZn2(OH)6(H2O)2Mon. 2/m : P21/b
4.FM.55'Hydroplumbite'3PbO · H2O

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 GerasimovskiteHide

References for GerasimovskiteHide

Localities for GerasimovskiteHide

Showing 11 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 et al. (1993) +1 other reference
Russia
 
  • Murmansk Oblast
...
    • Kukisvumchorr Mt
Pekov (1998)
    • Lovozersky District
Pekov (2000)
Arzamastsev et al. (2008)
Pekov (2000)
        • Second Eastern Stream
Pekov (1998)
Trud.Inst.min.geokh.cryst. redkikh elementov (1957) +3 other references
Pekov et al. (2013)
 
and/or  
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