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Edgarite

A valid IMA mineral species
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About EdgariteHide

Formula:
FeNb3S6
FeNb3+2Nb4+S6
Colour:
Dark grey
Lustre:
Metallic
Hardness:
2 - 2½
Specific Gravity:
4.99 (Calculated)
Crystal System:
Hexagonal
Name:
Named after Alan D. Edgar (1935–1998), Professor of Petrology, University of Western Ontario, London, Ontario, Canada, in recognition of his contributions to the study of alkaline rocks and synthetic equivalents.
An unusual sulphide mineral that appears to have formed at a very late, or final, stage of metamorphism, after the main event of fenitization, from a highly reduced, subalkaline S-C-H-rich fluid, which may have remobilized Nb as a result of destabilization of oxide minerals (Barkov et al. 2000).

The first mineral showing chalcophile behaviour of Nb. Also the first mineral with two reduced Nb cations (compare niobocarbide).


Unique IdentifiersHide

Mindat ID:
6910
Long-form identifier:
mindat:1:1:6910:2

IMA Classification of EdgariteHide

Classification of EdgariteHide

2.DB.25

2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
D : Metal Sulfides, M: S = 3 :4 and 2:3
B : M:S = 2:3
Dana 7th ed.:
2.11.13.1

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

Physical Properties of EdgariteHide

Metallic
Transparency:
Opaque
Colour:
Dark grey
Hardness:
2 - 2½ on Mohs scale
Hardness:
VHN100=135 (5 s test time) - Vickers
Cleavage:
Perfect
basal
Density:
4.99 g/cm3 (Calculated)

Optical Data of EdgariteHide

Anisotropism:
White to dark brown
Reflectivity:
WavelengthR1 (%)R2 (%)
470nm28.1% 40.2%
546nm27.4% 39.3%
589nm27.0% 38.5%
650nm27.0% 36.9%


Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 40.2%.
R1 shown in black, R2 shown in red
Pleochroism:
Strong
Comments:
Grey to light grey with a bluish tint
Comments:
Anisotropy strong.

Chemistry of EdgariteHide

Mindat Formula:
FeNb3S6

FeNb3+2Nb4+S6
Element Weights:
Element% weight
Nb52.893 %
S36.510 %
Fe10.598 %

Calculated from ideal end-member formula.
Common Impurities:
V,Mn

Crystallography of EdgariteHide

Crystal System:
Hexagonal
Class (H-M):
6 - Pyramidal
Space Group:
P63
Cell Parameters:
a = 5.912(1) Å, c = 12.675(2) Å
Ratio:
a:c = 1 : 2.144
Unit Cell V:
383.7 ų
Z:
2
Comment:
From Bindi and Martin (2018)

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0013199EdgariteAnzenhofer K, van den Berg J M, Cossee P, Helle J N (1970) The crystal structures and magnetic susceptibilities of MnNb3S6, FeNb3S6, CoNb3S6 and NiNb3S6 Journal of Physics and Chemistry of Solids 31 1057-10671970synthetic0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
High-? alteration and/or metamorphism
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])
Stage 4b: Highly evolved igneous rocks>3.0
35 : Ultra-alkali and agpaitic igneous rocks

Type Occurrence of EdgariteHide

General Appearance of Type Material:
Platy inclusions in Ti-(V)-rich pyrrhotite and ferroan alabandite, and as dark gray aggregates of platy grains.
Place of Conservation of Type Material:
Royal Ontario Museum, Toronto, Canada.
Geological Setting of Type Material:
In a feldspar-rich fenitized xenolith approximately 200m across in foyaite at the Khibina alkaline complex.
Associated Minerals at Type Locality:

Synonyms of EdgariteHide

Other Language Names for EdgariteHide

Dutch:Edgariet
German:Edgarit
Spanish:Edgarita

Common AssociatesHide

Associations Based on Photo Data:
3 photos of Edgarite associated with PyrrhotiteFe1-xS

Related Minerals - Strunz-mindat GroupingHide

2.DB.StangersiteSnGeS3Mon. 2/m : P21/b
2.DB.05AntimonseliteSb2Se3Orth. mmm(2/m2/m2/m) : Pnma
2.DB.05MetastibniteSb2S3Amor.
2.DB.05PääkköneniteSb2AsS2Mon. 2/m : B2/m
2.DB.05BismuthiniteBi2S3Orth. mmm(2/m2/m2/m) : Pnma
2.DB.05StibniteSb2S3Orth. mmm(2/m2/m2/m)
2.DB.05GuanajuatiteBi2Se3Orth. mmm(2/m2/m2/m) : Pnma
2.DB.10SuredaitePbSnS3Orth. mmm(2/m2/m2/m) : Pnma
2.DB.10OttemanniteSn2S3Orth. mmm(2/m2/m2/m)
2.DB.15KashiniteIr2S3Orth. mmm(2/m2/m2/m) : Pbcn
2.DB.15BowieiteRh2S3Orth. mmm(2/m2/m2/m) : Pbcn
2.DB.20Montbrayite(Au,Ag,Sb,Bi,Pb)23(Te,Sb,Bi,Pb)38Tric. 1 : P1
2.DB.30Tarkianite(Cu,Fe)(Re,Mo)4S8Iso. 43m : F43m
2.DB.35CameroniteCu5-x(Cu,Ag)3+xTe10 (x = 0.43)Mon. 2/m : B2/b
2.DB.40'Schreibersite (of Shephard)'Cr2S3

Fluorescence of EdgariteHide

nonfluorescent

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 EdgariteHide

References for EdgariteHide

Reference List:

Localities for EdgariteHide

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.
Russia (TL)
 
  • Murmansk Oblast
Barkov et al. (2000) +1 other reference
Olga Yakovleva et al. (2009)
 
and/or  
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