Vozhminite
A valid IMA mineral species
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Formula:
(Ni,Co)4(As,Sb)S2
Type material contains minor Co and Sb, possibly stabilising the structure.
Colour:
Yellow with brownish tint
Lustre:
Metallic
Hardness:
4½ - 5
Specific Gravity:
6.2 (Calculated)
Crystal System:
Hexagonal
Name:
Named after its discovery locality, Vozhminskiy massif, Karelia, Russia.
Unique Identifiers
Mindat ID:
4210
Long-form identifier:
mindat:1:1:4210:5
IMA Classification of Vozhminite
Approved
IMA Formula:
Ni4AsS2
Approval year:
1981
Classification of Vozhminite
2.BB.05
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
B : Metal Sulfides, M: S > 1: 1 (mainly 2: 1)
B : With Ni
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
B : Metal Sulfides, M: S > 1: 1 (mainly 2: 1)
B : With Ni
2.3.6.1
2 : SULFIDES
3 : AmBnXp, with (m+n):p = 5:2
2 : SULFIDES
3 : AmBnXp, with (m+n):p = 5:2
5.8.19
5 : Sulphosalts - Sulpharsenites and Sulphobismuthites (those containing Sn, Ge,or V are in Section 6)
8 : Sulpharsenites etc. of Mn, Fe, Co and Ni
5 : Sulphosalts - Sulpharsenites and Sulphobismuthites (those containing Sn, Ge,or V are in Section 6)
8 : Sulpharsenites etc. of Mn, Fe, Co and Ni
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Voz | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Vozhminite
Metallic
Transparency:
Opaque
Colour:
Yellow with brownish tint
Streak:
Black
Hardness:
4½ - 5 on Mohs scale
Hardness:
VHN100=436 kg/mm2 - Vickers
Cleavage:
Distinct/Good
one distinct
one distinct
Density:
6.2 g/cm3 (Calculated)
Optical Data of Vozhminite
Anisotropism:
Distinct, in brownish tones.
Bireflectance:
Weak
Reflectivity:
| Wavelength | R1 (%) | R2 (%) |
|---|---|---|
| 420nm | 35.0% | 41.2% |
| 440nm | 37.0% | 43.0% |
| 460nm | 39.2% | 45.0% |
| 480nm | 41.7% | 47.0% |
| 500nm | 44.0% | 48.6% |
| 520nm | 45.9% | 49.8% |
| 540nm | 47.5% | 50.0% |
| 560nm | 48.9% | 51.9% |
| 580nm | 50.2% | 52.7% |
| 600nm | 51.2% | 53.3% |
| 620nm | 52.1% | 54.2% |
| 640nm | 52.8% | 55.0% |
| 660nm | 53.4% | 55.8% |
| 680nm | 53.7% | 56.6% |
| 700nm | 54.1% | 57.1% |
| 720nm | 54.6% | 57.7% |
| 740nm | 54.9% | 58.2% |
Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 58.2%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Rose-orange
Chemistry of Vozhminite
Mindat Formula:
(Ni,Co)4(As,Sb)S2
Type material contains minor Co and Sb, possibly stabilising the structure.
Type material contains minor Co and Sb, possibly stabilising the structure.
Element Weights:
Common Impurities:
Fe
Crystallography of Vozhminite
Crystal System:
Hexagonal
Cell Parameters:
a = 17.46(4) Å, c = 7.20(1) Å
Ratio:
a:c = 1 : 0.412
Unit Cell V:
1,900.87 ų (Calculated from Unit Cell)
Z:
18
Morphology:
Massive(?).
Comment:
Point group and space group not determined.
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 8.7 Å | (100) |
| 3.07 Å | (90) |
| 2.717 Å | (60) |
| 2.303 Å | (70) |
| 2.111 Å | (90) |
| 1.776 Å | (100 broad) |
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| High-? alteration and/or metamorphism | |
| 33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12]) |
Type Occurrence of Vozhminite
General Appearance of Type Material:
Grains, 5-50 microns.
Place of Conservation of Type Material:
Mining Institute, St. Petersburg, Russia, 1139/1.
Geological Setting of Type Material:
Serpentinites. In polymineral phenocrysts composed primarily of heazlewoodite.
Associated Minerals at Type Locality:
Synonyms of Vozhminite
Other Language Names for Vozhminite
Related Minerals - Strunz-mindat Grouping
| 2.BB. | Arsenotučekite | Ni18Sb3AsS16 |
| 2.BB. | Hrabákite | Ni9PbSbS8 |
| 2.BB. | 'UM2007-27-S:CuFeIrNiRh' | (Ni,Fe,Cu,Rh,Ir)11S9 |
| 2.BB. | Horomanite | Fe6Ni3S8 |
| 2.BB. | Samaniite | Cu2Fe5Ni2S8 |
| 2.BB.05 | Heazlewoodite | Ni3S2 |
| 2.BB.05 | 'UM2007-30-S:Fe' | Fe3S2 |
| 2.BB.05 | Oregonite | Ni2FeAs2 |
| 2.BB.10 | Hauchecornite | Ni9BiSbS8 |
| 2.BB.10 | Arsenohauchecornite | Ni18Bi3AsS16 |
| 2.BB.10 | Tellurohauchecornite | Ni9Bi(Te,Bi)S8 |
| 2.BB.10 | Jinxiuite | Ni18Bi2SbAsS16 |
| 2.BB.10 | Bismutohauchecornite | Ni9Bi2S8 |
| 2.BB.10 | Tučekite | Ni9Sb2S8 |
| 2.BB.15 | Argentopentlandite | Ag(Fe,Ni)8S8 |
| 2.BB.15 | Shadlunite | (Pb,Cd)(Fe,Cu)8S8 |
| 2.BB.15 | Ferhodsite | (Fe,Rh,Ni,Ir,Cu,Pt)9S8 |
| 2.BB.15 | Cobaltpentlandite | Co9S8 |
| 2.BB.15 | 'UM2002-26-S:FeNi' | (Ni,Fe)9S8 |
| 2.BB.15 | Pentlandite | (NixFey)Σ9S8 |
| 2.BB.15 | Oberthürite | Rh3Ni32S32 |
| 2.BB.15 | Geffroyite | (Cu,Fe,Ag)9(Se,S)8 |
| 2.BB.15 | Kharaelakhite | (Cu,Pt,Pb,Fe,Ni)9S8 |
| 2.BB.15 | 'Manganoshadlunite' | (Mn,Pb,Cd)(Cu,Fe)8S8 |
| 2.BB.15 | Sugakiite | Cu(Fe,Ni)8S8 |
| 2.BB.15 | Godlevskite | (Ni,Fe)9S8 |
| 2.BB.15 | Wangyanite | PdNi8S8 |
Other Information
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 Vozhminite
mindat.org URL:
https://www.mindat.org/min-4210.html
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References for Vozhminite
Localities for Vozhminite
Showing 1 localities.
Locality List
- 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).
All localities listed without proper references should be considered as questionable.
Russia (TL) | |
| Rudashevskii N S et al. (1982) +2 other references |
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