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Wangyanite

A valid IMA mineral species
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Formula:
PdNi8S8
Colour:
yellowish brown
Lustre:
Metallic
Specific Gravity:
5.14 (Calculated)
Crystal System:
Isometric
Name:
named in honor of Prof. Christina Yan Wang, (b 1968) a well-known researcher on platinum-group element (PGE) occurrences and enrichment mechanisms in mafic-ultramafic intrusions, notably those deposits related to the Emeishan large igneous province in China.
The new mineral was found in a sample designated 1569-108.4, obtained from the drill hole 1569 (45.391253°N, 109.886659°W) in the area of the Stillwater mine.


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Unique IdentifiersHide

Mindat ID:
471480
Long-form identifier:
mindat:1:1:471480:0

IMA Classification of WangyaniteHide

Classification of WangyaniteHide

2.BB.15

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

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

Physical Properties of WangyaniteHide

Metallic
Transparency:
Opaque
Colour:
Yellowish brown
Streak:
Black
Tenacity:
Brittle
Cleavage:
None Observed
Parting:
none
Fracture:
Irregular/Uneven
Density:
5.14 g/cm3 (Calculated)

Optical Data of WangyaniteHide

Anisotropism:
not discernible
Bireflectance:
not discernible
Reflectivity:
WavelengthR1 (%)R2 (%)
470nm34.6%41.6%
546nm27.6%32.8%
589nm42.7%50.5%
650nm44.6%52.9%


Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 52.9%.
R1 shown in black, R2 shown in red
Colour in reflected light:
subtle pale yellow color
Pleochroism:
Not Visible

Chemistry of WangyaniteHide

Mindat Formula:
PdNi8S8
Element Weights:
Element% weight
Ni56.403 %
S30.814 %
Pd12.783 %

Calculated from ideal end-member formula.
Ni
S
Pd

Crystallography of WangyaniteHide

Crystal System:
Isometric
Class (H-M):
m3m(4/m32/m) - Hexoctahedral
Space Group:
Fm3m
Setting:
Fm3m
Cell Parameters:
a = 10.117(1) Å
Unit Cell V:
1,035.51 ų (Calculated from Unit Cell)
Z:
4

X-Ray Powder DiffractionHide

Type Occurrence of WangyaniteHide

General Appearance of Type Material:
occurs as anhedral-subhedral granular crystals 200–400 µm in size
Place of Conservation of Type Material:
Type material is deposited in the collections of the Yifu Museum, China University of Geosciences, No. 388 Lumo Road, Wuhan 430074, People's Republic of China, catalogue number SW-JM1569108
Geological Setting of Type Material:
reef-type deposits in mafic-ultramafic intrusions at J-M reef of the Stillwater Complex
Associated Minerals at Type Locality:

Synonyms of WangyaniteHide

Other Language Names for WangyaniteHide

German:Wangyanit

Relationship of Wangyanite to other SpeciesHide

Other Members of Pentlandite Group:
ArgentopentlanditeAg(Fe,Ni)8S8Iso. m3m(4/m32/m) : Fm3m
CobaltpentlanditeCo9S8Iso. m3m(4/m32/m) : Fm3m
Geffroyite(Cu,Fe,Ag)9(Se,S)8Iso. m3m(4/m32/m) : Fm3m
OberthüriteRh3Ni32S32Iso.
Pentlandite(NixFey)Σ9S8Iso. m3m(4/m32/m) : Fm3m
Shadlunite(Pb,Cd)(Fe,Cu)8S8Iso. m3m(4/m32/m) : Fm3m
SugakiiteCu(Fe,Ni)8S8Tet. 4/mmm(4/m2/m2/m) : P42/mnm

Related Minerals - Strunz-mindat GroupingHide

2.BB.ArsenotučekiteNi18Sb3AsS16Tet. 4mm : I4mm
2.BB.HrabákiteNi9PbSbS8Tet. 4/mmm(4/m2/m2/m) : P4/mmm
2.BB.'UM2007-27-S:CuFeIrNiRh'(Ni,Fe,Cu,Rh,Ir)11S9
2.BB.HoromaniteFe6Ni3S8Tet. 4/mmm(4/m2/m2/m) : P4/mmm
2.BB.SamaniiteCu2Fe5Ni2S8Tet. 4/mmm(4/m2/m2/m) : P42/mnm
2.BB.05HeazlewooditeNi3S2Trig. 32 : R32
2.BB.05'UM2007-30-S:Fe'Fe3S2
2.BB.05Vozhminite(Ni,Co)4(As,Sb)S2Hex.
2.BB.05OregoniteNi2FeAs2Hex.
2.BB.10HauchecorniteNi9BiSbS8Tet. 4/mmm(4/m2/m2/m) : P4/mmm
2.BB.10ArsenohauchecorniteNi18Bi3AsS16Tet.
2.BB.10TellurohauchecorniteNi9Bi(Te,Bi)S8Tet. 4/mmm(4/m2/m2/m) : P4/mmm
2.BB.10JinxiuiteNi18Bi2SbAsS16Tet. 4/mmm(4/m2/m2/m) : I4/mmm
2.BB.10BismutohauchecorniteNi9Bi2S8Tet. 4/mmm(4/m2/m2/m) : P4/mmm
2.BB.10TučekiteNi9Sb2S8Tet. 4/mmm(4/m2/m2/m) : P4/mmm
2.BB.15ArgentopentlanditeAg(Fe,Ni)8S8Iso. m3m(4/m32/m) : Fm3m
2.BB.15Shadlunite(Pb,Cd)(Fe,Cu)8S8Iso. m3m(4/m32/m) : Fm3m
2.BB.15Ferhodsite(Fe,Rh,Ni,Ir,Cu,Pt)9S8Tet.
2.BB.15CobaltpentlanditeCo9S8Iso. m3m(4/m32/m) : Fm3m
2.BB.15'UM2002-26-S:FeNi'(Ni,Fe)9S8Hex.
2.BB.15Pentlandite(NixFey)Σ9S8Iso. m3m(4/m32/m) : Fm3m
2.BB.15OberthüriteRh3Ni32S32Iso.
2.BB.15Geffroyite(Cu,Fe,Ag)9(Se,S)8Iso. m3m(4/m32/m) : Fm3m
2.BB.15Kharaelakhite(Cu,Pt,Pb,Fe,Ni)9S8Orth. mmm(2/m2/m2/m) : Pmmm
2.BB.15'Manganoshadlunite'(Mn,Pb,Cd)(Cu,Fe)8S8
2.BB.15SugakiiteCu(Fe,Ni)8S8Tet. 4/mmm(4/m2/m2/m) : P42/mnm
2.BB.15Godlevskite(Ni,Fe)9S8Orth. 222 : C222

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 WangyaniteHide

References for WangyaniteHide

Localities for WangyaniteHide

Showing 1 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.
USA (TL)
 
  • Montana
    • Sweet Grass County
Sibanye Stillwater
 
and/or  
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