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Sudovikovite

A valid IMA mineral species
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About SudovikoviteHide

04045690017271928983366.jpg
Nikolai G. Sudovikov
Formula:
PtSe2
Colour:
Yellowish white
Lustre:
Metallic
Hardness:
2 - 2½
Specific Gravity:
9.7 (Calculated)
Crystal System:
Trigonal
Member of:
Name:
Named in honor of Nikolai Georgievich Sudovikov (Николай Георгиевич Судовиков) (26 December 1903, Sevastopol, the Taurian Gubernia, Russian Empire - 29 July 1966, Leningrad, USSR), geologist, petrologist and professor in the Geological Faculty of Leningrad State University.
This page provides mineralogical data about Sudovikovite.


Unique IdentifiersHide

Mindat ID:
7321
Long-form identifier:
mindat:1:1:7321:5

IMA Classification of SudovikoviteHide

Classification of SudovikoviteHide

2.EA.20

2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
E : Metal Sulfides, M: S <= 1:2
A : M:S = 1:2 - With Cu, Ag, Au

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

Physical Properties of SudovikoviteHide

Metallic
Transparency:
Opaque
Colour:
Yellowish white
Hardness:
2 - 2½ on Mohs scale
Hardness:
VHN20=81 - 93 kg/mm2 - Vickers
Density:
9.7 g/cm3 (Calculated)

Optical Data of SudovikoviteHide

Anisotropism:
Strong, rose-yellow to dark gray-lilac
Bireflectance:
Strong
Reflectivity:
WavelengthR1 (%)R2 (%)
400nm39.1%46.1%
420nm38.4%47.9%
440nm39.1%50.3%
460nm35.6%48.0%
470nm35.1%48.4%
480nm35.2%48.5%
500nm34.9%48.5%
520nm34.7%48.4%
540nm34.9%48.4%
546nm35.1%48.3%
560nm35.0%48.8%
580nm35.2%49.0%
589nm35.3%49.1%
600nm35.4%49.2%
620nm35.9%49.8%
640nm36.2%50.1%
650nm36.5%50.8%
660nm36.9%51.3%
680nm37.5%51.8%
700nm37.8%52.5%


Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 52.5%.
R1 shown in black, R2 shown in red
Colour in reflected light:
White
Pleochroism:
Visible
Comments:
Light yellow to light lilac

Chemistry of SudovikoviteHide

Mindat Formula:
PtSe2
Element Weights:
Element% weight
Pt55.264 %
Se44.736 %

Calculated from ideal end-member formula.
CAS Registry number:
12038-26-5

CAS Registry numbers are published by the American Chemical Society

Crystallography of SudovikoviteHide

Crystal System:
Trigonal
Class (H-M):
3m(32/m) - Hexagonal Scalenohedral
Space Group:
P3m1
Setting:
P3m1
Cell Parameters:
a = 3.730(7) Å, c = 5.024(17) Å
Ratio:
a:c = 1 : 1.347
Unit Cell V:
60.53 ų (Calculated from Unit Cell)
Z:
1

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0011796SudovikoviteWyckoff R W G (1963) Second edition. Interscience Publishers, New York, New York Crystal Structures 1 239-44419630293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
5.04 Å(30)
2.715 Å(100)
1.983 Å(50)
1.859 Å(50)
1.747 Å(30)
1.360 Å(40)

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])

Type Occurrence of SudovikoviteHide

Synonyms of SudovikoviteHide

Other Language Names for SudovikoviteHide

Relationship of Sudovikovite to other SpeciesHide

Member of:
Other Members of Melonite Group:
BerndtiteSnS2Trig. 3m(32/m) : P3m1
KitkaiteNiTeSeTrig. 3m(32/m) : P3m1
MeloniteNiTe2Trig. 3m(32/m) : P3m1
MerenskyitePdTe2Trig. 3m : P3m1
MoncheitePt(Te,Bi)2Trig. 3m(32/m) : P3m1
ShuangfengiteIrTe2Trig. 3m : P3m1

Related Minerals - Strunz-mindat GroupingHide

2.EA.RadvaniceiteGeS2Mon. m : Pb
2.EA.ZavyaloviteAg2TeS3Mon. m : Bb
2.EA.05SylvaniteAgAuTe4Mon. 2/m : P2/b
2.EA.10CalaveriteAuTe2Mon.
2.EA.15KostoviteCuAuTe4Orth.
2.EA.15KrenneriteAu3AgTe8Orth. mm2 : Pma2
2.EA.20MeloniteNiTe2Trig. 3m(32/m) : P3m1
2.EA.20MerenskyitePdTe2Trig. 3m : P3m1
2.EA.20OgnititeNiBiTeTrig. 3m : P3m1
2.EA.20ShuangfengiteIrTe2Trig. 3m : P3m1
2.EA.20BerndtiteSnS2Trig. 3m(32/m) : P3m1
2.EA.20KitkaiteNiTeSeTrig. 3m(32/m) : P3m1
2.EA.20MoncheitePt(Te,Bi)2Trig. 3m(32/m) : P3m1
2.EA.25VerbeekitePdSe2Mon.
2.EA.30DrysdalliteMoSe2Hex. 6/mmm(6/m2/m2/m) : P63/mmc
2.EA.30JordisiteMoS2Amor.
2.EA.30MolybdeniteMoS2Hex. 6/mmm(6/m2/m2/m) : P63/mmc
2.EA.30TungsteniteWS2Trig. 3m : R3m
2.EA.40PampaloiteAuSbTeMon. 2/m : B2/b

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 SudovikoviteHide

References for SudovikoviteHide

Localities for SudovikoviteHide

Showing 4 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.
Australia
 
  • Northern Territory
    • West Arnhem Region
      • South Alligator River
Pašava et al. (2013)
Brazil
 
  • Minas Gerais
    • Itabira
MinMag 66:327-336 +1 other reference
  • Pará
    • Curionópolis
Cabral et al. (2002) +4 other references
Russia (TL)
 
  • Republic of Karelia
    • Medvezhyegorsky District
      • Zaonezhie peninsula
Polekhovskiy et al. (1997) +3 other references
 
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