Cherepanovite (original) (raw)
A valid IMA mineral species
About CherepanoviteHide
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Specific Gravity:
9.72 (Calculated)
Crystal System:
Orthorhombic
Name:
For Vladimir Aleksandrovich Cherepanov (1927-1983) Russian geologist and mineralogist, Karpinskii All-Union Research Institute of Geology, St. Petersburg, Russia.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:990:0
d6dc8307-2311-46ad-b778-2a2e64079dde
IMA Classification of CherepanoviteHide
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Type description reference:
Classification of CherepanoviteHide
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2.CC.15
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
C : Metal Sulfides, M: S = 1: 1 (and similar)
C : With Ni, Fe, Co, PGE, etc.
2.8.17.2
2 : SULFIDES
8 : AmXp, with m:p = 1:1
3.12.11
3 : Sulphides, Selenides, Tellurides, Arsenides and Bismuthides (except the arsenides, antimonides and bismuthides of Cu, Ag and Au, which are included in Section 1)
12 : Sulphides etc. of the platinum metals
Mineral SymbolsHide
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As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Cpv | 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 CherepanoviteHide
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Hardness:
VHN50=726 - 754 kg/mm2 - Vickers
Cleavage:
Distinct/Good
One distinct direction
Density:
9.72 g/cm3 (Calculated)
Optical Data of CherepanoviteHide
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Anisotropism:
Green to gray-brown
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
420nm | 39.2% | 40.5% |
440nm | 39.6% | 41.0% |
460nm | 40.3% | 41.9% |
480nm | 41.0% | 42.9% |
500nm | 41.9% | 43.8% |
520nm | 42.7% | 44.7% |
540nm | 43.6% | 45.5% |
560nm | 44.1% | 46.1% |
580nm | 44.5% | 46.6% |
600nm | 44.9% | 47.1% |
620nm | 45.1% | 47.3% |
640nm | 45.2% | 47.4% |
660nm | 45.3% | 47.6% |
680nm | 45.5% | 47.6% |
700nm | 45.4% | 47.6% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 47.6%.
R1 shown in black, R2 shown in red
Colour in reflected light:
White with an orange tint
Comments:
In yellow to pinkish hue and bluish white.
Chemistry of CherepanoviteHide
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Common Impurities:
Ru,Pt,Ni
Crystallography of CherepanoviteHide
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Crystal System:
Orthorhombic
Class (H-M):
m m m _(_2/_m_2/_m_2/m ) - Dipyramidal
Cell Parameters:
a = 5.70(2) Å, b = 3.59(1) Å, c = 6.00(1) Å
Ratio:
a:b:c = 1.588 : 1 : 1.671
Unit Cell V:
122.78 ų (Calculated from Unit Cell)
Morphology:
Grains to 20 microns.
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0020514 | Cherepanovite | Heyding R D, Calvert L D (1961) Arsenides of the transition metals IV. A note on the platinum metal arsenides Canadian Journal of Chemistry 39 955-957 | 1961 | Synthetic | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.01 Å | (10) |
2.10 Å | (6) |
1.771 Å | (2) |
1.501 Å | (2) |
1.354 Å | (2) |
Geological EnvironmentHide
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Type Occurrence of CherepanoviteHide
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General Appearance of Type Material:
Individual grains (up to 20 microns) or their aggregates (up to 100 microns) included in ferronickelplatinum or among aggregates of cooperite.
Place of Conservation of Type Material:
Mining Institute, St. Petersburg, Russia, 2103/1.
Geological Setting of Type Material:
Placer platinum deposit derived from ultramafic massif in ophiolite belt.
Associated Minerals at Type Locality:
Reference:
Rudashevsky, N.S., Motshalov, A.G., Trubkin, N.V., Shumskaya, N.M., Shkursky, V.I., Evstigneeva, T.L. (1985) Cherepanovite RhAs - A new mineral. Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva: 114(4): 464-469.
Synonyms of CherepanoviteHide
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Other Language Names for CherepanoviteHide
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Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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2.CC. | Tilkerodeite | Pd2HgSe3 | Trig. 3_m_ _(_32/m ) : _P_3_m_1 |
---|---|---|---|
2.CC. | UM2007-26-S:CuFeIrNiPtRh | (Ir,Cu,Ni,Pt,Rh,Fe)9S11 | |
2.CC. | Crowningshieldite | (Ni0.9Fe0.1)S | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC. | Eliopoulosite | V7S8 | Trig. 32 : _P_3221 |
2.CC. | Kuvaevite | Ir5Ni10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC. | Torryweiserite | Rh5Ni10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC. | Tamuraite | Ir5Fe10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC. | Ferrotorryweiserite | Rh5Fe10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC.05 | Achávalite | FeSe | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Breithauptite | NiSb | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Freboldite | CoSe | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Kotulskite | Pd(Te,Bi)2-x (x ≈ 0.4) | Hex. |
2.CC.05 | Langisite | CoAs | Hex. 6 : _P_63 |
2.CC.05 | Nickeline | NiAs | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m c m |
2.CC.05 | Sederholmite | beta-NiSe | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Sobolevskite | PdBi | Hex. |
2.CC.05 | Stumpflite | PtSb | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Sudburyite | PdSb | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Jaipurite | CoS | Hex. |
2.CC.05 | Zlatogorite | NiCuSb2 | Trig. 3_m_ _(_32/m ) : P_31_m |
2.CC.10 | Pyrrhotite | Fe1-xS | Mon. |
2.CC.10 | Smythite | (Fe,Ni)3+xS4 (x=0-0.3) | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC.10 | Troilite | FeS | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.15 | Modderite | (Co,Fe)As | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.CC.15 | Ruthenarsenite | (Ru,Ni)As | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.CC.15 | Westerveldite | (Fe,Ni,Co)As | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.CC.15 | Minakawaite | RhSb | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.CC.20 | Millerite | NiS | Trig. 3_m_ : R_3_m |
2.CC.20 | Mäkinenite | γ-NiSe | Trig. 3_m_ |
2.CC.20 | UM1990-38-S:CuFeIrNiPtRh | (Ni,Fe,Rh,Cu,Ir,Pt)S | |
2.CC.25 | Mackinawite | FeS | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/n m m |
2.CC.30 | Hexatestibiopanickelite | (Pd,Ni)(Sb,Te) ? | Hex. |
2.CC.30 | Vavřínite | Ni2SbTe2 | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.35a | Braggite | PdPt3S4 | Tet. 4/m : _P_42/m |
2.CC.35b | Cooperite | PtS | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_42/m m c |
2.CC.35a | Vysotskite | PdS | Tet. 4/m : _P_42/m |
2.CC.45 | Jacutingaite | Pt2HgSe3 | Trig. 3_m_ _(_32/m ) : _P_3_m_1 |
2.CC.50 | Imgreite | NiTe (?) | Hex. |
Other InformationHide
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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 CherepanoviteHide
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References for CherepanoviteHide
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Reference List:
Localities for CherepanoviteHide
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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.
Locality ListHide
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- 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.