Cabriite (original) (raw)
A valid IMA mineral species
About CabriiteHide
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Colour:
White, pink with a slight violet tint
Crystal System:
Orthorhombic
Name:
Named in honor of Louis Jean Cabri (23 February 1934, Cairo - ), Canadian mineralogist, formerly with Canada Centre for Mineral and Energy Technology (CANMET), Ottawa, a world renowned specialist in platinum-group minerals (PGM), for his many contributions to the mineralogy and geochemistry of this group. Cabri described many new PGM species from localities around the world and was the coeditor of Canadian Mineralogist (1975-1982).
This page provides mineralogical data about Cabriite.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:837:2
5d463d32-ef18-4b23-8746-c401dd25bff4
IMA Classification of CabriiteHide
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Type description reference:
Classification of CabriiteHide
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1.AG.30
1 : ELEMENTS (Metals and intermetallic alloys; metalloids and nonmetals; carbides, silicides, nitrides, phosphides)
A : Metals and Intermetallic Alloys
G : PGE-metal alloys
1.2.11.
1 : NATIVE ELEMENTS AND ALLOYS
2 : Platinum Group Metals and Alloys
1.70
1 : Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and Au)
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 |
---|---|---|
Cbr | 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 CabriiteHide
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Colour:
White, pink with a slight violet tint
Hardness:
VHN50=258 - 282 kg/mm2 - Vickers
Density:
11.1 g/cm3 (Measured) 10.7 g/cm3 (Calculated)
Optical Data of CabriiteHide
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Anisotropism:
Strong in grayish brown to golden colors
Bireflectance:
Detectable in air
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
400nm | 40.5% | 40.7% |
440nm | 41.7% | 42.0% |
480nm | 44.4% | 42.6% |
520nm | 47.8% | 44.0% |
560nm | 51.3% | 45.7% |
600nm | 55.6% | 48.6% |
640nm | 61.2% | 52.9% |
680nm | 66.8% | 57.9% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 66.8%.
R1 shown in black, R2 shown in red
Chemistry of CabriiteHide
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Common Impurities:
Pt,Ag,Sb
Crystallography of CabriiteHide
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Crystal System:
Orthorhombic
Class (H-M):
m m m _(_2/_m_2/_m_2/m ) - Dipyramidal
Cell Parameters:
a = 7.88(5) Å, b = 7.88(5) Å, c = 3.94(2) Å
Ratio:
a:b:c = 1 : 1 : 0.5
Unit Cell V:
244.65 ų (Calculated from Unit Cell)
Morphology:
Grains to 200 microns.
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.29 Å | (100) |
2.17 Å | (90) |
1.230 Å | (80) |
1.217 Å | (40) |
1.840 Å | (30b) |
1.434 Å | (30b) |
1.182 Å | (30) |
Geological EnvironmentHide
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Type Occurrence of CabriiteHide
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General Appearance of Type Material:
Place of Conservation of Type Material:
Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia.
Mineragraphy Laboratory of IGEM, Russian Academy of Sciences, Moscow, Russia.
National Mineral Collection, Geological Survey of Canada, Ottawa, Ontario, Canada.
Geological Setting of Type Material:
Copper-nickel sulfide deposit.
Associated Minerals at Type Locality:
Reference:
Estigneeva, T.L., Genkin, A.D. (1983) Cabriite, Pd2SnCu, a new mineral species in the mineral group of palladium, tin and copper compounds. The Canadian Mineralogist: 21: 481-487.
Synonyms of CabriiteHide
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Other Language Names for CabriiteHide
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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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1.AG. | Michitoshiite-(Cu) | Rh(Cu1-xGex) | Iso. m_3_m _(_4/_m_32/m ) : P m_3_m |
---|---|---|---|
1.AG. | Palladothallite | Pd3Tl | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_4/m m m |
1.AG. | Sluzhenikinite | Pd15(Sb7-xSnx) | Mon. 2/m : _P_21/m |
1.AG. | Driekopite | PtBi | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
1.AG. | Sidorovite | Fe3Pt | Iso. m_3_m _(_4/_m_32/m ) : P m_3_m |
1.AG.05 | Hexaferrum | (Fe,Os,Ru,Ir) | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
1.AG.05 | Garutiite | (Ni,Fe,Ir) | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
1.AG.10 | Atokite | (Pd,Pt)3Sn | Iso. m_3_m _(_4/_m_32/m ) : F m_3_m |
1.AG.10 | Rustenburgite | (Pt,Pd)3Sn | Iso. m_3_m _(_4/_m_32/m ) : F m_3_m |
1.AG.10 | Zvyagintsevite | Pd3Pb | Iso. m_3_m _(_4/_m_32/m ) : P m_3_n |
1.AG.15 | Taimyrite | (Pd,Cu,Pt)3Sn | Orth. |
1.AG.15 | Tatyanaite | (Pt,Pd,Cu)9Cu3Sn4 | Orth. |
1.AG.20 | Paolovite | Pd2Sn | Orth. m m m _(_2/_m_2/_m_2/m ) |
1.AG.25 | Plumbopalladinite | Pd3Pb2 | Hex. 6_m_ m : P_63_m c |
1.AG.25 | Stannopalladinite | (Pd,Cu)3Sn | Orth. |
1.AG.35 | Chengdeite | Ir3Fe | Iso. m_3_m _(_4/_m_32/m ) |
1.AG.35 | Isoferroplatinum | Pt3Fe | Iso. m_3_m _(_4/_m_32/m ) |
1.AG.40 | Ferronickelplatinum | Pt2FeNi | Tet. |
1.AG.40 | Tetraferroplatinum | PtFe | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m m m |
1.AG.40 | Tulameenite | Pt2CuFe | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m m m |
1.AG.45 | Hongshiite | PtCu | Trig. |
1.AG.45 | Skaergaardite | PdCu | Iso. m_3_m _(_4/_m_32/m ) : P m_3_m |
1.AG.50 | Yixunite | Pt3In | Iso. m_3_m _(_4/_m_32/m ) |
1.AG.55 | Damiaoite | PtIn2 | Iso. m_3_m _(_4/_m_32/m ) : F m_3_m |
1.AG.60 | Niggliite | PtSn | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
1.AG.65 | Bortnikovite | Pd4Cu3Zn | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m m m |
1.AG.70 | Nielsenite | PdCu3 | Tet. 4_m_ m : P_4_m m |
1.AG.75 | Norilskite | (Pd,Ag)2xPb (x = 0.08 - 0.11) | Trig. 32 : _P_3121 |
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 CabriiteHide
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References for CabriiteHide
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Reference List:
Localities for CabriiteHide
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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.