Taimyrite (original) (raw)
A valid IMA mineral species
About TaimyriteHide
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Crystal System:
Orthorhombic
Name:
Named after its discovery locality, the Talnakh deposit, Noril'sk-Talnakh Ni-Cu camp, Taymyr autonomous district, Russia. At some point the name was chnaged to taimyrite-I, but the name was reverted back to taimyrite in 2022.
Note: "Taimyrite-II" is a unapproved species.
Compare the chemically similar copper-free Atokite.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:3870:2
1bc156c2-b55d-4a0f-8da6-99e68c045acc
IMA Classification of TaimyriteHide
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IMA Formula:
(Pd,Pt)9Cu3Sn4
Type description reference:
Classification of TaimyriteHide
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1.AG.15
1 : ELEMENTS (Metals and intermetallic alloys; metalloids and nonmetals; carbides, silicides, nitrides, phosphides)
A : Metals and Intermetallic Alloys
G : PGE-metal alloys
1.2.10.1
1 : NATIVE ELEMENTS AND ALLOYS
2 : Platinum Group Metals and Alloys
1.71
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 |
---|---|---|
Tmy-I | 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 TaimyriteHide
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Hardness:
VHN50=480(25) kg/mm2 - Vickers
Optical Data of TaimyriteHide
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Anisotropism:
dark gray with a blue tint to yellowish-gray
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
400nm | 33.0% | 37.1% |
430nm | 37.8% | 41.2% |
460nm | 39.6% | 42.3% |
490nm | 42.3% | 45.2% |
520nm | 44.0% | 47.8% |
550nm | 45.5% | 49.6% |
580nm | 47.4% | 51.6% |
610nm | 49.7% | 54.0% |
640nm | 51.4% | 56.5% |
670nm | 53.0% | 59.2% |
700nm | 54.0% | 61.9% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 61.9%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Light gray with a distinct rose tint
Comments:
Distinct; from pale gray with a rose tint to a creamy tint.
Chemistry of TaimyriteHide
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Mindat Formula:
(Pd,Cu,Pt)3Sn
Crystallography of TaimyriteHide
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Crystal System:
Orthorhombic
Cell Parameters:
a = 5.61 Å, b = 4.79 Å, c = 13.56 Å
Ratio:
a:b:c = 1.171 : 1 : 2.831
Unit Cell V:
364.38 ų (Calculated from Unit Cell)
Comment:
Point Group: n.d.; Point Group: n.d.
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.155 Å | (100) |
2.29 Å | (55) |
2.365 Å | (40) |
1.44 Å | (40) |
Geological EnvironmentHide
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Type Occurrence of TaimyriteHide
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General Appearance of Type Material:
Rounded inclusions, sometimes vein-like up to 12 mm long but most often 0.3-0.5 mm in diameter.
Place of Conservation of Type Material:
Fersman Mineralogical Museum, Academy of Sciences, Moscow, Russia and in the Mineralogical Museum of the Moscow Geological-Prospecting Institute.
Associated Minerals at Type Locality:
Reference:
Begizov, V.D., Sluzhenikin, S.F. (1976) On the compositions of some platinum minerals from the northwest and extreme north of the Talnakh ore junction. TSentral’nyĭ Nauchno-issledovatelʹskiĭ Geologorazvedochnyĭ Institut TSvetnykh i Blagorodnykh Metallov: 122: 107-116.
Synonyms of TaimyriteHide
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Other Language Names for TaimyriteHide
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Simplified Chinese:锡铜钯矿
Traditional Chinese:錫銅鈀礦
Relationship of Taimyrite to other SpeciesHide
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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 | 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.30 | Cabriite | Pd2CuSn | Orth. m m m _(_2/_m_2/_m_2/m ) : P m m m |
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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Notes:
Not etched by dilute and concentrated acids (H2SO4, HCl, HNO3), browns in 30 seconds in aqua regia and blackens on longer etching.
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 TaimyriteHide
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References for TaimyriteHide
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Reference List:
Dunn, P. J., Fleischer, M., Chao, G. Y., Cabri, L. J., Mandarino, J. A. (1983) New mineral names. American Mineralogist, 68 (11-12) 1248-1252
Localities for TaimyriteHide
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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.