Tulameenite (original) (raw)
A valid IMA mineral species
About TulameeniteHide
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Specific Gravity:
14.9 (Calculated)
Crystal System:
Tetragonal
Name:
Named after its discovery locality, Tulameen and Similkameen Rivers, British Columbia, Canada.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:4046:0
28943c7d-71e6-4a9a-b56f-d98822ecac02
IMA Classification of TulameeniteHide
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Type description reference:
Classification of TulameeniteHide
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1.AG.40
1 : ELEMENTS (Metals and intermetallic alloys; metalloids and nonmetals; carbides, silicides, nitrides, phosphides)
A : Metals and Intermetallic Alloys
G : PGE-metal alloys
1.2.4.2
1 : NATIVE ELEMENTS AND ALLOYS
2 : Platinum Group Metals and Alloys
1.87
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.
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
Symbol | Source | Reference |
---|---|---|
Tul | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Tul | The Canadian Mineralogist (2019) | The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download |
Physical Properties of TulameeniteHide
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Hardness:
VHN50=420 - 456 kg/mm2 - Vickers
Density:
14.9 g/cm3 (Calculated)
Optical Data of TulameeniteHide
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Colour in reflected light:
white
Chemistry of TulameeniteHide
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Common Impurities:
Ir,Ni,Sb
Crystallography of TulameeniteHide
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Crystal System:
Tetragonal
Class (H-M):
4/m m m _(_4/_m_2/_m_2/m ) - Ditetragonal Dipyramidal
Cell Parameters:
a = 3.891(2) Å, c = 3.577(2) Å
Unit Cell V:
54.16 ų (Calculated from Unit Cell)
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0005244 | Tulameenite | Bayliss P (1990) Revised unit cell dimensions, space group, and chemical formula of some metallic minerals The Canadian Mineralogist 28 751-755 | 1990 | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.179 Å | (100) |
1.163 Å | (80) |
1.093 Å | (80) |
1.946 Å | (70) |
1.016 Å | (60) |
1.317 Å | (50) |
2.753 Å | (40) |
Geological EnvironmentHide
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Type Occurrence of TulameeniteHide
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Place of Conservation of Type Material:
Royal Ontario Museum, Toronto, Canada, M33256; National Museum of Natural History, Washington, D.C., USA, 128460.
Associated Minerals at Type Locality:
Reference:
CABRI, L.J., OWENS, D.R. & LAFLAMME, J.H.G. (1973): Tulameenite, a new platinum-iron-copper mineral from placers in the Tulameen River area, British Columbia. Canadian Mineralogist 12, 21-25.
Synonyms of TulameeniteHide
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Other Language Names for TulameeniteHide
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Varieties of TulameeniteHide
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Relationship of Tulameenite 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 | 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.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.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 TulameeniteHide
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References for TulameeniteHide
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Localities for TulameeniteHide
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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.