Nickeltyrrellite (original) (raw)
A valid IMA mineral species
About NickeltyrrelliteHide
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Specific Gravity:
7.36 (Calculated)
Name:
In allusion to being the Ni-dominant analogue of tyrrellite.
The Ni analogue of tyrrellite. Unique combination of elements.
Nickeltyrrellite formed in response to alteration of quijarroite + hansblockite + watkinsonite + clausthalite + penroseite aggregates by oxidizing, low-T, Cu-Ni-Co-Pb-bearing fluids at a fSe2/fS2 ratio greater than unity (Förster et al. 2019).
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:53346:1
abd64eba-499d-4fac-b968-167203855fbe
IMA Classification of NickeltyrrelliteHide
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Type description reference:
Förster, Hans-Jürgen, Ma, Chi, Grundmann, Günter, Bindi, Luca, Stanley, Christopher J. (2019) Nickeltyrrellite, CuNi2Se4, a new member of the spinel supergroup from El Dragón, Bolivia. The Canadian Mineralogist, 57 (5) 637-646 doi:10.3749/canmin.1900025
Classification of NickeltyrrelliteHide
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2.DA.05
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
D : Metal Sulfides, M: S = 3 :4 and 2:3
A : M:S = 3:4
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 |
---|---|---|
Nty | 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 NickeltyrrelliteHide
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Hardness Data:
Could not be measured
Parting:
No obvious parting
Fracture:
Irregular/Uneven
Density:
7.36 g/cm3 (Calculated)
Optical Data of NickeltyrrelliteHide
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Anisotropism:
Between crossed polarizers, it is isotropic
Reflectivity:
Wavelength | R |
---|---|
400nm | 42.1% |
420nm | 43.3% |
440nm | 44.4% |
460nm | 45.4% |
470nm | 45.9% |
480nm | 46.2% |
500nm | 46.7% |
520nm | 47.1% |
540nm | 47.5% |
546nm | 47.6% |
560nm | 47.8% |
580nm | 48.3% |
589nm | 48.1% |
600nm | 48.8% |
620nm | 49.9% |
640nm | 49.7% |
650nm | 49.8% |
660nm | 50.1% |
680nm | 50.5% |
700nm | 51.0% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 51.0%.
Chemistry of NickeltyrrelliteHide
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Crystallography of NickeltyrrelliteHide
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Class (H-M):
m_3_m _(_4/_m_32/m ) - Hexoctahedral
Cell Parameters:
a = 9.99 Å
Morphology:
Anhedral to subhedral grains (up to 20 μm in size).
Comment:
Measured using electron back- scatter diffraction (EBSD)
X-Ray Powder DiffractionHide
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Comments:
X-ray powder diffraction pattern not available (CNMNC Newsletter No. 47). Structure was determined using Electron Backscatter Diffraction (EBSD).
Geological EnvironmentHide
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Type Occurrence of NickeltyrrelliteHide
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General Appearance of Type Material:
Anhedral to subhedral grains (up to 20 μm in size).
Place of Conservation of Type Material:
Type material is deposited in the mineralogical collections of the Natural History Museum, London, catalogue number BM2018,19 (holotype), and the Mineralogical State Collection Munich − Museum Reich der Kristalle, inventory number MSM 73587 (cotype).
Empirical Formula of Type Material:
Cu1.00(Ni1.42Co0.56Fe0.02)Σ2.00(Se3.84S0.16)Σ4.00
Chemical Analysis of Type Material:
Cu | 13.01 % |
---|---|
Fe | 0.27 % |
Co | 6.66 % |
Ni | 16.98 % |
S | 1.04 % |
Se | 61.91 % |
Total: | 99.87 % |
Geological Setting of Type Material:
In a series of thinly stratified, pyrite-rich black shales and reddish-grey, hematite-bearing silt-stones of probably Devonian age. These rocks host a single vein from 0.5 to 2 cm in thickness, rich in selenium.
Associated Minerals at Type Locality:
Reference:
Förster, H.-J., Ma, C. Grundmann, G., Bindi, L., Stanley, C.J. (2019) Nickeltyrrellite, CuNi2Se4, a New Member of the Spinel Supergroup from El Dragón, Bolivia. The Canadian Mineralogist: 57 (5): 637–646.
Synonyms of NickeltyrrelliteHide
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Relationship of Nickeltyrrellite to other SpeciesHide
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Other Members of this group:
Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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2.DA. | Zaykovite | Rh3Se4 | Mon. 2/m : _B_2/m |
---|---|---|---|
2.DA. | Grimmite | NiCo2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA. | Zolenskyite | FeCr2S4 | Mon. 2/m : _B_2/m |
2.DA. | Ezochiite | Cu+(Rh3+Pt4+)S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA. | Ferrodimolybdenite | FeMo2S4 | Mon. 2/m : _B_2/b |
2.DA.05 | Bornhardtite | Co2+Co3+2Se4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Carrollite | CuCo2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Cuproiridsite | (Cu,Fe)Ir2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Cuprorhodsite | (Cu1+0.5Fe3+0.5)Rh3+2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Daubréelite | Fe2+Cr3+2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Fletcherite | CuNi2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Florensovite | (Cu,Zn)Cr1.5Sb0.5S4 | Iso. m_3_m _(_4/_m_32/m ) |
2.DA.05 | Greigite | Fe2+Fe3+2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Indite | FeIn2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Kalininite | ZnCr2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Linnaeite | Co2+Co3+2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Malanite | Cu1+(Ir3+Pt4+)S4 | Iso. m_3_m _(_4/_m_32/m ) |
2.DA.05 | Polydymite | Ni2+Ni3+2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Siegenite | CoNi2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Trüstedtite | Ni3Se4 | Iso. |
2.DA.05 | Tyrrellite | Cu(Co3+,Ni3+)2Se4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Violarite | Fe2+Ni3+2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Xingzhongite | Pb2+Ir3+2S4 | Iso. |
2.DA.05 | Cadmoindite | CdIn2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Cuprokalininite | CuCr2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Joegoldsteinite | MnCr2S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.05 | Shiranuiite | Cu+(Rh3+Rh4+)S4 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
2.DA.10 | Rhodostannite | Cu1+(Fe2+0.5Sn4+1.5)S4 | Tet. 4/m : _I_41/a |
2.DA.10 | Toyohaite | Ag1+(Fe2+0.5Sn4+1.5)S4 | Tet. 4/m : _I_41/a |
2.DA.15 | Brezinaite | Cr3S4 | Mon. 2/m |
2.DA.15 | Heideite | (Fe,Cr)1.15(Ti,Fe)2S4 | Mon. 2/m |
2.DA.20 | Inaglyite | Cu3Pb(Ir,Pt)8S16 | Hex. |
2.DA.20 | Konderite | Cu3Pb(Rh,Pt,Ir)8S16 | Hex. 6/m : _P_6/m |
2.DA.25 | Kingstonite | (Rh,Ir,Pt)3S4 | Mon. 2/m : _B_2/m |
Fluorescence of NickeltyrrelliteHide
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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 NickeltyrrelliteHide
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References for NickeltyrrelliteHide
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Reference List:
Miyawaki, Ritsuro, Hålenius, Ulf, Hatert, Frédéric, Pasero, Marco, Mills, Stuart J. (2019) IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) NEWSLETTER 47. European Journal of Mineralogy, 31 (1) 197-202 doi:10.1127/ejm/2019/0031-2839
Förster, Hans-Jürgen, Ma, Chi, Grundmann, Günter, Bindi, Luca, Stanley, Christopher J. (2019) Nickeltyrrellite, CuNi2Se4, a new member of the spinel supergroup from El Dragón, Bolivia. The Canadian Mineralogist, 57 (5) 637-646 doi:10.3749/canmin.1900025
Localities for NickeltyrrelliteHide
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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.
Bolivia (TL) | |
---|---|
Potosí Antonio Quijarro Province Porco Municipality ⓘ El Dragón mine (TL) | Förster et al. (2019) +1 other reference |