Cuproneyite (original) (raw)
A valid IMA mineral species
About CuproneyiteHide
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Specific Gravity:
7.113 (Calculated)
Crystal System:
Monoclinic
Name:
For the mineral neyite and its copper content.
Cu analogue of neyite.
‘Cu-enriched cuproneyite’ may be explained by aikinite nanoinclusions in cuproneyite (Ciobanu et al., 2016).
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:39287:3
4ab88fe3-e748-4e23-ad63-3e7f2a04716d
IMA Classification of CuproneyiteHide
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Type description reference:
Ilinca, G., Makovicky, E., Topa, D., Zagler, G. (2012) Cuproneyite, Cu7Pb27Bi25S68, a new mineral species from Băiţa Bihor, Romania. The Canadian Mineralogist, 50 (2) 353-370 doi:10.3749/canmin.50.2.353
Classification of CuproneyiteHide
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2.JB.25i
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
J : Sulfosalts of PbS archetype
B : Galena derivatives, with Pb
3.5.1.2
3 : SULFOSALTS
5 : 2.5 < ø < 3
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 |
---|---|---|
Cney | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Pronunciation of CuproneyiteHide
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Pronunciation:
Play | Recorded by | Country |
---|---|---|
Sorry, your browser doesn't support HTML5 audio. | Jolyon Ralph | United Kingdom |
Physical Properties of CuproneyiteHide
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Hardness:
VHN25=222 kg/mm2 - Vickers
Cleavage:
Perfect
Parallel to the c axis
Fracture:
Irregular/Uneven
Comment:
Fracture is subparallel, perpendicular to the c axis.
Density:
7.113 g/cm3 (Calculated)
Optical Data of CuproneyiteHide
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Anisotropism:
Moderate in air and strong in oil.
Bireflectance:
Bireflectance is perceptible in air and moderate in oil
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
400nm | 40.21% | 50.25% |
420nm | 41.61% | 48.13% |
440nm | 41.9% | 48.12% |
460nm | 40.47% | 47.57% |
470nm | 40.37% | 47.09% |
480nm | 40.63% | 47.17% |
500nm | 40.71% | 47.25% |
520nm | 40.18% | 46.63% |
540nm | 39.48% | 45.85% |
546nm | 39.30% | 45.74% |
560nm | 38.84% | 45.39% |
580nm | 38.38% | 44.67% |
589nm | 38.26% | 44.27% |
600nm | 38.20% | 44.46% |
620nm | 38.04% | 44.18% |
640nm | 37.84% | 43.76% |
650nm | 38.05% | 43.91% |
660nm | 37.79% | 43.59% |
680nm | 37.21% | 43.45% |
700nm | 37.72% | 43.37% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 50.25%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Greyish white
Internal Reflections:
None
Comments:
Greyish white with faint bluish tint (darkest position) to greyish white with faint yellowish tint (lightest position).
Chemistry of CuproneyiteHide
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Mindat Formula:
Cu7Pb27Bi25S68
Crystallography of CuproneyiteHide
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Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Cell Parameters:
a = 37.432(8) Å, b = 4.0529(9) Å, c = 43.545(9) Å
β = 108.803°
Ratio:
a:b:c = 9.236 : 1 : 10.744
Unit Cell V:
6,253.58 ų (Calculated from Unit Cell)
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0019214 | Cuproneyite | Ilinca G, Makovicky E, Topa D, Zagler G (2012) Cuproneyite, Cu7Pb27Bi25S68, a new mineral species from Baita Bihor, Romania The Canadian Mineralogist 50 353-370 | 2012 | skarn deposit of Baita Bihor, Romania | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.735 Å | (96) |
3.507 Å | (50) |
3.464 Å | (53) |
3.347 Å | (84) |
2.956 Å | (77) |
2.925 Å | (46) |
2.867 Å | (100) |
2.027 Å | (81) |
Geological EnvironmentHide
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Type Occurrence of CuproneyiteHide
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General Appearance of Type Material:
Irregular or short prismatic grains, of up to 300 μm in length, intergrown with lamellae and irregular patches of cosalite and Cu–Pb-rich bismuthinite derivatives.
Place of Conservation of Type Material:
Department of Mineralogy, Faculty of Geology and Geophysics, University of Bucharest, Romania (catalogue no. CATMIN 22/24).
Geological Setting of Type Material:
polymetallic mineralization related to contact metamorphism (skarn) developed around the Late Cretaceous magmatic complex at Băiţa Bihor
Associated Minerals at Type Locality:
Reference:
Ilinca, Gh., Makovicky, E., Topa, D., Zagler, G. (2012) Cuproneyite, Cu7Pb27Bi25S68, a new mineral from Băiţa Bihor, Romania. The Canadian Mineralogist: 50: 353-370.
Synonyms of CuproneyiteHide
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Related Minerals - Strunz-mindat GroupingHide
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2.JB. | Senandorite | AgPbSb3S6 | Orth. m _m_2 : P m _n_21 |
---|---|---|---|
2.JB. | Oscarkempffite | Ag10Pb4(Sb17Bi9)S48 | Orth. m _m_2 |
2.JB. | Chukotkaite | AgPb7Sb5S15 | Mon. 2/m : _P_21/b |
2.JB. | Arsenquatrandorite | Ag17.6Pb12.8Sb38.1As11.5S96 | Mon. 2/m : _P_21/b |
2.JB. | Clino-oscarkempffite | Ag15Pb6Sb21Bi18S72 | Mon. 2/m : _P_21/b |
2.JB. | Andreadiniite | CuHgAg7Pb7Sb24S48 | Mon. 2/m : _P_21/b |
2.JB. | Ginelfite | Ag2(Ag0.5Fe)TlPb23.5(Sb,As)33.5S76 | Tric. 1 : _P_1 |
2.JB. | Lazerckerite | Ag3.75Pb4.50(Sb7.75Bi4)S24 | Mon. 2/m |
2.JB. | Lasmanisite | Ag12Pb13Mn11Sb44S96 | Orth. 222 : _P_212121 |
2.JB. | Montpelvouxite | AgPb16Sb27As18S84 | Tric. 1 : _P_1 |
2.JB. | Selenojunoite | Cu2Pb3Bi8Se16 | Mon. 2/m : _B_2/m |
2.JB.05 | Diaphorite | Ag3Pb2Sb3S8 | Mon. 2/m : _P_21/b |
2.JB.10 | Cosalite | Pb2Bi2S5 | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.JB.15 | Freieslebenite | AgPbSbS3 | Mon. 2/m : _P_21/b |
2.JB.15 | Marrite | AgPbAsS3 | Mon. 2/m : _P_21/b |
2.JB.20 | Cannizzarite | Pb48Bi56S132 | Mon. 2/m : _P_21/m |
2.JB.20 | Wittite | Pb9Bi12(S,Se)27 | Mon. |
2.JB.25a | Junoite | Cu2Pb3Bi8(S,Se)16 | Mon. 2/m : _B_2/m |
2.JB.25i | Neyite | Ag2Cu6Pb25Bi26S68 | Mon. 2/m : _B_2/m |
2.JB.25c | Nordströmite | CuPb3Bi7(Se4S10) | Mon. 2/m : _P_21/m |
2.JB.25g | Nuffieldite | Cu1.4Pb2.4Bi2.4Sb0.2S7 | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.JB.25d | Proudite | CuPb7.5Bi9.33(S,Se)22 | Mon. 2/m : _B_2/m |
2.JB.25h | Weibullite | Pb5Bi8Se7S11 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.JB.25b | Felbertalite | Cu2Pb6Bi8S19 | Mon. 2/m : _B_2/m |
2.JB.25j | Rouxelite | Cu2HgPb23Sb27S65.5 | Mon. 2/m : _B_2/m |
2.JB.25f | Ángelaite | Cu2AgPbBiS4 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.JB.30a | Geocronite | Pb14Sb6S23 | Mon. 2/m : _P_21/m |
2.JB.30a | Jordanite | Pb14As6S23 | Mon. 2/m : _P_21/m |
2.JB.30b | Kirkiite | Pb10Bi3As3S19 | Mon. 2/m : _P_21/m |
2.JB.30c | Tsugaruite | Pb28As15S50Cl | Orth. m _m_2 : P n _n_2 |
2.JB.30a | Marcobaldiite | Pb12(Sb3As2Bi)Σ6S21 | Tric. 1 : _P_1 |
2.JB.30a | Arsenmarcobaldiite | Pb12(As3.2Sb2.8)Σ6S21 | Tric. 1 : _P_1 |
2.JB.35c | Pillaite | Pb9Sb10S23ClO0.5 | Mon. 2/m : _B_2/m |
2.JB.35a | Zinkenite | Pb9Sb22S42 | Hex. 6 : _P_63 |
2.JB.35b | Scainiite | Pb14Sb30S54O5 | Mon. 2/m : _B_2/m |
2.JB.35d | Pellouxite | (Cu,Ag)Pb10Sb12S27O(Cl,S)0.6 | Mon. 2/m : _B_2/m |
2.JB.35f | Tubulite | Ag2Pb22Sb20S53 | Mon. m : P b |
2.JB.35e | Chovanite | Pb15-2xSb14+2xS36Ox (x ~ 0.2) | Mon. 2/m : _B_2/m |
2.JB.40b | Aschamalmite | Pb6-3xBi2+xS9 | Mon. 2/m : _B_2/m |
2.JB.40a | Bursaite | Pb5Bi4S11 (?) | Orth. |
2.JB.40b | Eskimoite | Ag7Pb10Bi15S36 | Mon. |
2.JB.40a | Fizélyite | Ag5Pb14Sb21S48 | Mon. 2/m |
2.JB.40a | Gustavite | AgPbBi3S6 | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.JB.40a | Lillianite | Pb3-2xAgxBi2+xS6 | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.JB.40c | Ourayite | Ag3Pb4Bi5S13 | Orth. |
2.JB.40a | Ramdohrite | Pb5.9Fe0.1Mn0.1In0.1Cd0.2Ag2.8Sb10.8S24 | Mon. 2/m |
2.JB.40a | Roshchinite | Ag19Pb10Sb51S96 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.JB.40d | Schirmerite | PbAgBi3S6 - Pb3Ag1.5Bi3.5S9 | Orth. |
2.JB.40a | Treasurite | Ag7Pb6Bi15S32 | Mon. |
2.JB.40a | Uchucchacuaite | AgMnPb3Sb5S12 | Orth. m m m _(_2/_m_2/_m_2/m ) : P m m m |
2.JB.40e | Ustarasite | Pb(Bi,Sb)6S10 (?) | |
2.JB.40a | Vikingite | Ag5Pb8Bi13S30 | Mon. 2/m : _B_2/m |
2.JB.40a | Xilingolite | Pb3Bi2S6 | Mon. |
2.JB.40b | Heyrovskýite | Pb6Bi2S9 | Orth. m m m _(_2/_m_2/_m_2/m ) : C c c m |
2.JB.40 | UM1988-05-S:AgBiCuHgPb | (Hg,Ag,Cu,Pb)5Pb5Bi11S27 | |
2.JB.40 | UM1988-06-S:AgBiCuHgPb | (Pb,Hg)12(Cu,Ag)3(Bi,Sb)10(S,Te)27 | |
2.JB.40a | Quatrandorite | AgPbSb3S6 | Mon. 2/m : _P_21/b |
2.JB.40a | Menchettiite | AgPb2.40Mn1.60Sb3As2S12 | Mon. 2/m : _P_21/b |
2.JB.40a | Terrywallaceite | AgPb(Sb,Bi)3S6 | Mon. 2/m : _P_21/b |
2.JB.40a | Jasrouxite | Ag16Pb4(Sb24As16)S72 | Tric. 1 : _P_1 |
2.JB.40a | Erzwiesite | Ag8Pb12Bi16S40 | Orth. m m m _(_2/_m_2/_m_2/m ) : C m c m |
2.JB.40a | Staročeskéite | Ag0.70Pb1.60(Bi1.35Sb1.35)Σ2.70S6 | Orth. m m m _(_2/_m_2/_m_2/m ) : C m c m |
2.JB.40a | Oyonite | Ag3Mn2Pb4Sb7As4S24 | Mon. 2/m |
2.JB.40a | Holubite | Ag3Pb6(Sb8Bi3)S24 | Mon. 2/m |
2.JB.40b | Baiamareite | Ag4Pb12Fe4Sb20S48 | Mon. 2/m |
2.JB.40a | Tarutinoite | Ag3Pb7Bi7S19 | Mon. 2/m : _B_2/m |
2.JB.55 | Gratonite | Pb9As4S15 | Trig. 3_m_ : R_3_m |
2.JB.60 | Marrucciite | Hg3Pb16Sb18S46 | Mon. 2/m : _B_2/m |
2.JB.65 | Vurroite | Pb20Sn2(Bi,As)22S54Cl6 | Mon. 2/m : _B_2/b |
2.JB.65 | Tazieffite | Pb20Cd2(As,Bi)22S50Cl10 | Mon. 2/m : _B_2/b |
2.JB.70 | Daliranite | PbHgAs2S5 | Mon. |
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 CuproneyiteHide
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References for CuproneyiteHide
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Reference List:
Ilinca, G., Makovicky, E., Topa, D., Zagler, G. (2012) Cuproneyite, Cu7Pb27Bi25S68, a new mineral species from Băiţa Bihor, Romania. The Canadian Mineralogist, 50 (2) 353-370 doi:10.3749/canmin.50.2.353
Localities for CuproneyiteHide
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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.
Romania (TL) | |
---|---|
Bihor County Nucet ⓘ Băiţa mining district (TL) | Ilinca et al. (2012) +1 other reference |