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Příbramite

A valid IMA mineral species
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Formula:
CuSbSe2
Colour:
Lead grey
Lustre:
Metallic
Hardness:
3 - 4
Specific Gravity:
5.884 (Calculated)
Crystal System:
Orthorhombic
Name:
Named for the type locality.
The Se analogue of chalcostibite.

Chemically related to permingeatite and bytízite.

The associates also include a new Hg-Cu-Sb selenide and a new Sb-Cu selenide.

There is a single Cu and single Sb site in the structure, which also contains two Se sites. Sb environment is square-pyramidal, and links to form SbSe2 chains || b; Cu forms CuSe4 tetrahedra also forming chains, CuSe3 composition, that are also parallel to b. The two chain types joint to give sheets perpendicular to c.


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Name EncodingHide

CP1252:
Príbramite
Latin-1:
Príbramite
ASCII-7:
Pribramite

Unique IdentifiersHide

Mindat ID:
47784
Long-form identifier:
mindat:1:1:47784:6

Similar NamesHide

IMA Classification of PříbramiteHide

Classification of PříbramiteHide

2.HA.05

2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
H : Sulfosalts of SnS archetype
A : With Cu, Ag, Fe (without Pb)

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
PbmIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of PříbramiteHide

Metallic
Transparency:
Opaque
Colour:
Lead grey
Hardness:
3 - 4 on Mohs scale
Hardness Data:
Estimated
Comment:
By analogy to chalcostibite.
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
None observed
Density:
5.884 g/cm3 (Calculated)
Comment:
Calculated value based on the empirical formula.

Optical Data of PříbramiteHide

Anisotropism:
Strong, grey to brownish rotation tints
Bireflectance:
Medium
Reflectivity:
WavelengthR1 (%)R2 (%)
400nm39.6%42.1%
420nm39.9%43.1%
440nm39.9%43.9%
460nm39.9%44.6%
470nm39.8%44.8%
480nm39.8%44.9%
500nm39.9%45.2%
520nm40.1%45.6%
540nm40.4%46.0%
546nm40.4%46.2%
560nm40.6%46.4%
580nm40.5%46.6%
589nm40.4%46.5%
600nm40.2%46.4%
620nm39.8%45.9%
640nm39.2%45.2%
650nm38.9%44.8%
660nm38.5%44.3%
680nm38.1%43.6%
700nm37.4%42.8%


Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 46.6%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Grey with a yellowish hue
Internal Reflections:
Not observed
Pleochroism:
Weak
Comments:
Grey tints

Chemistry of PříbramiteHide

Mindat Formula:
CuSbSe2
Element Weights:
Element% weight
Se46.011 %
Sb35.475 %
Cu18.514 %

Calculated from ideal end-member formula.
Common Impurities:
Fe,Pb,Tl,Hg

Crystallography of PříbramiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm (2/m 2/m 2/m) - Dipyramidal
Space Group:
Pnma
Cell Parameters:
a = 6.3042(15) Å, b = 3.980(1) Å, c = 14.989(4) Å
Ratio:
a:b:c = 1.584 : 1 : 3.766
Unit Cell V:
376.09 ų
Z:
4

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
High-? alteration and/or metamorphism
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Type Occurrence of PříbramiteHide

General Appearance of Type Material:
Columnar crystals, up to 60 × 112 μm, forming aggregates up to 150 μm across, in calcite vein; intergrown with and replacing older permingeatite; also closely associated with antimonselite.
Place of Conservation of Type Material:
Cotypes: (1) Department of Mineralogy and Petrology, National Museum, Cirkusová 1740, Praha 9, Czech Republic (catalogue number P1P 15/2015) and (2) the Mining Museum Příbram, Czech Republic (catalogue number 1/2016).
Empirical Formula of Type Material:
Cu1.00(Sb1.02As0.01)1.03(Se1.81S0.15)1.96
Chemical Analysis of Type Material:
Cu18.52 %
Sb35.47 %
Se46.01 %
Total:100 %
Associated Minerals at Type Locality:

Synonyms of PříbramiteHide

Other Language Names for PříbramiteHide

Relationship of Příbramite to other SpeciesHide

Other Members of Chalcostibite Group:
ChalcostibiteCuSbS2Orth. mmm (2/m 2/m 2/m)
EmplectiteCuBiS2Orth. mmm (2/m 2/m 2/m) : Pmna
GrundmanniteCuBiSe2Orth. mmm (2/m 2/m 2/m) : Pnma

Related Minerals - Strunz-mindat GroupingHide

2.HA.05GrundmanniteCuBiSe2Orth. mmm (2/m 2/m 2/m) : Pnma
2.HA.05EmplectiteCuBiS2Orth. mmm (2/m 2/m 2/m) : Pmna
2.HA.05Hansblockite(Cu,Hg)(Bi,Pb)Se2Mon. 2/m : P21/b
2.HA.05ChalcostibiteCuSbS2Orth. mmm (2/m 2/m 2/m)
2.HA.10MiargyriteAgSbS2Mon. 2/m : B2/b
2.HA.20SunshuiteFeBi2S4Mon. 2/m : B2/m
2.HA.20GaravelliteFeSbBiS4Orth.
2.HA.20BerthieriteFeSb2S4Orth. mmm (2/m 2/m 2/m)
2.HA.20GraţianiteMnBi2S4Mon. 2/m : B2/m
2.HA.20CleriteMnSb2S4Orth. mmm (2/m 2/m 2/m)
2.HA.25AramayoiteAg3Sb2(Bi,Sb)S6Tric. 1 : P1
2.HA.25BaumstarkiteAg3Sb3S6Tric. 1 : P1
2.HA.30ZhonghongiteCu29(As,Sb)12S33Orth. mm2 : Fmm2

Other InformationHide

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 PříbramiteHide

References for PříbramiteHide

Localities for PříbramiteHide

Showing 3 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the Image symbol to view information about a locality. The Image symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

Image - This locality has map coordinates listed. Image - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. Image - Good crystals or important locality for species. Image - 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.
China
 
Luming Chen et al. (1995)
Czech Republic
 
  • Central Bohemian Region
Škácha et al. (2017)
      • Háje
        • Uranium Mine No. 16
Mineralogical Magazine +4 other references
 
Image Image
and/or  
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