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Pingguite

A valid IMA mineral species
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About PingguiteHide

Formula:
Bi6Te2O15
Originally assumed to be Bi6Te4+2O13.
Colour:
Yellow-green
Lustre:
Adamantine, Vitreous
Hardness:
5½ - 6
Specific Gravity:
8.44
Crystal System:
Orthorhombic
Name:
Named after its locality.
This page provides mineralogical data about Pingguite.


Unique IdentifiersHide

Mindat ID:
7237
Long-form identifier:
mindat:1:1:7237:9
GUID
(UUID V4):
a73fd0b5-e9c9-42cb-90bc-7e4030ca060a

IMA Classification of PingguiteHide

Approved
IMA Formula:
Bi6Te6+2O15
Approval year:
1993
First published:
1994

Classification of PingguiteHide

4.JL.20

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
L : Tellurites with additional anions, without H2O
34.5.4.1

34 : SELENITES, TELLURITES AND SULFITES
5 : A(X3O8)

Mineral SymbolsHide

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

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

Physical Properties of PingguiteHide

Adamantine, Vitreous
Transparency:
Translucent
Colour:
Yellow-green
Streak:
Pale yellow-green
Hardness:
5½ - 6 on Mohs scale
Hardness:
VHN50=449 - 572 kg/mm2 - Vickers
Tenacity:
Brittle
Density:
8.44 g/cm3 (Measured)    8.64 g/cm3 (Calculated)

Optical Data of PingguiteHide

Type:
Biaxial
RI values:
nα = 2.000 nβ = 2.145
Max Birefringence:
δ = 2.000
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Surface Relief:
Very High
Dispersion:
relatively weak
Reflectivity:
WavelengthR
470nm14.84%
546nm13.03%
589nm13.25%
650nm13.64%

Reflectance graph
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 14.84%.

Chemistry of PingguiteHide

Mindat Formula:
Bi6Te2O15

Originally assumed to be Bi6Te4+2O13.

Crystallography of PingguiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm (2/m 2/m 2/m) - Dipyramidal
Space Group:
Pnma
Cell Parameters:
a = 10.637(2) Å, b = 22.797(4) Å, c = 5.4136(11) Å
Ratio:
a:b:c = 0.467 : 1 : 0.237
Unit Cell V:
1,312.75 ų (Calculated from Unit Cell)
Morphology:
Granular aggregates, tiny crystals.
Comment:
Originally assumed to have a = 5.689, b = 10.791, c = 5.308 Å.

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.146 Å(100)
2.841 Å(80)
2.694 Å(20)
1.956 Å(10)
1.695 Å(20)
1.631 Å(10)

Geological EnvironmentHide

Type Occurrence of PingguiteHide

General Appearance of Type Material:
Granular aggregates, to 0.5 mm in diameter, that consist of tabular grains up to 0.6 µm long.
Place of Conservation of Type Material:
Geological Museum of China, Beijing, China
Geological Setting of Type Material:
Oxidation zone of a gold deposit
Associated Minerals at Type Locality:

Synonyms of PingguiteHide

Other Language Names for PingguiteHide

German:Pingguit
Simplified Chinese:平谷矿
Spanish:Pingguita

Related Minerals - Strunz-mindat GroupingHide

4.JL.TomiolloiteAl12(Te4+O3)5[(SO3)0.5(SO4)0.5](OH)24Hex. 6/m : P63/m
4.JL.05RodalquilariteFe2(TeO2OH)3(TeO3)ClTric. 1 : P1
4.JL.10MackayiteFe3+(Te4+2O5)(OH)Tet. 4/mmm (4/m 2/m 2/m) : I41/acd
4.JL.15MroseiteCaTe4+(CO3)O2Orth. mmm (2/m 2/m 2/m) : Pbca
4.JL.25Tlapallite(Ca,Pb)3CaCu6[Te4+3Te6+O12]2(Te4+O3)2(SO4)2 · 3H2OTrig. 3 2 : P3 2 1
4.JL.30GirditeH2Pb3(Te4+O3)(Te6+O6)Mon. m
4.JL.40BodieiteBi2(TeO3)2(SO4)Mon. 2/m

Other InformationHide

Thermal Behaviour:
TGA showed no significant weight loss, and DTA showed a small endothermic peak at about 800 °C.
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 PingguiteHide

References for PingguiteHide

Localities for PingguiteHide

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

- 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.
China (TL)
 
  • Beijing
    • Pinggu District
Zhifu Sun et al. (1994)
Poland
 
  • Lower Silesian Voivodeship
    • Kamienna Góra County
      • Gmina Kamienna Góra
        • Rędziny
Parafiniuk J. 2003: Secondary bismuth and tellurium minerals from Rędziny (SW Poland) +1 other reference
Russia
 
  • Chukotka Autonomous Okrug
    • Okhotsk-Chukotka belt
Sidorov et al. (2007, November)
Sweden
 
  • Västerbotten County
    • Skellefteå
      • Skellefte mining district
        • Sandfors
Aksel Osterlof specimen +1 other reference
USA
 
  • California
    • San Bernardino County
      • Silver Lake Mining District
        • Soda Mountains
          • Zzyzx
Collected by and in the collection of ... +1 other reference
In the collection of Alex Earl
 
矿物 and/or 产地  
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