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Cheremnykhite

A valid IMA mineral species
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Formula:
Pb3Zn3(VO4)2(TeO6)
Colour:
Greenish yellow
Lustre:
Adamantine
Hardness:
Specific Gravity:
6.44
Crystal System:
Orthorhombic
Member of:
Name:
Named for I.M. Cheremnykh (И. М. Черемных) (1928–), geologist, a discoverer of the Kuranakh deposit.
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Unique IdentifiersHide

Mindat ID:
989
Long-form identifier:
mindat:1:1:989:4
GUID
(UUID V4):
90ed8be7-ace6-4438-ba1d-ae51e30d785d

IMA Classification of CheremnykhiteHide

Classification of CheremnykhiteHide

8.DL.20

8 : PHOSPHATES, ARSENATES, VANADATES
D : Phosphates, etc. with additional anions, with H2O
L : With large and medium-sized cations, (OH, etc.):RO4 = 2:1
43.2.5.3

43 : COMPOUND PHOSPHATES, ETC.
2 : Anhydrous Normal Compound Phosphates, etc·
28.4.12

28 : Selenites, Selenates, Tellurites, and Tellurates
4 : Tellurates

Mineral SymbolsHide

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

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

Physical Properties of CheremnykhiteHide

Adamantine
Transparency:
Transparent
Colour:
Greenish yellow
Streak:
White
Hardness:
5½ on Mohs scale
Hardness:
VHN10=673 kg/mm2 - Vickers
Tenacity:
Brittle
Cleavage:
Perfect
One perfect
Density:
6.44 g/cm3 (Measured)    6.39 g/cm3 (Calculated)

Optical Data of CheremnykhiteHide

Type:
Biaxial (-)
RI values:
nα = 1.986 nβ = 1.997 nγ = 1.997
2V:
Measured: 20° , Calculated: 24°
Max Birefringence:
δ = 0.011
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Surface Relief:
Very High
Dispersion:
r > v
Pleochroism:
Not Visible
Comments:
X=a, Y=b, Z=c

Chemistry of CheremnykhiteHide

Mindat Formula:
Pb3Zn3(VO4)2(TeO6)
Common Impurities:
As

Crystallography of CheremnykhiteHide

Crystal System:
Orthorhombic
Cell Parameters:
a = 8.58(3) Å, b = 14.86(5) Å, c = 5.18(3) Å
Ratio:
a:b:c = 0.577 : 1 : 0.349
Unit Cell V:
660.44 ų (Calculated from Unit Cell)
Z:
2
Morphology:
Tabular crystals, with well-developed {100} and {010}
Comment:
Point Group: 2/m 2/m 2/m, mm2, or 222.; Space Group: Cmmm, Cmm2, Cm2m, or C222.

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.30 Å(10)
3.00 Å(9)
1.607 Å(6)
1.903 Å(5)
2.470 Å(4)
3.66 Å(3)
2.120 Å(3)

Geological EnvironmentHide

Type Occurrence of CheremnykhiteHide

General Appearance of Type Material:
Elongate tabular crystals, 0.1 to 0.5 mm.
Place of Conservation of Type Material:
Institute of Geosciences, Yakutsk Scientific Center, Academy of Sciences, Yakutsk, Russia, mk-113.
Associated Minerals at Type Locality:
Reference:
Kim, A.A., Zayakina, N.V., Makhotko, V.F. (1990) Kuksite Pb3Zn3TeO6(PO4)2 and cheremnykhite Pb3Zn3TeO6(VO4)2—new tellurates from the Kuranakh gold deposit (Central Aldan, southern Yakutia). Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva: 119(5): 50-57.

Synonyms of CheremnykhiteHide

Other Language Names for CheremnykhiteHide

Relationship of Cheremnykhite to other SpeciesHide

Member of:
Other Members of this group:
DugganitePb3Zn3(AsO4)2(TeO6)Trig. 3 2 : P3 2 1
JoëlbruggeritePb3Zn3(Sb5+,Te6+)As2O13(OH,O)Trig. 3 2 : P3 2 1
KuksitePb3Zn3(PO4)2(TeO6)Trig. 3 2 : P3 2 1

Related Minerals - Strunz-mindat GroupingHide

8.DL.05FoggiteCaAl(PO4)(OH)2 · H2OOrth. mmm (2/m 2/m 2/m)
8.DL.10CyriloviteNaFe3+3(PO4)2(OH)4 · 2H2OTet. 4 2 2 : P41 21 2
8.DL.10Millisite(Na,K)CaAl6(PO4)4(OH)9 · 3H2OTet.
8.DL.10WarditeNaAl3(PO4)2(OH)4 · 2H2OTet. 4 2 2 : P41 21 2
8.DL.10FluorowarditeNaAl3(PO4)2F2(OH)2(H2O)2 Tet. 4 2 2 : P41 21 2
8.DL.15Agardite-(Nd)NdCu6(AsO4)3(OH)6 · 3H2OHex. 6/m : P63/m
8.DL.15Agardite-(Y)YCu6(AsO4)3(OH)6 · 3H2OHex. 6/m : P63/m
8.DL.15Agardite-(Ce)CeCu6(AsO4)3(OH)6 · 3H2OHex. 6/m : P63/m
8.DL.15Agardite-(Dy)(Dy,La)Cu6(AsO4)3(OH)6 · 3H2OHex.
8.DL.15Agardite-(La)LaCu6(AsO4)3(OH)6 · 3H2OHex. 6/m : P63/m
8.DL.15GoudeyiteAlCu6(AsO4)3(OH)6 · 3H2OHex.
8.DL.15MixiteBiCu6(AsO4)3(OH)6 · 3H2OHex. 6/m : P63/m
8.DL.15Petersite-(Y)(Y,Ce,Nd)Cu6(PO4)3(OH)6 · 3H2OHex.
8.DL.15ZálesíiteCaCu6(AsO4)2(AsO3OH)(OH)6 · 3H2OHex. 6/m : P63/m
8.DL.15Plumboagardite(Pb,REE,Ca)Cu6(AsO4)3(OH)6 · 3H2OHex. 6/m : P63/m
8.DL.15CalciopetersiteCaCu6(PO4)2(PO3OH)(OH)6 · 3H2OHex. 6/m : P63/m
8.DL.15Petersite-(Ce)Cu6Ce(PO4)3(OH)6 · 3H2OHex. 6/m : P63/m
8.DL.15Petersite-(La)Cu6La(PO4)3(OH)6 · 3H2OHex. 6/m : P63/m
8.DL.20DugganitePb3Zn3(AsO4)2(TeO6)Trig. 3 2 : P3 2 1
8.DL.20KuksitePb3Zn3(PO4)2(TeO6)Trig. 3 2 : P3 2 1
8.DL.20WallkilldelliteCa2Mn2+3(AsO4)2(OH)4 · 9H2OHex.
8.DL.20Wallkilldellite-(Fe)(Ca,Cu)4Fe2+6(AsO4,SiO4)4(OH,O)8 · 18H2OHex.
8.DL.25AngastoniteCaMgAl2(PO4)2(OH)4 · 7H2OAmor.
8.DL.30LångbanshyttanitePb2Mn2Mg(AsO4)2(OH)4 · 6H2OTric. 1 : P1

Fluorescence of CheremnykhiteHide

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 CheremnykhiteHide

References for CheremnykhiteHide

Localities for CheremnykhiteHide

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.
Russia
 
  • Sakha
    • Aldan
      • Kuranakh ore field
Kondratieva et al. (2021)
Kim et al. (1990) +3 other references
 
and/or  
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