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Shchurovskyite

A valid IMA mineral species
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About ShchurovskyiteHide

06527220017272472433523.jpg
Grigory E. Shchurovsky
Formula:
K2CaCu6O2(AsO4)4
Colour:
olive-green or olive drab
Lustre:
Vitreous
Hardness:
3
Specific Gravity:
4.28 (Calculated)
Crystal System:
Monoclinic
Name:
Named in honor of Grigory Efimovich Shchurovsky (Григорий Ефимович Щуровский) (30 January (11 February) 1803, Moscow, Russian Empire - 20 March (1 April) 1884, Moscow, Russian Empire), geologist, paleontologist, and professor of geology and mineralogy of Moscow University for nearly fifty years.
Chemically related to calcioandyrobertsite, the second K-Ca-Cu-As mineral.

Structurally related to dmisokolovite in terms of general topology. The quasi-framework contains arsenate tetrahedra and Cu-centered polyhedra, with K and Ca in channels.


Unique IdentifiersHide

Mindat ID:
45966
Long-form identifier:
mindat:1:1:45966:4

IMA Classification of ShchurovskyiteHide

Classification of ShchurovskyiteHide

8.BG.25

8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
G : With medium-sized and large cations, (OH, etc.):RO4 = 0.5:1

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

Physical Properties of ShchurovskyiteHide

Vitreous
Transparency:
Transparent
Colour:
Olive-green or olive drab
Streak:
Pale greenish
Hardness:
Tenacity:
Brittle
Cleavage:
None Observed
Parting:
None observed
Fracture:
Irregular/Uneven
Density:
4.28 g/cm3 (Calculated)

Optical Data of ShchurovskyiteHide

Type:
Biaxial (+)
RI values:
nα = 1.795(5) nβ = 1.800(5) nγ = 1.810(6)
2V:
Measured: 70° (15)
Max. Birefringence:
δ = 0.015
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars.

Surface Relief:
Moderate

Chemistry of ShchurovskyiteHide

Mindat Formula:
K2CaCu6O2(AsO4)4
Element Weights:
Element% weight
Cu35.069 %
As27.564 %
O26.488 %
K7.192 %
Ca3.686 %

Calculated from ideal end-member formula.
Common Impurities:
P,S,Zn,(Rb,Al)

Crystallography of ShchurovskyiteHide

Crystal System:
Monoclinic
Class (H-M):
2 - Sphenoidal
Space Group:
B2
Setting:
C2
Cell Parameters:
a = 17.2856(9) Å, b = 5.6705(4) Å, c = 8.5734(6) Å
β = 92.953(6)°
Ratio:
a:b:c = 3.048 : 1 : 1.512
Unit Cell V:
839.23 ų (Calculated from Unit Cell)
Z:
2

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45a : [Sulfates, arsenates, selenates, antimonates]

Type Occurrence of ShchurovskyiteHide

General Appearance of Type Material:
coarse tabular or prismatic crystals up to 0.15 mm in size or anhedral grains forming parallel aggregates and crusts up to 1.5 cm × 2 cm across
Place of Conservation of Type Material:
Type material is deposited in the collections of the Fersman Mineralogical Museum of the Russian Academy of Sciences, Moscow, Russia, registration number 4421/1
Geological Setting of Type Material:
Fumarole
Associated Minerals at Type Locality:

Synonyms of ShchurovskyiteHide

Other Language Names for ShchurovskyiteHide

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Shchurovskyite associated with BradaczekiteNaCu4(AsO4)3

Related Minerals - Strunz-mindat GroupingHide

8.BG.AldomarinoiteSr2Mn3+(AsO4)2(OH)Mon. 2/m : P21/m
8.BG.DongchuanitePb4ZnZn2(PO4)4(OH)2Tric. 1 : P1
8.BG.CuprodongchuanitePb4CuZn2(PO4)4(OH)2Tric. 1 : P1
8.BG.CanosioiteBa2Fe3+(AsO4)2(OH)Mon. 2/m : P21/m
8.BG.05FeinglositePb2Zn(AsO4)2 · H2OMon. 2/m
8.BG.05TokyoiteBa2Mn3+(VO4)2(OH)Mon. 2/m : P21/m
8.BG.05LombardoiteBa2Mn3+(AsO4)2(OH)Mon. 2/m : P21/m
8.BG.05BearthiteCa2Al(PO4)2(OH)Mon. 2/m : P21/m
8.BG.05'Unnamed (possible ordered As-analogue of Tokyoite)'Ba2Mn[(As,V)O4]2(OH)Mon. 2/m : P21/m
8.BG.05GamagariteBa2Fe3+(VO4)2(OH)Mon. 2/m : P21/m
8.BG.05ArsentsumebitePb2Cu(AsO4)(SO4)(OH)Mon. 2/m : P21/m
8.BG.05'UM1994-19-PO:CuHMoPb'Pb2Cu(PO4)(MoO4,AsO4,CrO4,GaO4)(OH)
8.BG.05FerribushmakinitePb2Fe3+(PO4)(VO4)(OH)Mon. 2/m : P21/m
8.BG.05ArsenbrackebuschitePb2Fe3+(AsO4)2(OH)Mon. 2/m : P2/m
8.BG.05GoedkeniteSr2Al(PO4)2(OH)Mon. 2/m : P21/m
8.BG.05TsumebitePb2Cu(PO4)(SO4)(OH)Mon. 2/m : P21/m
8.BG.05BrackebuschitePb2Mn3+(VO4)2(OH)Mon. 2/m : P21/m
8.BG.05BushmakinitePb2Al(PO4)(VO4)(OH)Mon. 2/m : P21/m
8.BG.05CalderónitePb2Fe3+(VO4)2(OH)Mon. 2/m : P21/m
8.BG.10MélonjosephiteCaFe2+Fe3+(PO4)2(OH)Orth. mmm(2/m2/m2/m) : Pbam
8.BG.15TancoiteLiNa2Al(PO4)(PO3OH)(OH)Orth. mmm(2/m2/m2/m) : Pbca
8.BG.20DmisokoloviteK3Cu5AlO2(AsO4)4Mon. 2/m : B2/b
8.BG.30WrightiteK2Al2O(AsO4)2Orth. mmm(2/m2/m2/m) : Pmma
8.BG.35PolyarsiteNa7CaMgCu2(AsO4)4F2ClMon. 2/m

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 0.0000% 0 α, β, γ
Thorium (Th) 0.0000% 0 α, β, γ
Potassium (K) 7.1923% 2,230 β, γ

For comparison:

  • Banana: ~15 Bq per fruit
  • Granite: 1,000–3,000 Bq/kg
  • EU exemption limit: 10,000 Bq/kg

Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.

Interactive Simulator:

Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!

Activity:

DistanceDose rateRisk
1 cm
10 cm
1 m

The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).

D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield

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 ShchurovskyiteHide

References for ShchurovskyiteHide

Localities for ShchurovskyiteHide

Showing 1 localities.

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.
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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 (TL)
 
  • Kamchatka Krai
    • Milkovsky District
      • Tolbachik Volcanic field
        • Great Fissure eruption (Main Fracture)
          • Northern Breakthrough (North Breach)
            • Second scoria cone
Pekov et al. (2015)
 
and/or  
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