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Betpakdalite-CaCa

A valid IMA mineral species
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About Betpakdalite-CaCaHide

01482950017271921561473.jpg
Betpak-Dala desert, Kazakhstan
Formula:
[Ca2(H2O)17Ca(H2O)6][Mo6+8As5+2Fe3+3O36(OH)]
Colour:
Lemon-yellow with greenish tint
Lustre:
Dull
Hardness:
3
Specific Gravity:
2.98 - 3.05
Crystal System:
Monoclinic
Name:
Named betpakdalite by L.P. Ermilova and V.M. Senderova in 1961 after the Betpakdala (Bet-Pak-Dal) Desert, Kazakhstan that includes the type locality.

It was redefined in 2010 (IMA 10-E) and renamed betpakdalite-CaCa.
This page provides mineralogical data about Betpakdalite-CaCa.


Unique IdentifiersHide

Mindat ID:
651
Long-form identifier:
mindat:1:1:651:4

Similar NamesHide

Betpakdalite-NaCaA valid IMA mineral species[Na2(H2O)17Ca(H2O)6][Mo86+As25+Fe33+O34(OH)3]

IMA Classification of Betpakdalite-CaCaHide

Approved
IMA status notes:
Renamed by the IMA
First published:
1961
Approval history:
Renamed by IMA: 2010

Classification of Betpakdalite-CaCaHide

8.DM.15

8 : PHOSPHATES, ARSENATES, VANADATES
D : Phosphates, etc. with additional anions, with H2O
M : With large and medium-sized cations, (OH, etc.):RO4 > 2:1
49.4.1.1

49 : HYDRATED MOLYBDATES AND TUNGSTATES
4 : Compound Molybdates and Tungstates
22.5.8

22 : Phosphates, Arsenates or Vanadates with other Anions
5 : Phosphates, arsenates or vanadates with chromate, molybdate, niobate or tantalate

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

Physical Properties of Betpakdalite-CaCaHide

Transparency:
Transparent
Colour:
Lemon-yellow with greenish tint
Hardness:
Cleavage:
Very Good
{001}
Density:
2.98 - 3.05 g/cm3 (Measured)    2.913 g/cm3 (Calculated)

Optical Data of Betpakdalite-CaCaHide

Type:
Biaxial (+)
RI values:
nα = 1.782 - 1.809 nβ = 1.797 - 1.821 nγ = 1.850 - 1.857
2V:
Measured: 60° , Calculated: 53° to 88°
Max. Birefringence:
δ = 0.048 - 0.068
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. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
extreme, inclined
Optical Extinction:
Y = b; X ∧ c = 12°.
Pleochroism:
Visible
Comments:
X = pale yellow, Y = greenish yellow, Z= bluish.
Comments:
Absorption: Z > Y > X.

Chemistry of Betpakdalite-CaCaHide

Mindat Formula:
[Ca2(H2O)17Ca(H2O)6][Mo6+8As5+2Fe3+3O36(OH)]
Element Weights:
Element% weight
O43.386 %
Mo34.695 %
Fe7.572 %
As6.772 %
Ca5.434 %
H2.141 %

Calculated from ideal end-member formula.
O
Mo
Fe
As
Ca
H

Crystallography of Betpakdalite-CaCaHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/m
Setting:
C2/m
Cell Parameters:
a = 19.507(2) Å, b = 11.0768(9) Å, c = 15.2618(19) Å
β = 131.2618(5)°
Ratio:
a:b:c = 1.761 : 1 : 1.378
Unit Cell V:
2470.3 ų
Comment:
Cell parameters from SCXRD (Kampf et al 2012)

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0014792Betpakdalite-CaCaSchmetzer K, Nuber B, Tremmel G (1984) Betpakdalite from Tsumeb, Namibia: mineralogy, crystal chemistry and structure Neues Jahrbuch fur Mineralogie, Monatshefte 1984 393-4031984Tsumeb, Namibia0293
0005591Betpakdalite-CaCaCooper M A, Hawthorne F C (1999) The crystal structure of betpakdalite, and a new chemical formula: {Mg(H2O)6}Ca2(H2O)13[Mo8As2Fe3O36(OH)](H2O)4 The Canadian Mineralogist 37 61-6619990293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
8.75 Å(100)
3.63 Å(90)
1.532 Å(80)
1.480 Å(80)
2.95 Å(70)
1.723 Å(70)
1.191 Å(70)
1.024 Å(70)
Comments:
Kara-Oba deposit, Kazakhstan. Data from Ermilova and Senderova (1961).

Geological EnvironmentHide

Paragenetic Mode(s):

Type Occurrence of Betpakdalite-CaCaHide

General Appearance of Type Material:
Powdery finely-crystalline aggregates, individual crystals being 0.005 to 0.025 mm.
Place of Conservation of Type Material:
No designated type material.
Geological Setting of Type Material:
Oxidation zone of a wolframite deposit, that consists of early quartz-wolframite-veins and later quartz-huebnerite-pyrite-arsenopyrite veins.
Associated Minerals at Type Locality:

Other Language Names for Betpakdalite-CaCaHide

Relationship of Betpakdalite-CaCa to other SpeciesHide

Other Members of Betpakdalite Group:
Betpakdalite-CaMg[Ca2(H2O)17Mg(H2O)6][Mo8As2Fe3+3O36(OH)] Mon. 2/m : B2/m
Betpakdalite-FeFe[Fe3+2 (H2O)15(OH)2Fe3+(H2O)6][Mo8As2Fe3+3O37]Mon. 2/m : B2/m
Betpakdalite-NaCa[Na2(H2O)17Ca(H2O)6][Mo6+8As5+2Fe3+3O34(OH)3]Mon. 2/m : B2/m
Betpakdalite-NaNa[Na2(H2O)16Na(H2O)6][Mo8As2Fe3+3O33(OH)4] Mon. 2/m : B2/m

Common AssociatesHide

Associations Based on Photo Data:
9 photos of Betpakdalite-CaCa associated with ScoroditeFe3+AsO4 · 2H2O
6 photos of Betpakdalite-CaCa associated with MolybdeniteMoS2
3 photos of Betpakdalite-CaCa associated with FerrimolybditeFe2(MoO4)3 · nH2O
2 photos of Betpakdalite-CaCa associated with ZeuneriteCu(UO2)2(AsO4)2 · 12H2O
2 photos of Betpakdalite-CaCa associated with ChistyakovaiteAl(UO2)2(AsO4)2(F,OH) · 6.5H2O
1 photo of Betpakdalite-CaCa associated with QuartzSiO2
1 photo of Betpakdalite-CaCa associated with CalciteCaCO3
1 photo of Betpakdalite-CaCa associated with PharmacosideriteKFe3+4(AsO4)3(OH)4 · 6-7H2O
1 photo of Betpakdalite-CaCa associated with PowelliteCa(MoO4)
1 photo of Betpakdalite-CaCa associated with AnglesitePbSO4

Related Minerals - Strunz-mindat GroupingHide

8.DM.TomsquarryiteNaMgAl3(PO4)2(OH)6 · 8H2OTrig. 3m(32/m) : R3m
8.DM.ElliottiteNaMgAl3(PO4)2F6 · 9H2OMon. 2/m : B2/m
8.DM.Betpakdalite-FeFe[Fe3+2 (H2O)15(OH)2Fe3+(H2O)6][Mo8As2Fe3+3O37]Mon. 2/m : B2/m
8.DM.Penriceite[Mg(H2O)6][Na(H2O)2Al3(PO4)2F6] · H2OMon. 2/m : P21/b
8.DM.Betpakdalite-CaMg[Ca2(H2O)17Mg(H2O)6][Mo8As2Fe3+3O36(OH)] Mon. 2/m : B2/m
8.DM.Chinnerite[Mg(H2O)6]Na(H2O)2Al3(PO4)2F6Mon. 2/m : P2/m
8.DM.Sarrochite[Ca4(H2O)38][Mo8P2Fe3+3O37(OH)]Trig. 3m(32/m) : P3m1
8.DM.05EsperanzaiteNaCa2Al2(AsO4)2(OH)F4 · 2H2OMon. 2/m : P21/m
8.DM.05MoriniteNaCa2Al2(PO4)2(OH)F4 · 2H2OMon. 2/m : P21/m
8.DM.10AlexshubnikoviteCa2Cu9(AsO4)4(OH)9Cl(H2O)8 · 2H2OMon. 2/m : P2/b
8.DM.10TangdaniteCa2Cu9(AsO4)4(SO4)0.5(OH)9 · 9H2OMon. 2/m : B2/b
8.DM.10TyroliteCa2Cu9(AsO4)4(CO3)(OH)8 · 11H2OMon. 2/m
8.DM.15Melkovite[Ca2(H2O)15Ca(H2O)6][Mo8P2Fe3+3O36(OH)]Mon. 2/m : B2/m
8.DM.15Betpakdalite-NaCa[Na2(H2O)17Ca(H2O)6][Mo6+8As5+2Fe3+3O34(OH)3]Mon. 2/m : B2/m
8.DM.20Phosphovanadylite-BaBa[V4+4P2O8(OH)8] · 12H2OIso. 43m : I43m
8.DM.20Phosphovanadylite-CaCa[V4+4P2O12(OH)4] · 12H2O Iso. 43m : I43m
8.DM.25YukoniteCa3Fe3+(AsO4)2(OH)3 · 5H2OOrth. mm2
8.DM.30UdumineliteCa3Al8(PO4)2O12 · 2H2O
8.DM.35Aldermanite[Mg(H2O)6][Na(H2O)2Al3(PO4)2(OH,F)6] · H2O Mon. 2/m : P21/b
8.DM.35'Azovskite'Fe3+3(PO4)(OH)6 or near
8.DM.35DelvauxiteCaFe4(PO4,SO4)2(OH)8 · 4-6H2O not confirmedAmor.
8.DM.40Santafeite(Na,Ca,Sr)12(Mn2+,Fe3+,Al,Mg)8Mn4+8(VO4)16(OH,O)20 · 8H2OOrth. mmm(2/m2/m2/m)
8.DM.55TapiaiteCa5Al2(AsO4)4(OH)4 · 12H2OMon.
8.DM.60Alcantarillaite[Fe3+0.5(H2O)4][CaAs3+2(Fe3+2.5W6+0.5)(AsO4)2O7]Orth. mmm(2/m2/m2/m) : Imma

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 Betpakdalite-CaCaHide

References for Betpakdalite-CaCaHide

Reference List:

Localities for Betpakdalite-CaCaHide

Showing 20 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.
Australia
 
  • New South Wales
    • Gough Co.
      • Elsmore
Williams et al. (2005)
Chile
 
  • Atacama
    • Copiapó Province
      • Tierra Amarilla
        • Pampa Larga mining district
analysed with Edx (by dr. Jochen Schlüter) +1 other reference
China
 
  • Hebei
    • Zhangjiakou
      • Guyuan County
Dahlkamp (2009)
Czech Republic
 
  • Karlovy Vary Region
    • Sokolov District
      • Krásno
Sejkora et al. (2006)
  • Ústí nad Labem Region
    • Teplice District
      • Krupka
        • Knöttel area
Sejkora (1998)
France
 
  • Nouvelle-Aquitaine
    • Haute-Vienne
      • Bellac
        • Vaulry
Robinson et al. (1992)
          • Vaulry Mines
Queneau (n.d.) +1 other reference
Germany
 
  • Saxony
    • Sächsische Schweiz-Osterzgebirge
      • Dippoldiswalde
Witzke (2023)
Greece
 
  • Attica
    • East Attica
      • Lavreotiki
Rieck et al. (2020)
        • Plaka
          • Plaka mines
Rieck et al. (2020)
Italy
 
  • Lombardy
    • Varese Province
      • Cuasso al Monte
        • Cuasso al Piano
Gentile et al. (2023)
  • Tuscany
    • Livorno Province
      • Livorno
        • Valle Benedetta
Marco Bonifazi collection
Japan
 
  • Hiroshima Prefecture
    • Ikuchi Island
The Mineral Species of Japan (5th ed)
Kazakhstan (TL)
 
  • Jambyl Region
    • Moiynkum District
Ermilova et al. (1961) +1 other reference
  • Jetisu Region
    • Alakol District
Pavel M. Kartashov (n.d.)
Mongolia
 
  • Khentii Province
    • Tsenkhermandal District
Kampf et al. (2012)
Namibia
 
  • Oshikoto Region
    • Tsumeb
Schmetzer
Norway
 
  • Nordland
    • Hamarøy
      • Drag
Husdal (2011) +1 other reference
Russia
 
  • Zabaykalsky Krai
    • Nerchinsky District
      • Adun-Cholon Range
Kasatkin et al. (2014)
USA
 
  • Utah
    • Tooele County
      • Gold Hill Mining District (Clifton Mining District)
Kampf et al. (2012)
 
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