Betpakdalite-NaNa
A valid IMA mineral species
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Formula:
[Na2(H2O)16Na(H2O)6][Mo8As2Fe3+3O33(OH)4]
Colour:
Yellow
Lustre:
Sub-Adamantine, Vitreous
Hardness:
3
Specific Gravity:
2.87
Crystal System:
Monoclinic
Member of:
Name:
First recognized as a potential hypothetical member of the betpakdalite group (IMA 10-E). Later in 2011, approved by IMA as a valid species.
Type Locality:
Dimorph of:
Unique Identifiers
Mindat ID:
41945
Long-form identifier:
mindat:1:1:41945:3
GUID
(UUID V4):
(UUID V4):
6137eeb5-9fee-4df5-abf2-0f032a98d14d
IMA Classification of Betpakdalite-NaNa
Classification of Betpakdalite-NaNa
8.BM.
8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
M : With medium-sized and large cations, (OH, etc.):RO4 = 4:1
8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
M : With medium-sized and large cations, (OH, etc.):RO4 = 4:1
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Bpd-NaNa | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Betpakdalite-NaNa
Sub-Adamantine, Vitreous
Transparency:
Transparent
Colour:
Yellow
Streak:
Colorless to very pale yellow
Hardness:
3 on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
{001}
{001}
Fracture:
Splintery
Density:
2.87(3) g/cm3 (Measured) 2.877 g/cm3 (Calculated)
Optical Data of Betpakdalite-NaNa
Type:
Biaxial (+)
RI values:
nα = 1.765(5) nβ = 1.785(5) nγ = 1.850
2V:
Measured: 60° (5)
Max Birefringence:
δ = 0.085
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
and does not take into account mineral colouration.
Surface Relief:
Very High
Dispersion:
r > v moderate
Pleochroism:
Non-pleochroic
Chemistry of Betpakdalite-NaNa
Mindat Formula:
[Na2(H2O)16Na(H2O)6][Mo8As2Fe3+3O33(OH)4]
Crystallography of Betpakdalite-NaNa
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/m
Setting:
C2/m
Cell Parameters:
a = 19.2370(12) Å, b = 11.0945(7) Å, c = 15.1459(9) Å
β = 130.342(1)°
β = 130.342(1)°
Ratio:
a:b:c = 1.734 : 1 : 1.365
Unit Cell V:
2463.8 ų
Morphology:
Striated prismatic to bladed crystals, flattened on {001} and elongated prallel to [010] (Up to 0.4mm in length and 0.1 mm in diameter). Forms observed: {001}, {110},{10-1} and {20-1}.
Twinning:
Multipel, complex penetrations twins.
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
11.586 Å | (27) |
9.640 Å | (30) |
8.930 Å | (100) |
7.389 Å | (33) |
3.697 Å | (25) |
3.168 Å | (25) |
2.980 Å | (24) |
2.862 Å | (27) |
Geological Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Stage 7: Great Oxidation Event | <2.4 |
47a : [Near-surface hydration of prior minerals] | |
47d : [Arsenates, antimonates, selenates, bismuthinates] |
Type Occurrence of Betpakdalite-NaNa
General Appearance of Type Material:
Matrix: brecciated vein quartz intermixed with, cemented by or coated by jarosite and oxyhydroxides.
Place of Conservation of Type Material:
Natural History Museum of Los Angeles County, Los Angeles, California, USA, catalogue numbers 63570 and 63571
Geological Setting of Type Material:
Upper oxidation zone of the Chiquicamata Mine, Chile, a porphyry copper deposit
Associated Minerals at Type Locality:
Synonyms of Betpakdalite-NaNa
Other Language Names for Betpakdalite-NaNa
German:Betpakdalit-NaNa
Relationship of Betpakdalite-NaNa to other Species
Member of:
Other Members of this group:
Betpakdalite-CaCa | [Ca2(H2O)17Ca(H2O)6][Mo6+8As5+2Fe3+3O36(OH)] | Mon. 2/m : B2/m |
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 |
Related Minerals - Strunz-mindat Grouping
8.BM. | Gunmaite | (Na2Sr)Sr2Al10(PO4)4F14(OH)12 |
8.BM.05 | Retzian-(Ce) | Mn2+2Ce(AsO4)(OH)4 |
8.BM.05 | Retzian-(La) | (Mn2+,Mg)2(La,Ce,Nd)(AsO4)(OH)4 |
8.BM.05 | Retzian-(Nd) | Mn2+2(Nd,Ce,La)(AsO4)(OH)4 |
8.BM.10 | Paulkellerite | (BiO)2Fe3+(PO4)(OH)2 |
8.BM.10 | Kolitschite | PbZn0.5Fe3(AsO4)2(OH)6 |
8.BM.15 | Brendelite | (Bi3+,Pb)2(Fe3+,Fe2+)(PO4)O2(OH) |
Fluorescence of Betpakdalite-NaNa
None
Other Information
Notes:
Slowly soluble in concentrated HCl
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-NaNa
mindat.org URL:
https://www.mindat.org/min-41945.html
Please feel free to link to this page.
Please feel free to link to this page.
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External Links:
Mineral Dealers:
References for Betpakdalite-NaNa
Reference List:
Williams, P. A., Hatert, F., Pasero, M., Mills, S. J. (2011) New minerals and nomenclature modifications approved in 2011. CNMNC Newsletter No 11. Mineralogical Magazine, 75 (6) 2887-2893 doi:10.1180/minmag.2011.075.6.2887
Kampf, A. R., Mills, S. J., Rumsey, M. S., Dini, M., Birch, W. D., Spratt, J., Pluth, J. J., Steele, I. M., Jenkins, R. A., Pinch, W. W. (2012) The heteropolymolybdate family: structural relations, nomenclature scheme and new species. Mineralogical Magazine, 76 (5) 1175-1207 doi:10.1180/minmag.2012.076.5.09
Localities for Betpakdalite-NaNa
Locality List
- 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.
All localities listed without proper references should be considered as questionable.
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