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Braithwaiteite

A valid IMA mineral species
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About BraithwaiteiteHide

06269640017271949587253.jpg
R. S. W. Braithwaite
Formula:
NaCu5(Ti4+Sb5+)(AsO4)4(HAsO4)2O2 · 8H2O
Ti and Sb disordered on same crystal site: ratio is 0.87:1.13 in type material.
Colour:
Blue
Lustre:
Vitreous
Hardness:
2
Specific Gravity:
3.442
Crystal System:
Triclinic
Name:
Named in 2009 by Werner H. Paar, Mark A. Cooper, Frank C. Hawthorne, Elizabeth Moffatt, Mickey E. Gunter, Andrew C. Roberts, and Pete J. Dunn in honour of Richard S. W. Braithwaite [1930-], a British mineral spectroscopist and professor at the University of Manchester, United Kingdom.
New structure type.


Unique IdentifiersHide

Mindat ID:
31499
Long-form identifier:
mindat:1:1:31499:0

IMA Classification of BraithwaiteiteHide

Approved
IMA Formula:
NaCu2+5(Ti4+Sb5+)O2(As5+O4)4[As5+O3(OH)]2·8H2O
Approval year:
2006
First published:
2009

Classification of BraithwaiteiteHide

8.DB.75

8 : PHOSPHATES, ARSENATES, VANADATES
D : Phosphates, etc. with additional anions, with H2O
B : With only medium-sized cations, (OH, etc.):RO4< 1:1
39.3.16.

39 : HYDRATED ACID PHOSPHATES,ARSENATES AND VANADATES
3 : Miscellaneous

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

Pronunciation of BraithwaiteiteHide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Physical Properties of BraithwaiteiteHide

Vitreous
Transparency:
Transparent
Colour:
Blue
Streak:
Very pale blue
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
{001}
Fracture:
Irregular/Uneven
Density:
3.442 g/cm3 (Measured)    3.753 g/cm3 (Calculated)

Optical Data of BraithwaiteiteHide

Type:
Biaxial (-)
RI values:
nα = 1.6982 nβ = 1.7575 nγ = 1.7835
2V:
Measured: 59° , Calculated: 65°
Birefringence:
0.085
Max. Birefringence:
δ = 0.085
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.
Optical Extinction:
X ∧ a = 20.5°, X ∧ b = 109.2°, X ∧ c = 110.8°.
Y ∧ a = 69.5°, Y ∧ b = 42.3°, Y ∧ c = 79.9°.
Z ∧ a = 88.4°, Z ∧ b = 125.9°, Z ∧ c = 23.4°.
Pleochroism:
Visible
Comments:
X = Y = pale blue, Z = greenish blue.
Comments:
Absorption: X = Y < Z.

Chemistry of BraithwaiteiteHide

Mindat Formula:
NaCu5(Ti4+Sb5+)(AsO4)4(HAsO4)2O2 · 8H2O

Ti and Sb disordered on same crystal site: ratio is 0.87:1.13 in type material.
Element Weights:
Element% weight
O35.741 %
As29.536 %
Cu20.876 %
Sb8.000 %
Ti3.145 %
Na1.511 %
H1.192 %

Calculated from ideal end-member formula.
O
As
Cu
Sb
Ti
Na
H

Crystallography of BraithwaiteiteHide

Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Setting:
P1
Cell Parameters:
a = 7.0308 Å, b = 9.8823 Å, c = 10.6754 Å
α = 106.973°, β = 104.274°, γ = 93.839°
Ratio:
a:b:c = 0.711 : 1 : 1.08
Unit Cell V:
679.76 ų (Calculated from Unit Cell)
Z:
1
Morphology:
Lath-like. Forms include {100}, {103}, {001}, {203}.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0013021BraithwaiteiteHawthorne F C, Cooper M A, Paar W H (2008) The crystal structure of braithwaiteite Journal of Coordination Chemistry 61 15-292008Black Vein, Laurani, Bolivia0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
9.825 Å(100)
9.334 Å(10)
5.887 Å(50)
5.454 Å(15)
5.075 Å(20)
4.635 Å(30)
4.109 Å(20)
3.674 Å(25)
3.601 Å(3)
3.503 Å(20)
3.354 Å(30)
3.232 Å(30)
3.195 Å(5)
3.105 Å(20)
3.020 Å(5)
2.947 Å(60)
2.858 Å(10)
2.812 Å(3)
2.736 Å(30
2.633 Å(3)
2.589 Å(5)
2.548 Å(5)
2.524 Å(10)
2.442 Å(30b)

Geological EnvironmentHide

Paragenetic Mode(s):

Type Occurrence of BraithwaiteiteHide

General Appearance of Type Material:
Small dark sky-blue bladed crystals or masses.
Place of Conservation of Type Material:
Canadian Museum of Nature, Ottawa, Ontario, Canada, number CMNMC 86085.
Geological Setting of Type Material:
Oxidized portion of an epithermal vein deposit.
Associated Minerals at Type Locality:

Synonyms of BraithwaiteiteHide

Other Language Names for BraithwaiteiteHide

Related Minerals - Strunz-mindat GroupingHide

8.DB.ArangasiteAl2F(PO4)(SO4) · 9H2O Mon. 2/m : P2/b
8.DB.HösliteFe3+3(VO4)2(SO4)(OH)(H2O)4 · 3H2OMon. 2/m : P21/c
8.DB.AgujaiteNa6Al6(H2O)15(OH)3(AsO4)5(AsO3OH)3 · 3H2OTrig. 3m : P3c1
8.DB.Camaronesite[Fe3+(H2O)2(PO3OH)]2(SO4) · 1-2H2OTrig. 32 : R32
8.DB.05DestineziteFe3+2(PO4)(SO4)(OH) · 6H2OTric. 1 : P1
8.DB.05Pitticite(Fe, AsO4, H2O) (?)Amor.
8.DB.05DiadochiteFe3+2(PO4)(SO4)(OH) · 6H2OAmor.
8.DB.07WilhelmgümbeliteZnFe2+Fe3+3(PO4)3(OH)4(H2O)5 · 2H2OOrth. mmm(2/m2/m2/m)
8.DB.07Schmidite[Zn2(Fe3+,Mn2+)2Fe3+(PO4)3(OH)3(H2O)6] · 2H2OOrth.
8.DB.07WildenaueriteZn(Fe3+,Mn2+)2MnFe3+(PO4)3(OH)3(H2O)6 · 2H2OOrth. mmm(2/m2/m2/m) : Pbam
8.DB.10VashegyiteAl11(PO4)9(OH)6 · 38H2OOrth. mmm(2/m2/m2/m)
8.DB.15SchooneriteZnMn2+Fe2+2Fe3+(PO4)3(OH)2 · 9H2OOrth. mmm(2/m2/m2/m) : Pbam
8.DB.20SinkankasiteMn2+Al(PO3OH)2(OH) · 6H2OTric. 1 : P1
8.DB.25MitryaevaiteAl6(PO4)((P,S)O3(OH,O))2F2(OH)2 · 14.5H2OTric. 1 : P1
8.DB.30SanjuaniteAl2(PO4)(SO4)(OH) · 9H2OTric.
8.DB.35SarmientiteFe3+2(AsO4)(SO4)(OH) · 5H2OMon. 2/m : P21/c
8.DB.40BukovskýiteFe3+2(AsO4)(SO4)(OH) · 9H2OTric. 1 : P1
8.DB.40ManganflurliteZnMn2+3Fe3+(PO4)3(OH)2(H2O)7 · 2H2OMon. 2/m : P21/m
8.DB.40FlurliteZn3Mn2+Fe3+(PO4)3(OH)2 · 9H2OMon. 2/m : P21/m
8.DB.42BohuslaviteFe3+4(PO4)3(SO4)(OH) · nH2OTric. 1 : P1
8.DB.45ZýkaiteFe3+4(AsO4)3(SO4)(OH) · 15H2OOrth. 222 : P222
8.DB.47LapeyreiteCu3O[AsO3(OH)]2 · 0.75H2OMon. 2/m : B2/m
8.DB.50RossiantoniteAl3(PO4)(SO4)2(OH)2(H2O)14Tric. 1 : P1
8.DB.50GiniiteFe2+Fe3+4(PO4)3(OH)5 · 2H2OMon. 2/m : P2/b
8.DB.52'Arctowskite'Al9(PO4)8(OH)3 · 27H2OOrth.
8.DB.55Sasaite(Al,Fe3+)14(PO4)11(SO4)(OH)7 · 83H2OOrth.
8.DB.60McauslaniteFe3Al2(PO4)3(PO3OH)F · 18H2OTric.
8.DB.65GoldquarryiteCuCd2Al3(PO4)4F2(H2O,F)2 · 10H2OTric. 1 : P1
8.DB.70BirchiteCd2Cu2(PO4)2(SO4) · 5H2OOrth. mmm(2/m2/m2/m) : Pnma

Fluorescence of BraithwaiteiteHide

Not fluorescent in UV.

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 BraithwaiteiteHide

References for BraithwaiteiteHide

Localities for BraithwaiteiteHide

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.
Bolivia (TL)
 
  • La Paz
    • Aroma Province
      • Sica Sica Municipality
Canadian Mineralogist 47 (2009)
 
and/or  
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