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Bahianite

A valid IMA mineral species
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About BahianiteHide

08390740017271921339732.jpg
Flag of Bahia, Brazil
Formula:
Al5Sb3O14(OH)2
Colour:
Tan, cream, orange-brown, brown; crystals colourless, tan, pale violet; yellow internal reflections in transmitted light
Lustre:
Adamantine
Hardness:
9
Specific Gravity:
4.78 - 5.46
Crystal System:
Monoclinic
Name:
The name refers to the State of Bahia, Brazil, from within which state the initial specimens were found.
At the time of approval it was the only known purely aluminium antimonate mineral. Structurally related to simpsonite.

The structure is unique and is based on hcp (hexagonal close packed) arrange of oxygen atoms, the set being parallel to {001}. There are layers consisting of edge-sharing Al5O14(OH)2 sheets, that corner-link to linear trimers of the Sb3O1413- composition.


Unique IdentifiersHide

Mindat ID:
484
Long-form identifier:
mindat:1:1:484:4

Similar NamesHide

BahiaiteA rock subtype

IMA Classification of BahianiteHide

Approved
IMA Formula:
Al5Sb5+3O14(OH)2
Approval year:
1974

Classification of BahianiteHide

4.DC.05

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
D : Metal: Oxygen = 1:2 and similar
C : With medium-sized cations; sheets of edge-sharing octahedra
44.3.7.1

44 : ANTIMONATES
3 : Miscellaneous
7.13.7

7 : Oxides and Hydroxides
13 : Oxides of As, Sb and Bi

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

Physical Properties of BahianiteHide

Adamantine
Transparency:
Transparent, Translucent
Colour:
Tan, cream, orange-brown, brown; crystals colourless, tan, pale violet; yellow internal reflections in transmitted light
Hardness:
Hardness:
VHN100=1605 kg/mm2 - Vickers
Cleavage:
Perfect
on {100}
Fracture:
Irregular/Uneven
Density:
4.78 - 5.46 g/cm3 (Measured)    5.26 g/cm3 (Calculated)

Optical Data of BahianiteHide

Type:
Biaxial (-)
RI values:
nα = 1.81 nβ = 1.87 nγ = 1.92
Max. Birefringence:
δ = 0.110
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.

No measured or calculated 2V is on file for this mineral, so the value used here (82°) is estimated from its recorded refractive indices and optic sign, not from a direct 2V measurement.
Dispersion:
r > v
Pleochroism:
Weak

Chemistry of BahianiteHide

Mindat Formula:
Al5Sb3O14(OH)2
Element Weights:
Element% weight
Sb48.178 %
O33.763 %
Al17.793 %
H0.266 %

Calculated from ideal end-member formula.

Crystallography of BahianiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/m
Setting:
C2/m
Cell Parameters:
a = 9.406 Å, b = 11.541 Å, c = 4.41 Å
β = 90.94°
Ratio:
a:b:c = 0.815 : 1 : 0.382
Unit Cell V:
478.66 ų (Calculated from Unit Cell)
Z:
2
Morphology:
Curved and striated crystals, diamond-shaped or rectangular
Twinning:
Pseudohexagonal multiple contact twins, chrysoberyl-like

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0014703BahianiteMoore P B, Araki T (1976) Bahianite, Al5Sb3O14(O,OH)2, a novel hexagonal close-packed oxide structure Neues Jahrbuch fur Mineralogie, Abhandlungen 126 113-1251976Serra de Mangabeira, Bahia, Brazil0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.241 Å(100)
3.194 Å(100)
2.156 Å(80)
4.712 Å(70)
2.457 Å(70)
2.411 Å(70)
1.648 Å(70)
Comments:
Recorded on type material

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
26 : Hadean detrital minerals
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47d : [Arsenates, antimonates, selenates, bismuthinates]

Type Occurrence of BahianiteHide

General Appearance of Type Material:
Water-worn, bean-shaped pebbles, to 10 cm, with polycrystalline or radial-fibrous structure; also as crystals, lining pockets in the pebbles
Place of Conservation of Type Material:
Harvard University, Cambridge, Massachusetts, USA (No. 119088);
National Museum of Natural History, Washington, D.C., USA (Nos. 133875, 135922)
Geological Setting of Type Material:
In potholes as stream-worn pebbles and as residual concentrates above weathered volcanic rock
Associated Minerals at Type Locality:

Synonyms of BahianiteHide

Other Language Names for BahianiteHide

Dutch:Bahianiet
German:Bahianit
Spanish:Bahianita

Common AssociatesHide

Associations Based on Photo Data:
2 photos of Bahianite associated with QuartzSiO2
2 photos of Bahianite associated with MuscoviteKAl2(AlSi3O10)(OH)2

Related Minerals - Strunz-mindat GroupingHide

4.DC.10SimpsoniteAl4Ta3O13(OH)Trig. 3 : P3

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 BahianiteHide

References for BahianiteHide

Localities for BahianiteHide

Showing 3 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.
Brazil
 
  • Bahia
    • Érico Cardoso
      • Paramirim das Crioulas
Cassedanne et al. (1980)
Anthony (1997)
    • Ibitiara
Cassedanne (1985)
 
and/or  
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