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Stibiocolumbite

A valid IMA mineral species - grandfathered
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About StibiocolumbiteHide

Formula:
Sb(Nb,Ta)O4
Colour:
Dark brown to light yellowish brown; reddish yellow, reddish brown, greenish yellow
Lustre:
Adamantine, Resinous
Hardness:
Specific Gravity:
5.68
Crystal System:
Orthorhombic
Name:
The name reflects its antimony (Greek "stibi") content and similarity to columbite.
This page provides mineralogical data about Stibiocolumbite.


Unique IdentifiersHide

Mindat ID:
3778
Long-form identifier:
mindat:1:1:3778:1

IMA Classification of StibiocolumbiteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
SbNbO4

Classification of StibiocolumbiteHide

4.DE.30

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
D : Metal: Oxygen = 1:2 and similar
E : With medium-sized cations; with various polyhedra
8.1.6.1

8 : MULTIPLE OXIDES CONTAINING NIOBIUM,TANTALUM OR TITANIUM
1 : ABO4
18.1.27

18 : Niobates and Tantalates
1 : Niobates and tantalates containing neither rare earths nor U

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

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

Physical Properties of StibiocolumbiteHide

Adamantine, Resinous
Transparency:
Translucent
Colour:
Dark brown to light yellowish brown; reddish yellow, reddish brown, greenish yellow
Streak:
Light yellow, yellow-brown
Hardness:
5½ on Mohs scale
Tenacity:
Brittle
Cleavage:
Distinct/Good
{010} distinct; {100} indistinct
Fracture:
Sub-Conchoidal
Density:
5.68 g/cm3 (Measured)    5.72 g/cm3 (Calculated)

Optical Data of StibiocolumbiteHide

Type:
Biaxial (+)
RI values:
nα = 2.398 nβ = 2.419 nγ = 2.459
2V:
Measured: 73° , Calculated: 74°
Max. Birefringence:
δ = 0.061
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
Dispersion:
r < v

Chemistry of StibiocolumbiteHide

Mindat Formula:
Sb(Nb,Ta)O4
Element Weights:
Element% weight
Sb43.694 %
Nb33.340 %
O22.966 %

Calculated from ideal end-member formula.
Common Impurities:
Ta

Crystallography of StibiocolumbiteHide

Crystal System:
Orthorhombic
Class (H-M):
mm2 - Pyramidal
Cell Parameters:
a = 4.929 Å, b = 11.797 Å, c = 5.559 Å
Ratio:
a:b:c = 0.418 : 1 : 0.471
Unit Cell V:
323.24 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Prismatic [001]. {010} and {110} striated parallel to [001]. The crystals infreqently exhibit morphological evidence of hemimorphism.
Twinning:
About [010] with composition plane {001}, commonly an irregular junction, or polysynthetic
Comment:
Space Group: P c21n (synthetic SbNbO4).

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.125 Å(100)
2.947 Å(28)
1.735 Å(21)
3.517 Å(18)
1.891 Å(12)
2.779 Å(10)
2.023 Å(10)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 4b: Highly evolved igneous rocks>3.0
34 : Complex granite pegmatites

Type Occurrence of StibiocolumbiteHide

Place of Conservation of Type Material:
The type crystal was totally consumed during analysis before realization it was of a new species.
Associated Minerals at Type Locality:

Synonyms of StibiocolumbiteHide

Other Language Names for StibiocolumbiteHide

Relationship of Stibiocolumbite to other SpeciesHide

Other Members of Cervantite Group:
BismutocolumbiteBi(Nb,Ta)O4Orth. mmm (2/m 2/m 2/m)
BismutotantaliteBiTaO4Orth.
CervantiteSb3+Sb5+O4Orth. mm2
ClinocervantiteSb3+Sb5+O4Mon. 2/m : B2/b
StibiotantaliteSb(Ta,Nb)O4Orth. mm2
Forms a series with:

Related Minerals - Strunz-mindat GroupingHide

4.DE.ColchesteriteBi3+2Mo6+2O9Mon. 2/m
4.DE.PertolditeGeO2Trig. 3 2
4.DE.ZiroiteZrO2Tet. 4/mmm (4/m 2/m 2/m) : P42/nmc
4.DE.05DowneyiteSeO2Tet. 4/mmm (4/m 2/m 2/m) : P42/mbc
4.DE.10Koragoite(Mn2+,Fe3+)3(Nb,Ta,Ti)2(Nb,Mn)2(W,Ta)2O20Mon. 2 : P21
4.DE.15RusselliteBi2WO6Orth. mm2 : Pca21
4.DE.15KoechliniteBi2MoO6Orth. mm2 : Pna21
4.DE.15TungstibiteSb3+2WO6Orth. 2 2 2
4.DE.20TelluriteTeO2Orth. mmm (2/m 2/m 2/m) : Pbca
4.DE.25ParatelluriteTeO2Tet. 4 2 2
4.DE.30BismutotantaliteBiTaO4Orth.
4.DE.30StibiotantaliteSb(Ta,Nb)O4Orth. mm2
4.DE.30CervantiteSb3+Sb5+O4Orth. mm2
4.DE.30BismutocolumbiteBi(Nb,Ta)O4Orth. mmm (2/m 2/m 2/m)
4.DE.30ClinocervantiteSb3+Sb5+O4Mon. 2/m : B2/b
4.DE.35BaddeleyiteZrO2Mon. 2/m : P21/b
4.DE.40BillwiseiteSb3+5Nb3WO18Mon. 2/m : B2/m
4.DE.45KyawthuiteBi3+Sb5+O4Mon. 2/m

Other InformationHide

Electrical:
Strongly pyroelectric.
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 StibiocolumbiteHide

References for StibiocolumbiteHide

Localities for StibiocolumbiteHide

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.

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.
Angola
 
  • Namibe Province
    • Moçâmedes
      • Giraúl pegmatite field
Gonçalves et al. (2019)
Gonçalves et al. (2019)
Canada
 
  • Northwest Territories
    • O'Grady Lake area
      • O'Grady Batholith
Ercit et al. (2003)
Italy
 
  • Lombardy
    • Brescia Province
      • Cevo
        • Upper Val Saviore
          • Monte Foppa (north slope)
            • Forcel Rosso Gully (Forcel Rosso Pass)
Pezzotta +1 other reference
Mozambique
 
  • Zambezia Province
    • Gilé District
      • Muiane-Naipa group
Wilson et al. (2000)
Norway
 
  • Nordland
    • Sørfold
Ellingsen et al. (2000) +1 other reference
Pakistan
 
  • Gilgit-Baltistan
    • Roundu District
      • Haramosh Mountains
Scovill (2007)
imported from Rondu District +1 other reference
Poland
 
  • Lower Silesian Voivodeship
    • Ząbkowice Śląskie County
      • Gmina Ząbkowice Śląskie
        • Szklary
Pieczka (2000) +7 other references
Pieczka et al. (2001)
Russia
 
  • Sverdlovsk Oblast
    • Rezhevsky District
      • Lipovsk pegmatite field
Igor.V. Pekov (2008)
Switzerland
 
  • Valais
    • Visp
      • Embd
Stalder et al. (1998)
Tajikistan
 
  • Gorno-Badakhshan
    • Shughnon
      • Shakhdara Range
Pekov (1998)
USA (TL)
 
  • California
    • San Diego County
      • Mesa Grande Mining District
        • Gem Hill
Fisher (2002)
      • Ramona Mining District
        • Ramona
          • Little Three Mine area
Foord et al. (1989)
  • Colorado
    • Park County
      • Lake George
Eckel et al. (1997)
 
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