Stibiocolumbite
A valid IMA mineral species - grandfathered
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About Stibiocolumbite
Formula:
Sb(Nb,Ta)O4
Colour:
Dark brown to light yellowish brown; reddish yellow, reddish brown, greenish yellow
Lustre:
Adamantine, Resinous
Hardness:
5½
Specific Gravity:
5.68
Crystal System:
Orthorhombic
Member of:
Name:
The name reflects its antimony (Greek "stibi") content and similarity to columbite.
This page provides mineralogical data about Stibiocolumbite.
Unique Identifiers
Mindat ID:
3778
Long-form identifier:
mindat:1:1:3778:1
GUID
(UUID V4):
(UUID V4):
92cf3e92-eea1-4b28-8cbe-d3d078bd2508
Classification of Stibiocolumbite
Approved, 'Grandfathered' (first described prior to 1959)
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
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
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
18 : Niobates and Tantalates
1 : Niobates and tantalates containing neither rare earths nor U
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 |
---|---|---|
Sclb | 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 Stibiocolumbite
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
{010} distinct; {100} indistinct
Fracture:
Sub-Conchoidal
Density:
5.68 g/cm3 (Measured) 5.72 g/cm3 (Calculated)
Optical Data of Stibiocolumbite
Type:
Biaxial (+)
RI values:
nα = 2.398 nβ = 2.419 nγ = 2.459
2V:
Measured: 73° , Calculated: 74°
Max Birefringence:
δ = 0.061
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
Chemical Properties of Stibiocolumbite
Formula:
Sb(Nb,Ta)O4
IMA Formula:
SbNbO4
Elements listed:
Common Impurities:
Ta
Crystallography of Stibiocolumbite
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 Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
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 Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Stage 4b: Highly evolved igneous rocks | >3.0 |
34 : Complex granite pegmatites |
Type Occurrence of Stibiocolumbite
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:
Reference:
Penfield, S.L., Ford, W.E. (1906) On stibiotantalite. American Journal of Science, 4th. series: 22: 61-77.
Synonyms of Stibiocolumbite
Columbite-Tantalite (in part)
Other Language Names for Stibiocolumbite
Relationship of Stibiocolumbite to other Species
Member of:
Other Members of this group:
Bismutocolumbite | Bi(Nb,Ta)O4 | Orth. mmm (2/m 2/m 2/m) |
Bismutotantalite | Bi(Ta,Nb)O4 | Orth. |
Cervantite | Sb3+Sb5+O4 | Orth. mm2 |
Clinocervantite | Sb3+Sb5+O4 | Mon. 2/m : B2/b |
Stibiotantalite | Sb(Ta,Nb)O4 | Orth. mm2 |
Forms a series with:
Related Minerals - Strunz-mindat Grouping
4.DE. | Ziroite | ZrO2 | Tet. 4/mmm (4/m 2/m 2/m) : P42/nmc |
4.DE. | Pertoldite | GeO2 | Trig. 3 2 |
4.DE.05 | Downeyite | SeO2 | Tet. 4/mmm (4/m 2/m 2/m) : P42/mbc |
4.DE.10 | Koragoite | (Mn2+,Fe3+)3(Nb,Ta,Ti)2(Nb,Mn)2(W,Ta)2O20 | Mon. 2 : P21 |
4.DE.15 | Koechlinite | Bi2MoO6 | Orth. mm2 : Pna21 |
4.DE.15 | Russellite | Bi2WO6 | Orth. mm2 : Pca21 |
4.DE.15 | Tungstibite | Sb3+2WO6 | Orth. 2 2 2 |
4.DE.20 | Tellurite | TeO2 | Orth. mmm (2/m 2/m 2/m) : Pbca |
4.DE.25 | Paratellurite | TeO2 | Tet. 4 2 2 |
4.DE.30 | Bismutotantalite | Bi(Ta,Nb)O4 | Orth. |
4.DE.30 | Bismutocolumbite | Bi(Nb,Ta)O4 | Orth. mmm (2/m 2/m 2/m) |
4.DE.30 | Cervantite | Sb3+Sb5+O4 | Orth. mm2 |
4.DE.30 | Stibiotantalite | Sb(Ta,Nb)O4 | Orth. mm2 |
4.DE.30 | Clinocervantite | Sb3+Sb5+O4 | Mon. 2/m : B2/b |
4.DE.35 | Baddeleyite | ZrO2 | Mon. 2/m : P21/b |
4.DE.40 | Billwiseite | Sb3+5Nb3WO18 | Mon. 2/m : B2/m |
4.DE.45 | Kyawthuite | Bi3+Sb5+O4 | Mon. 2/m |
Other Information
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.
References for Stibiocolumbite
Reference List:
Sort by Year (asc) | by Year (desc) | by Author (A-Z) | by Author (Z-A)
Penfield, S.L., Ford, W.E. (1906) On stibiotantalite. American Journal of Science, 4th. series: 22: 61-77.
Schaller (1915) private contr. in Dana: 74.
Palache, Charles, Harry Berman & Clifford Frondel (1944) The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana Yale University 1837-1892, Volume I: Elements, Sulfides, Sulfosalts, Oxides. John Wiley and Sons, Inc., New York. 7th edition, revised and enlarged: 767-769.
Roth, R.S., Waring,J.L. (1963) Synthesis and stability of bismutotantalite, stibiotantalite and chemically similar ABO4 compounds. American Mineralogist: 48: 1348-1356.
Foord, E.E. (1981) Bismuthian stibiocolumbite-tantalite and other minerals from the Little Three mine, Ramona, California: Mineral Society of America – Friends of Mineralogy, symposium abstracts.
Konovalenko, S.I., Voloshin, A.V., Pakhomovskii, Y.A., Rossovskii, L.N., Anan’yev, A.N. (1982) Tungsten varieties of tantaloniobates in granitic miarolitic pegmatites of southwestern Pamirs. Mineralogicheskii Zhurnal, Kiev: 4(1): 65–74 (70).
Zubkova, N.V., Puscharovsky, D.Yu., Giester, G., Smolin, A.S., Tillmanns, E., Brandstätter, F., Hammer, V., Peretyazhko, I.S., Sapozhnikov, A.N., and Kashaev, A.A. (2002) Bismutocolumbite, Bi(Nb0.79Ta0.21)O4, stibiocolumbite, Sb(Nb0.67Ta0.33)O4, and their structural relation to the other ABO4 minerals with stibiotantalite (SbTaO4) structure. Neues Jahrbuch für Mineralogie, Monatshefte 2002: 145-159.
Internet Links for Stibiocolumbite
mindat.org URL:
https://www.mindat.org/min-3778.html
Please feel free to link to this page.
Please feel free to link to this page.
External Links:
Mineral Dealers:
Localities for Stibiocolumbite
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.
Angola | |
| Gonçalves, A. O., Melgarejo, J. C., Alfonso, P., Amores, S., Paniagua, A., Neto, A. B., ... & Camprubí, A. (2019). The Distribution of Rare Metals in the LCT Pegmatites from the Giraúl Field, Angola. Minerals, 9(10), 580. |
Gonçalves, A. O., Melgarejo, J. C., Alfonso, P., Amores, S., Paniagua, A., Neto, A. B., ... & Camprubí, A. (2019). The Distribution of Rare Metals in the LCT Pegmatites from the Giraúl Field, Angola. Minerals, 9(10), 580. | |
Canada | |
| Ercit, T.S., Groat, L.A. & Gault, R.A, (2003): Granitic pegmatites of the O'Grady batholith, N.W.T., Canada: a case study of the evolution of elbaite subtype of rare-element granitic pegmatite. The Canadian Mineralogist, 41, 117-137. |
Italy | |
| Pezzotta, Federico and Guastoni, Alessandro, The New Discovery of a LCT Pegmatite in the Adamello Massif, Central Southern Alps, Italy; Museo Civico di Storia Naturale, Milan, Italy. |
Mozambique | |
| Dias, M. Bettencourt and Wilson, W.E. (2000): Famous mineral localities: The Alto Ligonha pegmatites (Mozambique). Mineralogical Record, 31, 459-497 |
Norway | |
| Husdal, T. (2008): The minerals of the pegmatites within the Tysfjord granite, northern Norway. Norsk Bergverksmuseum, skrift 38, 5-28. |
Pakistan | |
| Scovill, J. (2007): Lapis 32 (4), 40-42. |
imported from Rondu District; Transferred from OLD Skardu District | |
Poland | |
| Geologia Sudetica, 33 (1): 23-31. ; Pieczka, A.; Grew, E.S.; Groat, L.A.; Evans, R.J. (2011): Holtite and dumortierite from the Szklary Pegmatite, Lower Silesia, Poland. Mineralogical Magazine 75, 303-315.; Pieczka, A., Evans, R. J., Grew, E. S., Groat, L. A., Ma, C., & Rossman, G. R. (2013). The dumortierite supergroup. II. Three new minerals from the Szklary pegmatite, SW Poland: Nioboholtite,(Nb0. 6⃞0. 4) Al6BSi3O18, titanoholtite,(Ti0. 75⃞0. 25) Al6BSi3O18, and szklaryite, ⃞Al6BAs33+ O15. Mineralogical Magazine, 77(6), 2841-2856.; Pieczka, A., Biagioni, C., Gołębiowska, B., Jeleń, P., Pasero, M., & Sitarz, M. (2018). Parafiniukite, Ca2Mn3 (PO4) 3Cl, a New Member of the Apatite Supergroup from the Szklary Pegmatite, Lower Silesia, Poland: Description and Crystal Structure. Minerals, 8(11), 485. Szuszkiewicz, Adam, Adam Pieczka, Bożena Gołębiowska, Magdalena Dumańska-Słowik, Mariola Marszałek, and Eligiusz Szełęg. (2018) "Chemical Composition of Mn- and Cl-Rich Apatites from the Szklary Pegmatite, Central Sudetes, SW Poland: Taxonomic and Genetic Implications" Minerals 8, no. 8: 350. https://doi.org/10.3390/min8080350 |
Pieczka, A., & Gołębiowska, B. (2001). Altered pyrochlore from the Szklary rare-element pegmatite, Lower Silesia, Poland. In Mineral Deposits at the Beginning of the 21 st Century. Proceedings of the Joint sixth Biennial SGA-SEG Meeting (pp. 469-472). | |
Russia | |
| Igor.V. Pekov, Lyudmila R. Memetova (2008) Minerals of the Lipovka Granite Pegmatites, Central Urals, Russia. Mineralogical Almanac 13:6-45 |
Switzerland | |
| Stalder, H. A., Wagner, A., Graeser, S. and Stuker, P. (1998): "Mineralienlexikon der Schweiz", Wepf (Basel), p. 387. |
Tajikistan | |
| Pekov, I. (1998) Minerals First discovered on the territory of the former Soviet Union 369p. Ocean Pictures, Moscow |
USA (TL) | |
| Fisher, J. 2002. Gem and rare-element pegmatites of southern California. Mineralogical Record, Volume 33, Number 5: pages 390-396, photographs. |
| Foord, Eugene E., Spaulding, Louis B. Jr., Martin, Robert F. & Mason, Roger A. (1989), Mineralogy and Paragenesis of the Little Three Mine Pegmatites, Ramona District, San Diego County, California. Mineralogical Record, 20(2): p. 123. |
| Minerals of Colorado (1997) E.B. Eckel |
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Quartzite quarries, Embd, Visp, Valais, Switzerland