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Tancoite

A valid IMA mineral species
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About TancoiteHide

Formula:
LiNa2Al(PO4)(PO3OH)(OH)
Colour:
Colorless to light pink
Lustre:
Vitreous, Sub-Vitreous
Hardness:
4 - 4½
Specific Gravity:
2.752
Crystal System:
Orthorhombic
Name:
Named in 1980 by Robert A. Ramik, Bozidar Darko Sturman, Pete J. Dunn, and Alexander Sergevich Povarennykh for its discovery locality, the Tanco Mine (pegmatite), Bernic Lake, Manitoba, Canada.
Colorless to pale pink tabular crystals


Unique IdentifiersHide

Mindat ID:
3879
Long-form identifier:
mindat:1:1:3879:5

Similar NamesHide

Tancaite-(Ce)A valid IMA mineral speciesFeCe(MoO4)3 · 3H2O
TanguéiteA synonym of Tangeite
Tankite (of Haidinger)A synonym of Xenotime-(Y)

IMA Classification of TancoiteHide

Classification of TancoiteHide

8.BG.15

8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
G : With medium-sized and large cations, (OH, etc.):RO4 = 0.5:1
41.4.7.1

41 : ANHYDROUS PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
4 : (AB)5(XO4)2Zq
19.8.4

19 : Phosphates
8 : Phosphates of Al and other metals

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

Physical Properties of TancoiteHide

Vitreous, Sub-Vitreous
Transparency:
Transparent
Colour:
Colorless to light pink
Streak:
White
Hardness:
4 - 4½ on Mohs scale
Tenacity:
Brittle
Cleavage:
Imperfect/Fair
{010} and {100}
Fracture:
Conchoidal, Sub-Conchoidal
Density:
2.752 g/cm3 (Measured)    2.724 g/cm3 (Calculated)

Optical Data of TancoiteHide

Type:
Biaxial (-)
RI values:
nα = 1.541 nβ = 1.563 nγ = 1.564
2V:
Measured: 23° , Calculated: 24°
Birefringence:
0.023
Max. Birefringence:
δ = 0.023
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:
Low (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.
Dispersion:
r
Optical Extinction:
XYZ = cba
Pleochroism:
Non-pleochroic

Chemistry of TancoiteHide

Mindat Formula:
LiNa2Al(PO4)(PO3OH)(OH)
Element Weights:
Element% weight
O50.022 %
P21.520 %
Na15.973 %
Al9.373 %
Li2.411 %
H0.700 %

Calculated from ideal end-member formula.
O
P
Na
Al
Li
H

Crystallography of TancoiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Pbca
Cell Parameters:
a = 14.08 Å, b = 14.13 Å, c = 6.97 Å
Ratio:
a:b:c = 0.996 : 1 : 0.493
Unit Cell V:
1,386.68 ų (Calculated from Unit Cell)
Z:
8
Comment:
Pbcb

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0015695TancoiteHawthorne F C (1983) The crystal structure of tancoite Tschermaks Mineralogische und Petrographische Mitteilungen 31 121-13519830293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Geological EnvironmentHide

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

Type Occurrence of TancoiteHide

General Appearance of Type Material:
Isolated crystals up to 1 mm in length and as druses of columnar individuals, oriented subparallel to [001].
Place of Conservation of Type Material:
Harvard Mineralogical Museum, Cambridge, Massachusetts, USA, number 117129 (cotype).
University of Manitoba, Winnipeg, Manitoba, Canada, number M5553/4 (cotype).
Natural History Museum, London, United Kingdom, number BM 1980,52 (cotype).
National Museum of Natural History, Washington, D.C., USA, number 146248 (type).
Royal Ontario Museum, Toronto, Ontario, Canada, number M36416-M34418 (cotype).
Geological Setting of Type Material:
LCA granite pegmatite.
Associated Minerals at Type Locality:

Synonyms of TancoiteHide

Other Language Names for TancoiteHide

Dutch:Tancoiet
German:Tancoit
Spanish:Tancoita

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Tancoite associated with LithiophosphateLi3PO4
1 photo of Tancoite associated with 'Apatite'Ca5(PO4)3A

Related Minerals - Strunz-mindat GroupingHide

8.BG.AldomarinoiteSr2Mn3+(AsO4)2(OH)Mon. 2/m : P21/m
8.BG.DongchuanitePb4ZnZn2(PO4)4(OH)2Tric. 1 : P1
8.BG.CuprodongchuanitePb4CuZn2(PO4)4(OH)2Tric. 1 : P1
8.BG.CanosioiteBa2Fe3+(AsO4)2(OH)Mon. 2/m : P21/m
8.BG.05FeinglositePb2Zn(AsO4)2 · H2OMon. 2/m
8.BG.05TokyoiteBa2Mn3+(VO4)2(OH)Mon. 2/m : P21/m
8.BG.05LombardoiteBa2Mn3+(AsO4)2(OH)Mon. 2/m : P21/m
8.BG.05BearthiteCa2Al(PO4)2(OH)Mon. 2/m : P21/m
8.BG.05'Unnamed (possible ordered As-analogue of Tokyoite)'Ba2Mn[(As,V)O4]2(OH)Mon. 2/m : P21/m
8.BG.05GamagariteBa2Fe3+(VO4)2(OH)Mon. 2/m : P21/m
8.BG.05ArsentsumebitePb2Cu(AsO4)(SO4)(OH)Mon. 2/m : P21/m
8.BG.05'UM1994-19-PO:CuHMoPb'Pb2Cu(PO4)(MoO4,AsO4,CrO4,GaO4)(OH)
8.BG.05FerribushmakinitePb2Fe3+(PO4)(VO4)(OH)Mon. 2/m : P21/m
8.BG.05ArsenbrackebuschitePb2Fe3+(AsO4)2(OH)Mon. 2/m : P2/m
8.BG.05GoedkeniteSr2Al(PO4)2(OH)Mon. 2/m : P21/m
8.BG.05TsumebitePb2Cu(PO4)(SO4)(OH)Mon. 2/m : P21/m
8.BG.05BrackebuschitePb2Mn3+(VO4)2(OH)Mon. 2/m : P21/m
8.BG.05BushmakinitePb2Al(PO4)(VO4)(OH)Mon. 2/m : P21/m
8.BG.05CalderónitePb2Fe3+(VO4)2(OH)Mon. 2/m : P21/m
8.BG.10MélonjosephiteCaFe2+Fe3+(PO4)2(OH)Orth. mmm(2/m2/m2/m) : Pbam
8.BG.20DmisokoloviteK3Cu5AlO2(AsO4)4Mon. 2/m : B2/b
8.BG.25ShchurovskyiteK2CaCu6O2(AsO4)4Mon. 2 : B2
8.BG.30WrightiteK2Al2O(AsO4)2Orth. mmm(2/m2/m2/m) : Pmma
8.BG.35PolyarsiteNa7CaMgCu2(AsO4)4F2ClMon. 2/m

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 TancoiteHide

References for TancoiteHide

Localities for TancoiteHide

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.
Canada (TL)
 
  • Manitoba
    • Lac-du-Bonnet area
      • Bernic Lake
153-155. +4 other references
 
and/or  
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