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Thoreaulite

A valid IMA mineral species - grandfathered
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About ThoreauliteHide

02361410017271927148035.jpg
Jacques Thoreau (1885-1973)
Formula:
Sn2+Ta2O6
Minor Pb may replace the divalent Sn.
Colour:
Brown to yellow
Lustre:
Adamantine, Resinous
Hardness:
5½ - 6
Specific Gravity:
7.6 - 7.9
Crystal System:
Monoclinic
Member of:
Name:
Named in 1933 by Henri Buttgenbach in honor of Jacques Thoreau [September 27, 1886 Brussels, Belgium - January 11, 1973 Kessel-Lo, Belgium], Professor of Mineralogy, Université Catholique de Leuvain-UCL, Belgium.
Isostructural with:
Foordite-Thoreaulite Series.
Thoreaulite was first described by Buttgenbach (1933) from a pegmatite at the Manono Mine, Tanganyika, DR Congo.


Unique IdentifiersHide

Mindat ID:
3943
Long-form identifier:
mindat:1:1:3943:3

Similar NamesHide

TheraliteA rock subtype
ThraulitA synonym of Hisingerite

IMA Classification of ThoreauliteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Sn2+Ta5+2O6
First published:
1933

Classification of ThoreauliteHide

4.DG.15

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
D : Metal: Oxygen = 1:2 and similar
G : With large (+- medium-sized) cations; chains of edge-sharing octahedra
Dana 7th ed.:
8.3.10.1
8.3.10.1

8 : MULTIPLE OXIDES CONTAINING NIOBIUM,TANTALUM OR TITANIUM
3 : AB2O6
18.1.21

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

Physical Properties of ThoreauliteHide

Adamantine, Resinous
Transparency:
Opaque
Comment:
adamantine on the cleavage
Colour:
Brown to yellow
Streak:
Brown to yellow, slightly greenish
Hardness:
5½ - 6 on Mohs scale
Cleavage:
Perfect
On {100}; on {011} imperfect.
Density:
7.6 - 7.9 g/cm3 (Measured)    7.6(5) g/cm3 (Calculated)

Optical Data of ThoreauliteHide

Type:
Biaxial (+)
RI values:
nα = 2.39 nβ = 2.42 nγ = 2.52
2V:
Measured: 25° to 35°, Calculated: 60°
Birefringence:
On {100} cleavages = 0.039.
Max. Birefringence:
δ = 0.130
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.
Dispersion:
r < v
Pleochroism:
Non-pleochroic

Chemistry of ThoreauliteHide

Mindat Formula:
Sn2+Ta2O6

Minor Pb may replace the divalent Sn.
Element Weights:
Element% weight
Ta62.764 %
Sn20.588 %
O16.649 %

Calculated from ideal end-member formula.
Ta
Sn
O

Crystallography of ThoreauliteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/b
Setting:
C2/c
Cell Parameters:
a = 17.127(20) Å, b = 4.869(5) Å, c = 5.52(2) Å
β = 91°
Ratio:
a:b:c = 3.518 : 1 : 1.134
Unit Cell V:
460.25 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Crystals rough, prismatic [001].
Twinning:
Lamellar twins, with composition face {010}.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0015601ThoreauliteMaksimova N V, Ilyukhin V V, Belov N V (1975) Crystal structure of thoreaulite, SaTa2O6 Soviet Physics Doklady 20 528-5291975Manono, Katanga, Democratic Republic of the Congo0293
0000199ThoreauliteMumme W G (1970) The crystal structure of SnTa2O7, thoreaulite, an example of tin in five-fold coordination American Mineralogist 55 367-37719700293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.10 Å(100)
3.07 Å(100)
2.857 Å(80)
2.432 Å(80)
1.724 Å(80)
3.59 Å(60)
3.57 Å(60)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
26 : Hadean detrital minerals
Stage 4b: Highly evolved igneous rocks>3.0
34 : Complex granite pegmatites

Type Occurrence of ThoreauliteHide

General Appearance of Type Material:
Coarse crystals reaching several centimeters, without a characteristic shape and resembling wood tin.
Place of Conservation of Type Material:
University of Liège, Liège, Belgium, 2067 and 2068.
Geological Setting of Type Material:
Granite pegmatite (tin bearing)
Associated Minerals at Type Locality:

Synonyms of ThoreauliteHide

Other Language Names for ThoreauliteHide

Relationship of Thoreaulite to other SpeciesHide

Member of:
Other Members of Foordite Group:
FoorditeSn2+Nb2O6Mon. 2/m : B2/b
Forms a series with:

Common AssociatesHide

Associations Based on Photo Data:
10 photos of Thoreaulite associated with CassiteriteSnO2
7 photos of Thoreaulite associated with Rankamaite(Na,K)3(Ta,Nb,Al)11(O,OH)31
6 photos of Thoreaulite associated with AlbiteNa(AlSi3O8)
5 photos of Thoreaulite associated with LithiotantiteLiTa3O8
4 photos of Thoreaulite associated with QuartzSiO2
3 photos of Thoreaulite associated with Cesplumtantite(Cs,Na)2(Pb,Sb3+)3Ta8O24
1 photo of Thoreaulite associated with SimpsoniteAl4Ta3O13(OH)
1 photo of Thoreaulite associated with Lepidolite

Related Minerals - Strunz-mindat GroupingHide

4.DG.05FersmiteCaNb2O6Orth. mmm(2/m2/m2/m) : Pbcn
4.DG.05Uranopolycrase(U4+,Y)(Ti,Nb)2O6Orth. mmm(2/m2/m2/m) : Pbcn
4.DG.05Yttrocrasite-(Y)(Y,Th,Ca,U)(Ti,Fe)2(O,OH)6Amor.
4.DG.05Tanteuxenite-(Y)Y(Ta,Nb,Ti)2(O,OH)6Orth. mmm(2/m2/m2/m) : Pbcn
4.DG.05Loranskite-(Y)(Y,Ce,Ca)ZrTaO6 (?)
4.DG.05Euxenite-(Y)(Y,Ca,Ce,U,Th)(Nb,Ta,Ti)2O6Orth. mmm(2/m2/m2/m) : Pbcn
4.DG.05Kobeite-(Y)(Y,U)(Ti,Nb)2(O,OH)6 (?)Iso.
4.DG.10Yttrotantalite-(Y)(Y,U,Fe2+)(Ta,Nb)(O,OH)4Orth.
4.DG.10Clinofergusonite-(Y)YNbO4Mon. 2/m
4.DG.10Clinofergusonite-(Nd)(Nd,Ce)NbO4Mon.
4.DG.10Clinofergusonite-(Ce)CeNbO4Mon. 2/m : B2/m
4.DG.15FoorditeSn2+Nb2O6Mon. 2/m : B2/b
4.DG.20RaspitePb(WO4)Mon. 2/m : P21/b

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 ThoreauliteHide

References for ThoreauliteHide

Reference List:

Localities for ThoreauliteHide

Showing 10 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
 
  • Minas Gerais
    • Itinga
      • Monte Belo
Cassedanne et al. (1981) +1 other reference
China
 
  • Heilongjiang
    • Hegang
      • Luobei County
Deshi Lu (1993)
DR Congo
 
  • Maniema
Buttgenbach (1947)
Uher et al. (2008)
  • South Kivu
    • Walungu Territory
Vanrusselt (2023)
  • Tanganyika
Buttgenbach (1933) +1 other reference
Kazakhstan
 
  • East Kazakhstan Region
    • Irtysh River
Pekov (1998)
    • Ulan District
Voloshin et al. (1983) +1 other reference
Rwanda
 
  • Western Province
    • Ngororero District
      • Kabaya
Ann. Soc. Geol. Belgique
      • Muhororo
Bertossa (1968) +1 other reference
 
and/or  
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