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Guilleminite

A valid IMA mineral species
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About GuilleminiteHide

02688140017271923675102.jpg
Claude Guillemin in the field in Congo
Formula:
Ba(UO2)3(SeO3)2O2 · 3H2O
Colour:
Bright yellow
Lustre:
Waxy, Greasy, Dull, Earthy
Hardness:
2
Specific Gravity:
4.88
Crystal System:
Orthorhombic
Name:
Named by R. Pierrot, J. Toussaint, and T. Verbeek in 1965 in honor of Jean Claude Guillemin [September 13, 1923 France - April 6, 1994 France], chemist and mineralogist, 1957-1969 he was professor at the Ecole des Mines in Paris and curator of the mineral collection of the Ecole des Mines. Guillemin was director general of the Union Miniere du Haut-Katanga and co-founder of the International Mineralogical Association.
The Ba analogue of borzęckiite. Compare 'UM1966-05-SeO:BaHPbU'.


Unique IdentifiersHide

Mindat ID:
1771
Long-form identifier:
mindat:1:1:1771:4

IMA Classification of GuilleminiteHide

Classification of GuilleminiteHide

4.JJ.10

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
J : Selenites with additional anions, with H2O
34.7.3.1

34 : SELENITES, TELLURITES AND SULFITES
7 : Hydrated Selenites, Tellurites and Sulfites containing Hydroxyl or Halogen
28.1.9

28 : Selenites, Selenates, Tellurites, and Tellurates
1 : Selenites

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

Physical Properties of GuilleminiteHide

Waxy, Greasy, Dull, Earthy
Transparency:
Translucent
Colour:
Bright yellow
Streak:
Light yellow
Hardness:
Hardness Data:
Estimated
Tenacity:
Brittle
Cleavage:
Perfect
{100} perfect, {010} good.
Density:
4.88(2) g/cm3 (Measured)    5.08 g/cm3 (Calculated)

Optical Data of GuilleminiteHide

Type:
Biaxial (-)
RI values:
nα = 1.720 nβ = 1.798 nγ = 1.805
2V:
Measured: 35° , Calculated: 32°
Birefringence:
0.085
Max. Birefringence:
δ = 0.085
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 strong
Optical Extinction:
Parallel. X = c; Y = b; Z = a.
Pleochroism:
Strong
Comments:
X = bright yellow; Y = yellow; Z = colorless.

Chemistry of GuilleminiteHide

Mindat Formula:
Ba(UO2)3(SeO3)2O2 · 3H2O
Element Weights:
Element% weight
U55.469 %
O21.128 %
Se12.267 %
Ba10.667 %
H0.470 %

Calculated from ideal end-member formula.
U
O
Se
Ba
H

Crystallography of GuilleminiteHide

Crystal System:
Orthorhombic
Class (H-M):
mm2 - Pyramidal
Space Group:
Pmn21
Cell Parameters:
a = 7.29 Å, b = 16.87 Å, c = 7.07 Å
Ratio:
a:b:c = 0.432 : 1 : 0.419
Unit Cell V:
869.48 ų (Calculated from Unit Cell)
Z:
2
Morphology:
As rectangular crystals, tabular on {010}. Forms include {001}, {010}, {001}, and minor {101}.
Comment:
Space group is P21nm

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0005466GuilleminiteCooper M A, Hawthorne F C (1995) The crystal structure of guilleminite, a hydrated Ba-U-Se sheet structure The Canadian Mineralogist 33 1103-110919950293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
8.39 Å(100)
7.29 Å(100)
6.68 Å(60)
6.51 Å(20)
3.55 Å(80)
3.17 Å(40)
3.04 Å(60)
2.80 Å(60)
Comments:
ICDD 18-582.

Geological EnvironmentHide

Type Occurrence of GuilleminiteHide

General Appearance of Type Material:
Canary-yellow coatings and silky masses up to 1 cm2. In geodes, it forms tablets up to 0.4 x 0.2 mm.
Place of Conservation of Type Material:
National School of Mines, Paris, France.
National Museum of Natural History, Washington, D.C., USA, 119360.
Geological Setting of Type Material:
Oxidized zone of a uranium-selenium-copper deposit.
Associated Minerals at Type Locality:

Synonyms of GuilleminiteHide

Other Language Names for GuilleminiteHide

Common AssociatesHide

Associations Based on Photo Data:
59 photos of Guilleminite associated with MalachiteCu2(CO3)(OH)2
26 photos of Guilleminite associated with VandenbrandeiteCu(UO2)(OH)4
24 photos of Guilleminite associated with DigeniteCu9S5
20 photos of Guilleminite associated with CuprosklodowskiteCu(UO2)2(SiO3OH)2 · 6H2O
13 photos of Guilleminite associated with MarthoziteCu2+(UO2)3(SeO3)2O2 · 8H2O
12 photos of Guilleminite associated with DemesmaekeritePb2Cu5(UO2)2(SeO3)6(OH)6 · 2H2O
5 photos of Guilleminite associated with WulfenitePb(MoO4)
5 photos of Guilleminite associated with KasolitePb(UO2)(SiO4) · H2O
5 photos of Guilleminite associated with TorberniteCu(UO2)2(PO4)2 · 12H2O
4 photos of Guilleminite associated with DerriksiteCu4(UO2)(SeO3)2(OH)6

Related Minerals - Strunz-mindat GroupingHide

4.JJ.KristekiteCu2(H2O)4(UO2)(SeO3)3 · 4H2OMon. 2/m : P21/m
4.JJ.XLarisaiteNa(H3O)(UO2)3(SeO3)O2 · 4H2OMon. m : Pm
4.JJ.BorzęckiitePb(UO2)3(SeO3)2O2 · 3H2OOrth. mm2
4.JJ.PetermegawiteAl6(Se4+O3)3[SiO3(OH)](OH)9 · 10H2OOrth. mm2 : Cmc21
4.JJ.Amurselite(NH4)2(UO2)5(SeO3)3O2(OH)2(H2O) · 8H2OTric. 1 : P1
4.JJ.05MarthoziteCu2+(UO2)3(SeO3)2O2 · 8H2OOrth. mm2
4.JJ.15PiretiteCa(UO2)3(SeO3)2(OH)4 · 4H2OOrth.
4.JJ.20DemesmaekeritePb2Cu5(UO2)2(SeO3)6(OH)6 · 2H2OTric. 1 : P1
4.JJ.25Haynesite(UO2)3(Se4+O3)2(OH)2 · 5H2OOrth.
4.JJ.30FavreauitePbBiCu6O4(SeO3)4(OH) · H2OTet. 4/m : P4/n

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 55.4686% 13,867,150 α, β, γ
Thorium (Th) 0.0000% 0 α, β, γ
Potassium (K) 0.0000% 0 β, γ

For comparison:

  • Banana: ~15 Bq per fruit
  • Granite: 1,000–3,000 Bq/kg
  • EU exemption limit: 10,000 Bq/kg

Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.

Interactive Simulator:

Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!

Activity:

DistanceDose rateRisk
1 cm
10 cm
1 m

The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).

D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield

Fluorescence of GuilleminiteHide

Not fluorescent.

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 GuilleminiteHide

References for GuilleminiteHide

Reference List:

Localities for GuilleminiteHide

Showing 5 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.
Czech Republic
 
  • Central Bohemian Region
    • Příbram District
      • Příbram
        • Bytíz
Plášil et al. (2026)
DR Congo
 
  • Haut-Katanga
    • Kambove Territory
      • Shinkolobwe
KMMA +1 other reference
  • Lualaba
    • Mutshatsha
      • Kolwezi
Pierrot et al. (1965) +2 other references
France
 
  • Auvergne-Rhône-Alpes
    • Puy-de-Dôme
      • Clermont-Ferrand
        • Olloix
- (1998) +1 other reference
Spain
 
  • Catalonia
    • Lleida
      • Pallars Jussà
        • La Vall Fosca
          • La Torre de Cabdella
            • Castell-estaó
Castillo-Oliver et al. (2019)
 
and/or  
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