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Derriksite

A valid IMA mineral species
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About DerriksiteHide

02203570017271922557451.jpg
Jean-Marie François Joseph Derriks
Formula:
Cu4(UO2)(SeO3)2(OH)6
Formula originally assumed to contain 1 water molecule.
Colour:
Dark green to bottle-green, clear green
Specific Gravity:
4.61 (Calculated)
Crystal System:
Orthorhombic
Name:
After Jean-Marie François "Joseph" Derriks (Huy, Belgium, August 8 1912 - Angleur (Liège) March 5 1992), geologist and administrator of the Union Minière du Haut Katanga (UMHK).
This page provides mineralogical data about Derriksite.


Unique IdentifiersHide

Mindat ID:
1264
Long-form identifier:
mindat:1:1:1264:1

IMA Classification of DerriksiteHide

Classification of DerriksiteHide

4.JG.30

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
G : Selenites with additional anions, without H2O
34.7.5.1

34 : SELENITES, TELLURITES AND SULFITES
7 : Hydrated Selenites, Tellurites and Sulfites containing Hydroxyl or Halogen
28.1.7

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

Physical Properties of DerriksiteHide

Transparency:
Translucent
Colour:
Dark green to bottle-green, clear green
Cleavage:
Distinct/Good
Good on (010)
Density:
4.61 g/cm3 (Calculated)

Optical Data of DerriksiteHide

Type:
Biaxial (-)
RI values:
nα = 1.77 nβ = 1.85 nγ = 1.89
Max. Birefringence:
δ = 0.120
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.

No measured or calculated 2V is on file for this mineral, so the value used here (68°) is estimated from its recorded refractive indices and optic sign, not from a direct 2V measurement.
Dispersion:
r > v distinct
Optical Extinction:
X = a; Y = b; Z = c.

Chemistry of DerriksiteHide

Mindat Formula:
Cu4(UO2)(SeO3)2(OH)6

Formula originally assumed to contain 1 water molecule.
Element Weights:
Element% weight
Cu28.879 %
U27.043 %
O25.449 %
Se17.942 %
H0.687 %

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

Crystallography of DerriksiteHide

Crystal System:
Orthorhombic
Cell Parameters:
a = 5.570(2) Å, b = 19.088(8) Å, c = 5.965(2) Å
Ratio:
a:b:c = 0.292 : 1 : 0.313
Unit Cell V:
634.20 ų (Calculated from Unit Cell)
Z:
2
Comment:
Pn21m

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0009986DerriksiteGinderow D, Cesbron F (1983) Structure da la derriksite, Cu4(UO2)(SeO3)2(OH)6 Acta Crystallographica C39 1605-16071983Musoni, Shaba, Ziare0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
4.78 Å(very very strong)
4.072 Å(very strong)
3.748 Å(very strong)
4.352 Å(strong)
3.218 Å(strong)
5.35 Å(moderately strong)
4.197 Å(moderately strong)
Comments:
Musonoi mine, Congo. Data from the type description.

Geological EnvironmentHide

Type Occurrence of DerriksiteHide

Place of Conservation of Type Material:
University of Pierre and Marie Curie, Paris, France, number 204, 12.251.
Natural History Museum, Paris, France, number 181.35.
National School of Mines, Paris, France, number 9.104.
Associated Minerals at Type Locality:

Synonyms of DerriksiteHide

Other Language Names for DerriksiteHide

Common AssociatesHide

Associations Based on Photo Data:
13 photos of Derriksite associated with DemesmaekeritePb2Cu5(UO2)2(SeO3)6(OH)6 · 2H2O
12 photos of Derriksite associated with MalachiteCu2(CO3)(OH)2
8 photos of Derriksite associated with ChalcomeniteCuSeO3 · 2H2O
4 photos of Derriksite associated with GuilleminiteBa(UO2)3(SeO3)2O2 · 3H2O
3 photos of Derriksite associated with DigeniteCu9S5
2 photos of Derriksite associated with MarthoziteCu2+(UO2)3(SeO3)2O2 · 8H2O
1 photo of Derriksite associated with CobaltomeniteCoSeO3 · 2H2O
1 photo of Derriksite associated with MetatorberniteCu(UO2)2(PO4)2 · 8H2O
1 photo of Derriksite associated with BaryteBaSO4
1 photo of Derriksite associated with QuartzSiO2

Related Minerals - Strunz-mindat GroupingHide

4.JG.PrewittiteKPb1.5ZnCu6(SeO3)2O2Cl10Orth. mmm(2/m2/m2/m) : Pnnm
4.JG.MasaitisiteKCu5O2(SeO3)2Cl3Orth. mmm(2/m2/m2/m) : Pnma
4.JG.WangkuirenitePb3Cl2(SeO3)2Mon. 2/m : B2/b
4.JG.GuangyuanitePb3Cl3(Se4+O3)(OH)Orth. mmm(2/m2/m2/m) : Pnma
4.JG.05GeorgbokiiteCu5(SeO3)2O2Cl2Mon. 2/m : P21/c
4.JG.05ParageorgbokiiteCu5(SeO3)2O2Cl2Mon. 2/m : P21/c
4.JG.10ChloromeniteCu9(SeO3)4O2Cl6Mon. 2/m : B2/m
4.JG.15SofiiteZn2(SeO3)Cl2Orth. mmm(2/m2/m2/m) : Pccn
4.JG.20Ilinskite(Na,K)Cu5(SeO3)2O2Cl3Orth. mmm(2/m2/m2/m) : Pnma
4.JG.25FrancisiteCu3Bi(SeO3)2O2ClOrth. mmm(2/m2/m2/m) : Pmmn
4.JG.35BurnsiteKCdCu2+7(SeO3)2O2Cl9Hex. 6/mmm(6/m2/m2/m) : P63/mmc
4.JG.40AllochalcoseliteCu+PbCu2+5(SeO3)2Cl5O2Mon. 2/m : B2/m
4.JG.45NicksoboleviteCu7(SeO3)2O2Cl6Mon. 2/m : P21/c
4.JG.50PlumboselitePb3O2(SeO3)Orth. mm2 : Cmc21
4.JG.55SarrabusitePb5CuCl4(SeO3)4Mon. 2/m : B2/b

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 27.0434% 6,760,850 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

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 DerriksiteHide

References for DerriksiteHide

Reference List:

Localities for DerriksiteHide

Showing 2 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
 
  • Olomouc Region
    • Jeseník District
      • Javorník
        • Zálesí
Pauliš et al. (2016)
DR Congo (TL)
 
  • Lualaba
    • Mutshatsha
      • Kolwezi
Cesbron et al. (1971) +2 other references
 
and/or  
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