Cuprosklodowskite

IMA-GP
Uranium 53.3.1.4
(Dana Classification Number)
(Images) 8/B.34-20
(Strunz ID)


Madam Marie Curie
(1867-1934)
1903 Nobel Laureate in Physics
1911 Nobel Laureate in Chemistry

Property Data Remarks
Named for: in the mistaken belief that it was the copper analogue of Sklodowskite, which in turn was named for Marie Curie (née Maria Sklodowska), (1867 - 1934), 1903 Nobel Laureate in Physics, and 1911 Nobel Laureate in Chemistry.
Alternate
    Name(s):
  •  
    Mineral Class:
    Silicates
      NesosilicatesNesosilicates
    "Insel" silicates with anions unfamiliar to tetraheders.
    Uranyl-"Insel" silicates with [UO2]2+ - [SiO4]4-
        Sklodowskite - Uranophane - Kasolite series
     
    Chemical
        Formula:
    Cu(UO2)2Si2O7 . 6H2O  
    Chemical
        Composition:
    Copper: (Cu) 7.37%
    Hydrogen: (H) 1.17%
    Oxygen: (O) 29.70%
    Silicon: (Si) 6.52%
    Uranium: (U) 55.24%
    by weight
    Molecular
        Weight:
    861.84 daltons (amu)
    Specific
        Radioactivity:

    (All radiation is for a 1 gram, fully aged specimen)

    Specific Activity Dose Rate
    Becquerels Curies milliRems/hour microSieverts/hour
    9.8874 × 1004 2.67 × 10-06 1.36 136.14

    Estimated Average Annual Exposure: 360 mRem (3.6 milliSieverts)

    Crystalography:
    System: Triclinic - Pinacoidal
    Axial Ratios: a: 0.7609
    b: 1
    c: 0.7181
    Cell Dimensions: a: 7.052 Å
    b: 9.267 Å
    c: 6.655 Å
    Z: 1
    a: 109.23°
    b: 89.84°
    g: 110.01°
    V: 385.85 Å3
    DenCalc: 3.71
    H-M Symbol: -1
    Space Group: P-1
    X-Ray Diffraction:
      By Intensity ( I/Io )
    (1): 8.16 Å
    (0.9): 4.82 Å
    (0.7): 6.06 Å
    Cuprosklodowskite
    Crystal
    Habit:
  • Acicular flat bladed crystals (typical)
  • Crusts
  • Fibrous tufts
  • Radial aggregates
  •  
    Cleavage:
    [001]  
    [010]  
    [100] Good
     
    Fracture: Uneven  
    Moh's
        Hardness:
    4  
    Density: 3.8 grams/cm3
    Color: Grass green to dark green  
    Streak: Greenish yellow to light Green  
    Luster: Vitreous to Silky  
    Diaphaneity: Transparent to Translucent  
    Pleochroism:
    (x):  
    (y:)  
    (z:)  
     
    Ultra Violet
        Fluorescence:
    None

    (Expected to be non-fluorescent due to copper being a common fluorescence 'poison')
    (two Specimens Examined)
    Magnetism: Non-magnetic  
    Occurance:

    Formed from the oxidation of copper and uranium bearing minerals.

     
    Associated
        Minerals:

    Autunite, Barite, Becquerelite, Bornite, Brochantite, Calcite, Chalcocite, Chalcopyrite, Chrysocolla, Covellite, Curite, Dolomite, Galena, Goethite, Hematite, Kasolite, Malachite, Metatorbernite, Metazeunerite, Pyrite, Quartz, Schoepite, Sklodowskite, Soddyite, Sphalerite, Torbernite, Tyuyamunite, Uraninite, Uranophane, Uranopilite, Zippeite

    Mineral   -   > 65% of sites
    Mineral   -   > 50% of sites
    Mineral   -   > 31% of sites
    Minerals   -   Uranium & Thorium
    mineral links

    These are minerals known to be found with Cuprosklodoskite
    Localities:

    Relatively common

    Cuprosklodoskite Localities
    Notes:

    Strongly radioactive a- and b-particles, g-rays.

    Crystals are probably metamict.

    Cuprosklodowskite Images

    Specimen #1
    (001) (001a) (001b) (001c)

    Kambove (Kakanda) Mine, Katanga District, Shaba (Katanga), Congo (Zaïre)


    Specimen Notes

    This specimen shows the radial clusters of Cuprosklodowskite so closely intergrown that they form a tangle of crystals. This is not unusual for Cuprosklodowskite that has grown in a vug.

    See the notes for specimen #3 below.
     


    Specimen #4
    (004a) (004b) (004c) (004d)

    (with Metatyuyamunite)

    (with Metatyuyamunite)
    (004e)
    Mashamba West Mine, Kolwezi, Shaba (Katanga), Congo (Zaïre)


    Specimen #4 Notes

    This specimen is primarily Metatyuyamunite, but has a minimum of eight uranium minerals on its surface. See Metatorbernite Specimen #2 for detailed notes on this specimen.

    Image 004a shows the Cuprosklodowskite's habit of forming bladed crystals. Image 004b shows the terminations are both single and double beveled chissel shaped.

    Image 004c shows the habit of the crystals forming radial clusters. While visable in the other images, this one illustrates this habit quite graphically.

    Images 004d and 004e show how the crystals grow primarilly from the end. When the crystal encounters an obstacle, its growth is stopped, while that portion of the crystal not blocked continues to grow.