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Cliffordite

A valid IMA mineral species
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About ClifforditeHide

05109870017271922312883.jpg
Clifford Frondel
Formula:
(UO2)Te4+3O7
Colour:
Bright sulfur yellow
Lustre:
Adamantine
Hardness:
4
Specific Gravity:
6.57
Crystal System:
Isometric
Name:
Named by Richard V. Gaines in 1969 in honor of Clifford Frondel (8 January 1907, Brooklyn, New York, New York, USA - 12 November 2002, Winchester, Massachusetts, USA), American mineralogist, Professor of Mineralogy, Harvard University, Cambridge, Massachusetts, USA. The mineral frondelite is also named in his honor.
This page provides mineralogical data about Cliffordite.


Unique IdentifiersHide

Mindat ID:
1064
Long-form identifier:
mindat:1:1:1064:7

IMA Classification of ClifforditeHide

Approved
IMA Formula:
U6+Te4+3O9
Approval year:
1966
First published:
1969

Classification of ClifforditeHide

4.JK.75

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
K : Tellurites without additional anions, without H2O
34.3.1.1

34 : SELENITES, TELLURITES AND SULFITES
3 : A2(XO3)3·xH2O
28.3.18

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

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

Physical Properties of ClifforditeHide

Adamantine
Transparency:
Translucent
Colour:
Bright sulfur yellow
Hardness:
Density:
6.57 g/cm3 (Measured)    6.77 g/cm3 (Calculated)
Comment:
On synthetic material.

Optical Data of ClifforditeHide

Type:
Isotropic
RI values:
n = 2.25(2)
Surface Relief:
Very High
Comments:
On synthetic material

Chemistry of ClifforditeHide

Mindat Formula:
(UO2)Te4+3O7
Element Weights:
Element% weight
Te50.051 %
U31.122 %
O18.827 %

Calculated from ideal end-member formula.

Crystallography of ClifforditeHide

Crystal System:
Isometric
Class (H-M):
m3(2/m3) - Diploidal
Space Group:
Pa3
Cell Parameters:
a = 11.42(5) Å
Unit Cell V:
1,489.36 ų (Calculated from Unit Cell)
Z:
8
Morphology:
Octahedral crystals, crusts.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0009388ClifforditeGaly J, Meunier G (1971) A propos de la cliffordite UTe3O8. Le Systeme UO3-TeO2 a 700 C. Structure cristalline de UTe3O9 Acta Crystallographica B27 608-6161971synthetic0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.273 Å(100)
2.844 Å(80)
2.007 Å(80)
2.755 Å(70)
1.712 Å(70)
4.63 Å(60)
4.02 Å(60)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47e : [Vanadates, chromates, manganates]
47h : [Near-surface oxidized, dehydrated minerals]
Geological Setting:
Oxidized zones of hydrothermal Au-Ag telluride deposits.

Type Occurrence of ClifforditeHide

General Appearance of Type Material:
Crusts of bright yellow microscopic crystals, on joint surfaces in druses and scattered between mackayite crysals.
Place of Conservation of Type Material:
1) Natural History Museum, Paris, France, 175.83, 180.61.
2) Harvard University, Cambridge, Massachusetts, 119079.
3) National Museum of Natural History, Washington, D.C., USA, 120246, 164341, 164342.
Associated Minerals at Type Locality:

Synonyms of ClifforditeHide

Other Language Names for ClifforditeHide

Common AssociatesHide

Associations Based on Photo Data:
4 photos of Cliffordite associated with MackayiteFe3+(Te4+2O5)(OH)
1 photo of Cliffordite associated with QuartzSiO2

Related Minerals - Strunz-mindat GroupingHide

4.JK.MatthiasweilitePbTe4+O3Tric. 1 : P1
4.JK.05Walfordite(Fe3+,Te6+)Te4+3O8Iso. m3(2/m3) : Ia3
4.JK.05WinstanleyiteTiTe4+3O8Iso. m3(2/m3) : Ia3
4.JK.10ZincospiroffiteZn2Te4+3O8Mon. 2/m : B2/b
4.JK.10SpiroffiteMn2+2Te4+3O8Mon. 2/m : B2/b
4.JK.15BalyakiniteCu(TeO3)Orth. mmm(2/m2/m2/m)
4.JK.20RajiteCu(Te4+2O5)Mon. 2/m : P21/b
4.JK.25CarlfriesiteCaTe4+2Te6+O8Mon. 2/m : B2/b
4.JK.30ChenzhangruiteMnFe2+Te4+4O10Tet. 4/mmm(4/m2/m2/m) : P42/nbc
4.JK.30StankeithiteMn2+Mn2+Te4+4 O10Tet. 4 : P42
4.JK.30PaulhlavaiteCaCuTe4+ 4O10Mon. 2/m : B2/b
4.JK.30DenningiteCaMn2+Te4+4O10Tet. 4/mmm(4/m2/m2/m) : P42/nbc
4.JK.35ChekhovichiteBi2Te4+4O11Mon. 2/m
4.JK.40SmirniteBi2Te4+O5Orth. mm2
4.JK.45Choloalite(Cu,Sb)3(Pb,Ca)3(TeO3)6ClIso. 432 : P4132
4.JK.50FairbankitePb2+12(Te4+O3)11(SO4)Tric. 1 : P1
4.JK.55PlumbotelluritePb(TeO3)Mon. 2/m : B2/b
4.JK.60Magnolite[Hg2]2+[Te4+O3]Orth. mm2
4.JK.65MoctezumitePb(UO2)(TeO3)2Mon. 2/m : P21/b
4.JK.70Schmitterite(UO2)(TeO3)Orth. mmm(2/m2/m2/m)

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 31.1221% 7,780,525 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

Notes:
Soluble in concentrated HCl but insoluble in dilute acid.
Dissolves slowly in solutions of the alkali hydroxides.
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 ClifforditeHide

References for ClifforditeHide

Localities for ClifforditeHide

Showing 4 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.
Mexico
 
  • Sonora
    • Moctezuma Municipality
      • Moctezuma
Braith et al. (2001) +1 other reference
Anthony et al. (2016)
Gaines (1969)
Braith et al. (2001) +1 other reference
 
and/or  
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