Ianthinite
About Ianthinite
May be confused with nollmotzite.
Sheets in the crystal structure are similar to those in rameauite, spriggite and wyartite.
Unique Identifiers
IMA Classification of Ianthinite
Classification of Ianthinite
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
G : Uranyl Hydroxides
A : Without additional cations
5 : OXIDES CONTAINING URANIUM OR THORIUM
6 : AX6O17·xH2O
7 : Oxides and Hydroxides
16 : Oxides of U
Mineral Symbols
Symbol | Source | Reference |
---|---|---|
Ian | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Pronunciation of Ianthinite
Play | Recorded by | Country |
---|---|---|
Jolyon Ralph | United Kingdom |
Physical Properties of Ianthinite
Perfect on {001}
Optical Data of Ianthinite
Based on recorded range of RI values above.
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.
Y = b = violet
Z = a = dark violet
Chemistry of Ianthinite
Crystallography of Ianthinite
Crystal Structure
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0013139 | Ianthinite | Burns P C, Finch R J, Hawthorne F C, Miller M L, Ewing R C (1997) The crystal structure of ianthinite, [U4+2(UO2)4O6(OH)4](H2O)5: a possible phase for Pu4+ incorporation during the oxidation of spent nuclear fuel Journal of Nuclear Materials 249 199-206 | 1997 | Shinkolobwe mine, Shaba, southern Congo | 0 | 293 |
X-Ray Powder Diffraction
d-spacing | Intensity |
---|---|
7.63 Å | (FF) |
3.81 Å | (m) |
3.24 Å | (m) |
3.59 Å | (fm) |
3.35 Å | (fm) |
2.61 Å | (f) |
2.53 Å | (f) |
Geological Environment
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Near-surface Processes | |
27 : Radioactive decay; auto-oxidation | |
Stage 7: Great Oxidation Event | <2.4 |
47a : [Near-surface hydration of prior minerals] | |
47f : [Uranyl (U⁶⁺) minerals] |
Type Occurrence of Ianthinite
Synonyms of Ianthinite
Other Language Names for Ianthinite
Common Associates
31 photos of Ianthinite associated with Schoepite | (UO2)8O2(OH)12 · 12H2O |
6 photos of Ianthinite associated with Parauranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
4 photos of Ianthinite associated with Uraninite | UO2 |
2 photos of Ianthinite associated with Umohoite | (UO2)MoO4 · 2H2O |
2 photos of Ianthinite associated with Uranopilite | (UO2)6(SO4)O2(OH)6 · 14H2O |
2 photos of Ianthinite associated with Fourmarierite | Pb(UO2)4O3(OH)4 · 4H2O |
1 photo of Ianthinite associated with Curite | Pb3(H2O)2[(UO2)4O4(OH)3]2 |
1 photo of Ianthinite associated with Gypsum | CaSO4 · 2H2O |
1 photo of Ianthinite associated with Arsenuranospathite | Al(UO2)2(AsO4)2F · 20H2O |
1 photo of Ianthinite associated with Pyrite | FeS2 |
Related Minerals - Strunz-mindat Grouping
4.GA.05 | Paraschoepite | UO3 · 2H2O |
4.GA.05 | Metaschoepite | (UO2)8O2(OH)12 · 10H2O |
4.GA.05 | Schoepite | (UO2)8O2(OH)12 · 12H2O |
4.GA.15 | Metastudtite | UO4 · 2H2O |
4.GA.15 | Studtite | [(UO2)(O2)(H2O)2] · H2O |
4.GA.20 | Paulscherrerite | UO2(OH)2 |
4.GA.25 | Heisenbergite | UO2(OH) · 2H2O (simplified UO3 · 2H2 O) |
Radioactivity
Element | % Content | Activity (Bq/kg) | Radiation Type |
---|---|---|---|
Uranium (U) | 75.9539% | 18,988,475 | 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.
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: –
Distance | Dose rate | Risk |
---|---|---|
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 Information
Alters upon heating with dilute hydrogen peroxide, turning brown, then yellow.
Internet Links for Ianthinite
Please feel free to link to this page.
References for Ianthinite
Localities for Ianthinite
Locality List




All localities listed without proper references should be considered as questionable.
Australia | |
| Bottrill (2018) |
Brazil | |
| Pires et al. (2014) |
DR Congo (TL) | |
| Guillemin et al. (1959) +2 other references |
Gauthier et al. (1989) | |
Egypt | |
| Hussein et al. (1988) |
France | |
| - (1998) |
J. Chervet et G. Branche : ... +1 other reference | |
| - (1998) |
J. Geffroy | |
| Marcel Roubault et al. (1960 -1965) +1 other reference |
| Lièvre et al. (2002) |
| Lièvre et al. (2002) |
| - (1998) |
- (1998) | |
| - (1998) |
| Bariand et al. (1993) +1 other reference |
| Henriot et al. (1998) |
- (1998) | |
Germany | |
| Kolitsch (1997) +3 other references |
| Walenta (1989) |
| |
| Weiß (1990) |
Dill et al. (2010) | |
Greece | |
| Rieck et al. (2018) |
India | |
| Singh et al. (2015) |
| SINGH et al. (2014) |
Italy | |
| Olmi F. |
| Campostrini et al. (2006) |
Mexico | |
| |
www.swri.org (2001) | |
Slovakia | |
| Koděra (1986) |
| Koděra (1986) |
| Koděra (1986) |
USA | |
| Eckel et al. (1997) |
| Gross (1965) +1 other reference |
Eckel et al. (1997) |
Krunkelbach Valley Uranium deposit, Menzenschwand, St Blasien, Waldshut, Freiburg Region, Baden-Württemberg, Germany