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VOOZH | about |
| Uranocircite I | Ba(UO2)2(PO4)2 · 12H2O |
| Symbol | Source | Reference for Standard |
|---|---|---|
| Urc-II | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
| 'Autunite' | Ca(UO2)2(PO4)2 · 10-12H2O |
| 'Torbernite' | Cu(UO2)2(PO4)2 · 12H2O |
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 47a : [Near-surface hydration of prior minerals] | |
| 47c : [Carbonates, phosphates, borates, nitrates] | |
| 47f : [Uranyl (U⁶⁺) minerals] |
| Autunite | Ca(UO2)2(PO4)2 · 10-12H2O | Orth. mmm(2/m2/m2/m) : Pnma |
| Bassetite | Fe2+(UO2)2(PO4)2 · 10H2O | Mon. 2/m |
| Heinrichite | Ba(UO2)2(AsO4)2 · 10H2O | Mon. 2/m : P2/b |
| Hydronováčekite | Mg(UO2)2(AsO4)2 · 12H2O | Tric. 1 : P1 |
| Kahlerite | Fe(UO2)2(AsO4)2 · 12H2O | Tet. 4/m : P42/n |
| Nováčekite | Mg(UO2)2(AsO4)2 · 10H2O | Mon. 2/m |
| Rauchite | Ni(UO2)2(AsO4)2 · 10H2O | Tric. 1 : P1 |
| Sabugalite | HAl(UO2)4(PO4)4 · 16H2O | Mon. 2/m : B2/m |
| Saléeite | Mg(UO2)2(PO4)2 · 10H2O | Mon. 2/m |
| Torbernite | Cu(UO2)2(PO4)2 · 12H2O | Tet. 4/mmm(4/m2/m2/m) : I4/mmm |
| Uranospinite | Ca(UO2)2(AsO4)2 · 10H2O | Tet. 4/mmm(4/m2/m2/m) : P4/nmm |
| Zeunerite | Cu(UO2)2(AsO4)2 · 12H2O | Tet. 4/mmm(4/m2/m2/m) : I4/mmm |
| 11 photos of Uranocircite associated with Quartz | SiO2 |
| 11 photos of Uranocircite associated with 'Smoky Quartz' | SiO2 |
| 6 photos of Uranocircite associated with Fluorite | CaF2 |
| 5 photos of Uranocircite associated with Orthoclase | K(AlSi3O8) |
| 2 photos of Uranocircite associated with Zircon | Zr(SiO4) |
| 2 photos of Uranocircite associated with Torbernite | Cu(UO2)2(PO4)2 · 12H2O |
| 2 photos of Uranocircite associated with Autunite | Ca(UO2)2(PO4)2 · 10-12H2O |
| 2 photos of Uranocircite associated with Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
| 1 photo of Uranocircite associated with Studtite | [(UO2)(O2)(H2O)2] · H2O |
| 1 photo of Uranocircite associated with Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
| 8.EB. | Meta-autunite Group | A1-2(UO2)2(TO4)2 · 5-10H2O | |
| 8.EB.05 | Rauchite | Ni(UO2)2(AsO4)2 · 10H2O | Tric. 1 : P1 |
| 8.EB.05 | Uranospinite | Ca(UO2)2(AsO4)2 · 10H2O | Tet. 4/mmm(4/m2/m2/m) : P4/nmm |
| 8.EB.05 | Zeunerite | Cu(UO2)2(AsO4)2 · 12H2O | Tet. 4/mmm(4/m2/m2/m) : I4/mmm |
| 8.EB.05 | Metarauchite | Ni(UO2)2(AsO4)2 · 8H2O | Tric. 1 : P1 |
| 8.EB.05 | Heinrichite | Ba(UO2)2(AsO4)2 · 10H2O | Mon. 2/m : P2/b |
| 8.EB.05 | Kahlerite | Fe(UO2)2(AsO4)2 · 12H2O | Tet. 4/m : P42/n |
| 8.EB.05 | Hydronováčekite | Mg(UO2)2(AsO4)2 · 12H2O | Tric. 1 : P1 |
| 8.EB.05 | Torbernite | Cu(UO2)2(PO4)2 · 12H2O | Tet. 4/mmm(4/m2/m2/m) : I4/mmm |
| 8.EB.05 | Nováčekite | Mg(UO2)2(AsO4)2 · 10H2O | Mon. 2/m |
| 8.EB.05 | Autunite | Ca(UO2)2(PO4)2 · 10-12H2O | Orth. mmm(2/m2/m2/m) : Pnma |
| 8.EB.05 | Saléeite | Mg(UO2)2(PO4)2 · 10H2O | Mon. 2/m |
| 8.EB.05 | Xiangjiangite | (Fe3+,Al)(UO2)4(PO4)2(SO4)2(OH) · 22H2O | Tet. |
| 8.EB.10 | Bassetite | Fe2+(UO2)2(PO4)2 · 10H2O | Mon. 2/m |
| 8.EB.10 | Lehnerite | Mn2+(UO2)2(PO4)2 · 8H2O | Mon. 2/m |
| 8.EB.10 | Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O | Tet. 4/mmm(4/m2/m2/m) |
| 8.EB.10 | Metasaléeite | Mg(UO2)2(PO4)2 · 8H2O | |
| 8.EB.10 | Metauranocircite | Ba(UO2)2(PO4)2 · 7H2O | Mon. 2 : P21 |
| 8.EB.10 | Metauranospinite | Ca(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P42/n |
| 8.EB.10 | Metaheinrichite | Ba(UO2)2(AsO4)2 · 8H2O | Mon. 2 : P21 |
| 8.EB.10 | Metakahlerite | Fe2+(UO2)2(AsO4)2 · 8H2O | Tric. 1 : P1 |
| 8.EB.10 | Metakirchheimerite | Co(UO2)2(AsO4)2 · 8H2O | Tric. 1 : P1 |
| 8.EB.10 | Metanováčekite | Mg(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P4/n |
| 8.EB.10 | Metanatroautunite | Na(UO2)(PO4)(H2O)3 | Tet. 4/mmm(4/m2/m2/m) : P4/ncc |
| 8.EB.10 | Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O | Tet. 4/m : P4/n |
| 8.EB.10 | Metazeunerite | Cu(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P42/n |
| 8.EB.10 | Przhevalskite | Pb2(UO2)3(PO4)2(OH)4 · 3H2O | Tet. |
| 8.EB.10 | 'Pseudo-autunite' | (H3O)4Ca2(UO2)2(PO4)4 · 5H2O | Orth. |
| 8.EB.15 | Abernathyite | K(UO2)(AsO4) · 3H2O | Tet. 4/mmm(4/m2/m2/m) : P4/ncc |
| 8.EB.15 | Uramphite | (NH4)2(UO2)2(PO4)2 · 6H2O | Tet. 4/mmm(4/m2/m2/m) : P4/nmm |
| 8.EB.15 | Meta-ankoleite | K2(UO2)2(PO4)2 · 6H2O | Tet. 4/mmm(4/m2/m2/m) : P4/nmm |
| 8.EB.15 | Natrouranospinite | Na2(UO2)2(AsO4)2 · 5H2O | Tet. 4/mmm(4/m2/m2/m) : P4/nmm |
| 8.EB.15 | Trögerite | (H3O)(UO2)(AsO4) · 3H2O | Tet. 4/mmm(4/m2/m2/m) : P4/nmm |
| 8.EB.15 | Chernikovite | (H3O)2(UO2)2(PO4)2 · 6H2O | Tet. 4/mmm(4/m2/m2/m) : P4/nmm |
| 8.EB.15 | Uramarsite | (NH4)(UO2)(AsO4) · 3H2O | Tet. 4/mmm(4/m2/m2/m) : P4/mmm |
| 8.EB.20 | Chistyakovaite | Al(UO2)2(AsO4)2(F,OH) · 6.5H2O | Mon. |
| 8.EB.20 | Threadgoldite | Al(UO2)2(PO4)2(OH) · 8H2O | Mon. |
| 8.EB.25 | Uranospathite | (Al,◻)(UO2)2(PO4)2F · 20(H2O,F) | Orth. mm2 : Pnn2 |
| 8.EB.25 | Arsenuranospathite | Al(UO2)2(AsO4)2F · 20H2O | Orth. mm2 : Pnn2 |
| 8.EB.30 | Vochtenite | (Fe2+,Mg)Fe3+(UO2)4(PO4)4(OH) · 12-13H2O | Mon. |
| 8.EB.35 | Coconinoite | Fe3+2Al2(UO2)2(PO4)4(SO4)(OH)2 · 20H2O | Mon. |
| 8.EB.40 | Ranunculite | HAl(UO2)(PO4)(OH)3 · 4H2O | Mon. 2/m : B2/b |
| 8.EB.45 | Triangulite | Al3(UO2)4(PO4)4(OH)5 · 5H2O | Tric. |
| 8.EB.50 | Furongite | Al13(UO2)7(PO4)13(OH)14 · 58H2O | Tric. 1 : P1 |
| 8.EB.55 | Arsenosabugalite | H0.5Al0.5(UO2)2(AsO4)2 · 8H2O | Tric. 1 : P1 |
| 8.EB.55 | Sabugalite | HAl(UO2)4(PO4)4 · 16H2O | Mon. 2/m : B2/m |
| 8.EB.60 | Horákite | (Bi7O7OH)[(UO2)4(PO4)2(AsO4)2(OH)2] · 3.5H2O | Mon. 2/m : B2/b |
| Element | % Content | Activity (Bq/kg) | Radiation Type |
|---|---|---|---|
| Uranium (U) | 45.4480% | 11,362,000 | α, β, γ |
| Thorium (Th) | 0.0000% | 0 | α, β, γ |
| Potassium (K) | 0.0000% | 0 | β, γ |
For comparison:
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
Showing 107 localities.
Australia | |
| Sorrell (n.d.) |
Austria | |
| Neschen (n.d.) |
| Exel (1993) |
Brazil | |
| Bruno Gioia specimen +1 other reference |
| |
Bulgaria | |
| Kalaidjiev et al. (2009) |
| Palache et al. (1951) | |
China | |
| Dahlkamp (2009) |
| National Geological Archives of China ... |
| National Geological Archives of China ... |
| Maozhong Min et al. (2005) |
| Dahlkamp (2009) |
| Dahlkamp (2009) | |
Czech Republic | |
| Hloušek et al. (2002) |
| M.E. Ciriotti |
| Jirásek et al. (2016) |
| Pauliš P. et al. (Kutna Hora, issue 1) |
| Pauliš P. et al. (Kutna Hora, issue 1) |
| Pauliš P. et al. (Kutna Hora, issue 1) |
| Škácha et al. (2017) |
DR Congo | |
| Gauthier et al. (1989) |
| Dewaele et al. (2016) |
France | |
| Cuchet et al. (2000) |
| R. Pierrot |
| |
| - (1998) |
| - (1998) | |
| OLLIC Pascal Collection +1 other reference |
| J. Geffroy |
| Asselborn (1983) +1 other reference |
| - (1998) |
| Schillinger et al. (2001) |
| - (1998) |
| - (1998) |
| - (1998) |
| Pierrot et al. (1973) |
| - (1998) | |
| R. Pierrot |
| R. Pierrot |
| R. Pierrot | |
| - (1998) | |
| - (1998) |
| R. Pierrot |
| |
| |
| Meisser et al. (2008) |
| - (1998) |
| - (1998) |
| |
| - (1998) |
| R. Pierrot |
| MAURY (S) +1 other reference |
Gabon | |
| Lheur et al. (2001) |
Germany | |
| Weiß (1990) |
| Walenta (1992) |
| Walenta (1992) | |
| Habel et al. (1994) |
| www.mineralienatlas.de (n.d.) |
| Lorenz (2004) |
| Dill et al. (2013) |
| collection H.J. Haas |
| Weiß (1990) |
| Bald +1 other reference | |
| Weiß (1990) |
| in the collection of Joachim Esche | |
| Dill et al. (2010) +1 other reference | |
| Martin et al. (1994) |
| Wittern (2001) |
| Lapis 30 (7/8) |
| Herrmann et al. (2007) |
| Weisbach (1877) +2 other references |
| Tröger (2006) +1 other reference |
| Matt Wall |
| Wittern (2001) | |
Japan | |
| Hayashi & Nagashima (1965) |
Madagascar | |
| Behier (1959) |
| Behier (1960) |
Niger | |
| |
Poland | |
| Mochnacka K. 1975: Mineralizacja skał ... +2 other references |
| Lis et al. (1986) | |
| Syczewski et al. (2023) |
Portugal | |
| LNEG - Laboratório Nacional de Energia ... |
| LNEG - Laboratório Nacional de Energia ... |
| LNEG - Siorminp database information |
| Palache et al. (1951) |
| LNEG |
| LNEG/Siorminp database +1 other reference |
| Mineralien Atlas |
| |
Russia | |
| Kovalev et al. (2017) |
South Korea | |
| Jeong et al. (1999) |
Spain | |
| Desor (07/2020) |
| Menor et al. (2010) |
Tajikistan | |
| Chernikov et al. (1997) |
USA | |
| Austin (1964) +1 other reference |
| Granger (1959) |
| Granger (1959) +1 other reference |
| Granger (1959) |
| Troxel et al. (1957) +1 other reference |
| Eckel et al. (1997) |
| Eckel et al. (1997) | |
| Meschter (1953) +3 other references |
| Jensen et al. (2012) |
| Januzzi et al. (1976) |
| Tom Loomis website |
| USGS: Geological Survey Circular 359 |
| Page et al. (1956) +3 other references |