Phurcalite
About Phurcalite
Unique Identifiers
Classification of Phurcalite
IMA Classification of Phurcalite
8 : PHOSPHATES, ARSENATES, VANADATES
E : Uranyl phosphates and arsenates
C : UO2:RO4 = 3:2
42 : HYDRATED PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
4 : (AB)5(XO4)2Zq·xH2O
19 : Phosphates
11 : Phosphates of U
Mineral Symbols
| Symbol | Source | Reference for Standard |
|---|---|---|
| Phu | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Phurcalite
{001} and {010}, perfect. Also {100}.
Optical Data of Phurcalite
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. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
Relative to Canada balsam mounting medium (n ≈ 1.537).
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.
Absorption: X < Y < Z.
Elongation positive.
Chemistry of Phurcalite
Chemical Analysis
| 1 | |
|---|---|
| UO3 | 65.2 % |
| CaO | 7.3 % |
| P2O5 | 16.8 % |
| H2O | 10.3 % |
| Total: | 99.6 % |
| ID | Locality | Reference | Notes |
|---|---|---|---|
| 1 | Putholi, Chittorgarh District, Udaipur Division, Rajasthan, India | Anhedral encrustation from fractures in quartzite. Method used for chemical analysis is not given. |
Crystallography of Phurcalite
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) |
|---|---|---|---|---|---|---|---|
| 0005255 | Phurcalite | Atencio D, Neumann R, Silva A J G C, Mascarenhas Y P (1991) Phurcalite from Perus, San Paulo, Brazil, and redetermination of its crystal structure The Canadian Mineralogist 29 95-105 | ![]() | 1991 | Perus, San Paulo, Brazil | 0 | 293 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 8.05 Å | (100) |
| 3.10 Å | (80) |
| 3.09 Å | (80) |
| 2.878 Å | (70) |
| 3.39 Å | (50) |
| 4.24 Å | (30) |
| 4.00 Å | (30) |
Geological Environment
| 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] |
Type Occurrence of Phurcalite
National Museum of Natural History, Washington, D.C., USA, number 144187.
Synonyms of Phurcalite
Other Language Names for Phurcalite
Relationship of Phurcalite to other Species
| Althupite | AlTh(UO2)7(PO4)4(OH)5O2 · 15H2O | Tric. 1 : P1 |
| Bergenite | Ca2Ba4(UO2)9(PO4)6O6 · 16H2O | Mon. 2/m : P21/b |
| Dewindtite | H2Pb3(UO2)6O4(PO4)4 · 12H2O | Orth. mmm(2/m2/m2/m) : Cmma |
| Dumontite | Pb2(UO2)3O2(PO4)2 · 5H2O | Mon. 2/m : P21/m |
| Françoisite-(Ce) | (Ce,Nd,Ca)(UO2)3(PO4)2O(OH) · 6H2O | Mon. 2/m : P21/b |
| Françoisite-(Nd) | (Nd,Ce,Sm)(UO2)3(PO4)2O(OH) · 6H2O | Mon. 2/m |
| Hügelite | Pb2(UO2)3(AsO4)2O2 · 5H2O | Mon. 2/m : P21/m |
| Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O | Orth. mmm(2/m2/m2/m) : Cmcm |
| Phuralumite | Al2[(UO2)3(PO4)2O(OH)](OH)3(H2O)9 | Mon. 2/m |
| Upalite | Al(UO2)3(PO4)2O(OH) · 7H2O | Mon. 2/m : P21/b |
| Vanmeersscheite | U6+(UO2)3(PO4)2(OH)6 · 4H2O | Orth. mmm(2/m2/m2/m) |
| Yingjiangite | K2Ca(UO2)7(PO4)4(OH)6 · 6H2O | Orth. mmm(2/m2/m2/m) : Cmcm |
Common Associates
| 20 photos of Phurcalite associated with Brochantite | Cu4(SO4)(OH)6 |
| 10 photos of Phurcalite associated with Malachite | Cu2(CO3)(OH)2 |
| 9 photos of Phurcalite associated with Torbernite | Cu(UO2)2(PO4)2 · 12H2O |
| 7 photos of Phurcalite associated with Autunite | Ca(UO2)2(PO4)2 · 10-12H2O |
| 6 photos of Phurcalite associated with Quartz | SiO2 |
| 5 photos of Phurcalite associated with Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
| 3 photos of Phurcalite associated with 'Manganese Oxides' | |
| 3 photos of Phurcalite associated with Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
| 2 photos of Phurcalite associated with 'Sandstone' | |
| 2 photos of Phurcalite associated with Haiweeite | Ca(UO2)2[Si5O12(OH)2] · 6H2O |
Related Minerals - Strunz-mindat Grouping
| 8.EC.05 | Upalite | Al(UO2)3(PO4)2O(OH) · 7H2O |
| 8.EC.05 | Françoisite-(Nd) | (Nd,Ce,Sm)(UO2)3(PO4)2O(OH) · 6H2O |
| 8.EC.05 | Françoisite-(Ce) | (Ce,Nd,Ca)(UO2)3(PO4)2O(OH) · 6H2O |
| 8.EC.05 | Phuralumite | Al2[(UO2)3(PO4)2O(OH)](OH)3(H2O)9 |
| 8.EC.10 | Yingjiangite | K2Ca(UO2)7(PO4)4(OH)6 · 6H2O |
| 8.EC.10 | Renardite | Pb(UO2)4(PO4)2(OH)4 · H2O |
| 8.EC.10 | Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
| 8.EC.10 | Arsenuranylite | Ca(UO2)4(AsO4)2(OH)4 · 6H2O |
| 8.EC.10 | 'Kivuite' | Th(UO2)4(PO3OH)2(OH)8 · 7H2O |
| 8.EC.10 | Dewindtite | H2Pb3(UO2)6O4(PO4)4 · 12H2O |
| 8.EC.15 | Dumontite | Pb2(UO2)3O2(PO4)2 · 5H2O |
| 8.EC.15 | Hügelite | Pb2(UO2)3(AsO4)2O2 · 5H2O |
| 8.EC.20 | Vanmeersscheite | U6+(UO2)3(PO4)2(OH)6 · 4H2O |
| 8.EC.20 | Arsenovanmeersscheite | U6+(UO2)3(AsO4)2(OH)6 · 4H2O |
| 8.EC.20 | Metavanmeersscheite | U6+(UO2)3(PO4)2(OH)6 · 2H2O |
| 8.EC.25 | Althupite | AlTh(UO2)7(PO4)4(OH)5O2 · 15H2O |
| 8.EC.30 | Mundite | Al(UO2)3(PO4)2(OH)3 · 5.5H2O |
| 8.EC.40 | Bergenite | Ca2Ba4(UO2)9(PO4)6O6 · 16H2O |
Radioactivity
| Element | % Content | Activity (Bq/kg) | Radiation Type |
|---|---|---|---|
| Uranium (U) | 57.6673% | 14,416,825 | 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
Fluorescence of Phurcalite
Other Information
Internet Links for Phurcalite
Please feel free to link to this page.
References for Phurcalite
Localities for Phurcalite
Showing 39 localities.
Locality List
- 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).
All localities listed without proper references should be considered as questionable.
Argentina | |
| O. Morello y C. N. Reyes Encinas (1990) |
| O. Morello y C. N. Reyes Encinas (1990) | |
| M. E. Saulnier y F. Greco (1988) | |
| Personally collected by Günter Frenz |
Australia | |
| Haupt (2003) |
| Elliott et al. (2019) |
| The mines & minerals of the Olary ... | |
Austria | |
| Brandstätter et al. (1987) +1 other reference |
Brazil | |
| D Atencio & R Hypolito () +1 other reference |
| Fosfatos e Silicatos Secundários de ... | |
Chile | |
| A.Molina & M. Dini collections - based ... |
| samples identified by Gerhard Möhn |
China | |
| Guang Fan et al. (2014) |
Czech Republic | |
| J. Plasil (SC-XRD) |
| Collected by Jan Hloušek +1 other reference |
DR Congo | |
| Deliens (1996) |
Egypt | |
| Ehab K. Abu Zeid (2020) |
| Ismail (2017) +1 other reference | |
France | |
| Chollet Pascal Collection - SEM-EDS ... |
| - (1998) |
Germany | |
| Steen et al. (2024) |
| Walenta (1994) +1 other reference |
| Habel et al. (1994) +1 other reference |
| https://www.mineralienatlas.de/?l=5281 |
| www.mineralienatlas.de (n.d.) |
| Deliens et al. (1978) |
| Witzke (2018) |
India | |
| Saini +3 other references |
| Singh et al. (1999) | |
Namibia | |
| Schnaitmann et al. (2009) |
Portugal | |
| Luis Casinhas collection |
| Cesar Menor Salvan |
UK | |
| Braithwaite et al. (1989) +1 other reference |
USA | |
| Braithwaite et al. (1989) |
| Pemberton (1983) +1 other reference |
| Excalibur Mineral Corp. - Mineral News |
| Caldwell (2018) |
| Min News 3:9 p5-6 |
Zambia | |
| Randabel et al. (2018) |





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Posey Mine, Red Canyon Mining District, San Juan County, Utah, USA