Niobokupletskite
About Niobokupletskite
Unique Identifiers
IMA Classification of Niobokupletskite
Classification of Niobokupletskite
9 : SILICATES (Germanates)
D : Inosilicates
C : Inosilicates with branched 2-periodic single chains; Si2O6 + 2SiO3 Si4O12
Mineral Symbols
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Nbk | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
| Nbk | Warr (2020) | Warr, L.N. (2020) Recommended abbreviations for the names of clay minerals and associated phases. Clay Minerals, 55, 261–264 doi:10.1180/clm.2020.30 |
Physical Properties of Niobokupletskite
Perfect {001}
Optical Data of Niobokupletskite
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.
No measured or calculated 2V is on file for this mineral, so the value used here (87°) is estimated from its recorded refractive indices and optic sign, not from a direct 2V measurement.
Chemistry of Niobokupletskite
Crystallography of Niobokupletskite
α = 112.927°, β = 94.750°, γ = 103.175°
Type-I = anhedral to subhedral, platy to tabular, light beige to yellow epitaxic overgrowths on primary, dark brown kupletskite.
Type-II = as a dense, fibrous, light yellow-brown overgrowth on coarse-grained primary kupletskite.
Type-III = as an overgrowth on primary kupletskite as very fine-grained bronze to silvery brown acicular crystals in sheaf-like aggregates, originally described as “witch’s broom astrophyllite”.
Crystal Structure
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Big Balls | Small Balls | Just Balls | Spacefill
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| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0005821 | Niobokupletskite | Piilonen P C, McDonald A M, Lalonde A E (2003) Insights into astrophyllite-group minerals II: Crystal chemistry The Canadian Mineralogist 41 27-54 | ![]() | 2003 | nepheline syenite pegmatite at Mont Saint-Hilaire, Quebec, Canada | 0 | 293 |
| 0005648 | Niobokupletskite | Piilonen P C, Lalonde A E, McDonald A M, Gault R A (2000) Niobokupletskite, a new astrophyllite-group mineral from Mont Saint-Hilaire, Quebec, Canada: Description and crystal structure The Canadian Mineralogist 38 627-639 | ![]() | 2000 | Mont Saint-Hilaire, Quebec, Canada | 0 | 293 |
Epitaxial Relationships of Niobokupletskite
| 'Kupletskite' | K2NaMn2+7Ti2[Si4O12]2O2(OH)4F |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 10.707 Å | (100) |
| 4.405 Å | (20) |
| 3.536 Å | (50) |
| 3.294 Å | (20) |
| 2.793 Å | (40) |
| 2.677 Å | (30) |
| 2.587 Å | (40) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 4b: Highly evolved igneous rocks | >3.0 |
| 35 : Ultra-alkali and agpaitic igneous rocks |
Type Occurrence of Niobokupletskite
Synonyms of Niobokupletskite
Other Language Names for Niobokupletskite
Relationship of Niobokupletskite to other Species
| Heyerdahlite | Na2NaMn2+7Ti2[Si4O12]2O2(OH)4F(H2O)2 | Tric. 1 : P1 |
| Kupletskite | K2NaMn2+7Ti2[Si4O12]2O2(OH)4F | Tric. 1 : P1 |
| Kupletskite-(Cs) | Cs2NaMn2+7Ti2[Si4O12]2O2(OH)4F | Tric. 1 : P1 |
| Laverovite | K2NaMn2+7Zr2[Si4O12]2O2(OH)4F | Tric. 1 : P1 |
Common Associates
| 13 photos of Niobokupletskite associated with Franconite | Na(Nb2O5)(OH) · 3H2O |
| 13 photos of Niobokupletskite associated with Aegirine | NaFe3+Si2O6 |
| 9 photos of Niobokupletskite associated with Albite | Na(AlSi3O8) |
| 6 photos of Niobokupletskite associated with Kupletskite | K2NaMn2+7Ti2[Si4O12]2O2(OH)4F |
| 3 photos of Niobokupletskite associated with Nepheline | Na3K(Al4Si4O16) |
| 2 photos of Niobokupletskite associated with Adamsite-(Y) | NaY[CO3]2 · 6H2O |
| 2 photos of Niobokupletskite associated with Astrophyllite Supergroup | A2pBrC7D2(T4O12)2Xod2XoA4XpdnWa2 |
| 2 photos of Niobokupletskite associated with Wurtzite | (Zn,Fe)S |
| 1 photo of Niobokupletskite associated with Thomasclarkite-(Y) | (Na,Ce)(Y,REE)(HCO3)(OH)3 · 4H2O |
| 1 photo of Niobokupletskite associated with Catapleiite | Na2Zr(Si3O9) · 2H2O |
Related Minerals - Strunz-mindat Grouping
| 9.DC. | Bulgakite | Li2CaFe2+7Ti2[Si4O12]2O2(OH)4O(H2O)2 |
| 9.DC.05 | Devitoite | Ba4Ba2Fe2+7Fe3+2[Si4O12]2[PO4]2[CO3]O2(OH)4◻2 |
| 9.DC.05 | Zircophyllite | K2NaFe2+7Zr2[Si4O12]2O2(OH)4F |
| 9.DC.05 | Nalivkinite | Li2NaFe2+7Ti2[Si4O12]2O2(OH)4F(H2O)2 |
| 9.DC.05 | Sveinbergeite | (H2O)2[Ca(H2O)](Fe2+6Fe3+)Ti2[Si4O12]2O2(OH)4[(OH)(H2O)] |
| 9.DC.05 | Niobophyllite | K2NaFe2+7(NbTi)[Si4O12]2O2(OH)4O |
| 9.DC.05 | Heyerdahlite | Na2NaMn2+7Ti2[Si4O12]2O2(OH)4F(H2O)2 |
| 9.DC.05 | Tarbagataite | (K◻)CaFe2+7Ti2[Si4O12]2O2(OH)4(OH) |
| 9.DC.05 | Astrophyllite | K2NaFe2+7Ti2[Si4O12]2O2(OH)4F |
| 9.DC.05 | 'Hydroastrophyllite' | [H3O]+2CaFe2+7Ti2[Si4O12]2O2(OH)4O |
| 9.DC.05 | Lobanovite | K2Na(Fe2+4Mg2Na)Ti2[Si4O12]2O2(OH)4◻ |
| 9.DC.05 | Kupletskite-(Cs) | Cs2NaMn2+7Ti2[Si4O12]2O2(OH)4F |
| 9.DC.05 | Kupletskite | K2NaMn2+7Ti2[Si4O12]2O2(OH)4F |
| 9.DC.05 | Laverovite | K2NaMn2+7Zr2[Si4O12]2O2(OH)4F |
Radioactivity
| Element | % Content | Activity (Bq/kg) | Radiation Type |
|---|---|---|---|
| Uranium (U) | 0.0000% | 0 | α, β, γ |
| Thorium (Th) | 0.0000% | 0 | α, β, γ |
| Potassium (K) | 5.7871% | 1,794 | 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
Internet Links for Niobokupletskite
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References for Niobokupletskite
Localities for Niobokupletskite
Showing 2 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.
Canada (TL) | |
| Piilonen et al. (2000) +1 other reference |
India | |
| Chakrabarty et al. (2018) |





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The
Poudrette quarry, Mont Saint-Hilaire, La Vallée-du-Richelieu RCM, Montérégie, Québec, Canada