Kupletskite
About Kupletskite
Unique Identifiers
Similar Names
| Kupletskite-(Cs) | A valid IMA mineral species | Cs2NaMn72+Ti2[Si4O12]2O2(OH)4F |
IMA Classification of Kupletskite
Classification of Kupletskite
9 : SILICATES (Germanates)
D : Inosilicates
C : Inosilicates with branched 2-periodic single chains; Si2O6 + 2SiO3 Si4O12
69 : INOSILICATES Chains with Side Branches or Loops
1 : Chains with Side Branches or Loops with (P=2, and N=4, 2 branches)
14 : Silicates not Containing Aluminum
9 : Silicates of Ti
Mineral Symbols
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Kpt | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
| Kpt | 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 Kupletskite
on [100]
Optical Data of Kupletskite
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.
Chemistry of Kupletskite
Chemical Analysis
| 1 | |
|---|---|
| Na2O | 3.52 % |
| K2O | 5.69 % |
| Rb2O | 0.37 % |
| Cs2O | 0.03 % |
| CaO | 0.41 % |
| SrO | 0.07 % |
| MgO | 0.36 % |
| MnO | 17.63 % |
| FeO | 16.01 % |
| ZnO | 0.47 % |
| Ce2O3 | 0.23 % |
| TiO2 | 9.74 % |
| ZrO2 | 1.07 % |
| Nb2O5 | 2.27 % |
| Ta2O5 | 0.09 % |
| SiO2 | 34.92 % |
| Al2O3 | 0.10 % |
| F | 1.65 % |
| H2O | 2.52 % |
| O=F | -0.69 % |
| Total: | 96.46 % |
| ID | Locality | Reference | Notes |
|---|---|---|---|
| 1 | Gjerdingselva, Lunner, Akershus, Norway |
Crystallography of Kupletskite
α = 113.066°, β = 94.702°, γ = 103.086°
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) |
|---|---|---|---|---|---|---|---|
| 0005820 | Kupletskite | 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 | altered nepheline syenite pegmatite at Mont Saint-Hilaire, Quebec, Canada | 0 | 293 |
| 0005817 | Kupletskite | 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 |
| 0005816 | Kupletskite | 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 |
| 0005815 | Kupletskite | 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 |
| 0005814 | Kupletskite | 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 |
| 0005813 | Kupletskite | 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 |
| 0005812 | Kupletskite | 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 |
| 0005811 | Kupletskite | 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 |
| 0005810 | Kupletskite | 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 |
| 0005808 | Kupletskite | 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 | Lovozero massif, Kola Peninsula, Russia | 0 | 293 |
| 0005807 | Kupletskite | 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 | Lovozero massif, Kola Peninsula, Russia | 0 | 293 |
| 0005804 | Kupletskite | 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 | Gjerdingen intrusion, Norway | 0 | 293 |
| 0006908 | Kupletskite | Piilonen P C, McDonald A M, LaLonde A E (2001) Kupletskite polytypes from the Lovozero massif, Kola Peninsula, Russia: Kupletskite-1A and kupletskite-Ma2b2c European Journal of Mineralogy 13 973-984 | 2001 | Lovozero massif, Kola Peninsula, Russia | 0 | 293 | |
| 0006907 | Kupletskite | Piilonen P C, McDonald A M, LaLonde A E (2001) Kupletskite polytypes from the Lovozero massif, Kola Peninsula, Russia: Kupletskite-1A and kupletskite-Ma2b2c European Journal of Mineralogy 13 973-984 | 2001 | Lovozero massif, Kola Peninsula, Russia | 0 | 293 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 3.505 Å | (8) |
| 2.642 Å | (8) |
| 2.573 Å | (4) |
| 2.099 Å | (3) |
| 1.732 Å | (3) |
| 3.249 Å | (1) |
| 2.998 Å | (1) |
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 Kupletskite
Other Language Names for Kupletskite
Varieties of Kupletskite
Relationship of Kupletskite to other Species
| Heyerdahlite | Na2NaMn2+7Ti2[Si4O12]2O2(OH)4F(H2O)2 | Tric. 1 : P1 |
| Kupletskite-(Cs) | Cs2NaMn2+7Ti2[Si4O12]2O2(OH)4F | Tric. 1 : P1 |
| Laverovite | K2NaMn2+7Zr2[Si4O12]2O2(OH)4F | Tric. 1 : P1 |
| Niobokupletskite | K2NaMn2+7(NbTi)[Si4O12]2O2(OH)4O | Tric. 1 : P1 |
Common Associates
| 56 photos of Kupletskite associated with Aegirine | NaFe3+Si2O6 |
| 27 photos of Kupletskite associated with Analcime | Na(AlSi2O6) · H2O |
| 16 photos of Kupletskite associated with Microcline | K(AlSi3O8) |
| 15 photos of Kupletskite associated with Natrolite | Na2Al2Si3O10 · 2H2O |
| 14 photos of Kupletskite associated with Catapleiite | Na2Zr(Si3O9) · 2H2O |
| 11 photos of Kupletskite associated with Albite | Na(AlSi3O8) |
| 10 photos of Kupletskite associated with Pectolite | NaCa2Si3O8(OH) |
| 10 photos of Kupletskite associated with Genthelvite | Be3Zn4(SiO4)3S |
| 10 photos of Kupletskite associated with Serandite | NaMn2+2Si3O8(OH) |
| 9 photos of Kupletskite associated with Monazite-(Ce) | Ce(PO4) |
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 | Niobokupletskite | K2NaMn2+7(NbTi)[Si4O12]2O2(OH)4O |
| 9.DC.05 | Kupletskite-(Cs) | Cs2NaMn2+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) | 5.9729% | 1,852 | 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
globule.
Internet Links for Kupletskite
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References for Kupletskite
Localities for Kupletskite
Showing 45 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.






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