Flinteite
About Flinteite
The most simple natural K-Zn chloride, chemically related to cryobostryxite (hydrated) and mellizinkalite (anhydrous).
In the structure there are 3 Zn sites, with Zn-centered ZnCl4 tetrahedra, and 6 K sites.
Chemically identical phase was reported to crystallize from volcanic gas (Iodake crater, Satsuma-Ioujima volcano) in an experimental condensation in silica tubes, in the temperature range of 400-500oC (Africano et al., 2002).
Unique Identifiers
IMA Classification of Flinteite
Classification of Flinteite
3 : HALIDES
A : Simple halides, without H2O
0 :
Mineral Symbols
Symbol | Source | Reference |
---|---|---|
Fnt | 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 Flinteite
One direction of distinct cleavage was observed
Optical Data of Flinteite
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.
Chemistry of Flinteite
Crystallography of Flinteite
Crystal Structure
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0020735 | Flinteite | Mikhail I, Peters K (1979) The structure of potassium tetrachlorozincate Acta Crystallographica B35 1200-1201 | ![]() | 1979 | synthetic | 0 | 293 |
0020736 | Flinteite | Kusz J, Kucharczyk D (1994) The comparative study of the commensurate structure of K2ZnC14 Applied Crystallography: Proceedings of the XVI Conference 16 268-272 | 1994 | synthetic | 0 | 293 |
X-Ray Powder Diffraction
d-spacing | Intensity |
---|---|
6.229 Å | (27) |
5.123 Å | (88) |
3.629 Å | (98) |
3.599 Å | (100) |
3.133 Å | (35) |
3.039 Å | (26) |
2.897 Å | (35) |
2.688 Å | (46) |
Geological Environment
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Stage 7: Great Oxidation Event | <2.4 |
45b : [Other oxidized fumarolic minerals] |
Type Occurrence of Flinteite
Synonyms of Flinteite
Other Language Names for Flinteite
Common Associates
Related Minerals - Strunz-mindat Grouping
3.A0. | Mellizinkalite | K3Zn2Cl7 |
3.A0. | Oskarssonite | AlF3 |
3.A0. | Sanguite | KCuCl3 |
3.A0. | Waimirite-(Y) | YF3 |
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) | 27.4000% | 8,494 | 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 Flinteite
Please feel free to link to this page.
References for Flinteite
Localities for Flinteite
Locality List




All localities listed without proper references should be considered as questionable.
Russia | |
| Pekov et al. (2015) |
| Williams et al. (2014) +3 other references |
| Pekov et al. (2015) +1 other reference |
Pekov et al. (2015) |
First scoria cone, Northern Breakthrough, Great Fissure eruption, Tolbachik Volcanic field, Milkovsky District, Kamchatka Krai, Russia