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Flinteite

A valid IMA mineral species
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About FlinteiteHide

09453480017272472464364.jpg
Evgeniy E. Flint
Formula:
K2ZnCl4
Colour:
Light green, light yellow to bright greenish-yellow , colourless
Lustre:
Vitreous
Hardness:
2
Specific Gravity:
2.49
Crystal System:
Orthorhombic
Name:
Named in honour of Evgeniy Evgenievich Flint (Евгений Евгеньевич Флинт) (7 September 1887, Moscow, Russian Empire – 10 November 1975, Moscow, USSR), crystallographer. He was a professor in the Department of Crystallography, Moscow State University, and later in the Department of Mineralogy and Crystallography MGRI and Institute of Crystallography, USSR Academy of Sciences. He did considerable reasearch on goniometric measurements of crystals.
The natural analogue of a well-known synthetic room-temperature modification of K2ZnCl4, a ferroelectric material.

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 IdentifiersHide

Mindat ID:
46109
Long-form identifier:
mindat:1:1:46109:4

IMA Classification of FlinteiteHide

Classification of FlinteiteHide

3.A0.

3 : HALIDES
A : Simple halides, without H2O
0 :

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference
FntIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of FlinteiteHide

Vitreous
Transparency:
Transparent
Colour:
Light green, light yellow to bright greenish-yellow , colourless
Hardness:
Tenacity:
Brittle
Cleavage:
Distinct/Good
One direction of distinct cleavage was observed
Density:
2.49 g/cm3 (Measured)    

Optical Data of FlinteiteHide

Type:
Biaxial (+)
RI values:
nα = 1.573(1) nβ = 1.574(1) nγ = 1.576(1)
2V:
Measured: 40°
Max. Birefringence:
δ = 0.003
Based on recorded range of RI values above.

Interference Colours:
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.

Surface Relief:
Moderate

Chemistry of FlinteiteHide

Mindat Formula:
K2ZnCl4
Element Weights:
Element% weight
Cl49.691 %
K27.400 %
Zn22.909 %

Calculated from ideal end-member formula.
Common Impurities:
Rb,Cs

Crystallography of FlinteiteHide

Crystal System:
Orthorhombic
Class (H-M):
mm2 - Pyramidal
Space Group:
Pna21
Setting:
Pna21
Cell Parameters:
a = 26.809(1) Å, b = 12.4085(6) Å, c = 7.2512(3) Å
Ratio:
a:b:c = 2.161 : 1 : 0.584
Unit Cell V:
2412.18 ų
Z:
12
Morphology:
Prismatic crystals. Granular aggregates or crusts.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0020735FlinteiteMikhail I, Peters K (1979) The structure of potassium tetrachlorozincate Acta Crystallographica B35 1200-12011979synthetic0293
0020736FlinteiteKusz J, Kucharczyk D (1994) The comparative study of the commensurate structure of K2ZnC14 Applied Crystallography: Proceedings of the XVI Conference 16 268-2721994synthetic0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45b : [Other oxidized fumarolic minerals]
Geological Setting:
Arsenatnaya and Glavnaya Tenoritovaya fumaroles, Second scoria cone

Type Occurrence of FlinteiteHide

General Appearance of Type Material:
Prismatic crystals up to 0.2 × 0.3 × 1.2 mm and granular aggregates or crusts up to 0.5 × 5 × 5 mm.
Place of Conservation of Type Material:
Type material is deposited in the collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia, registration number 4529/1
Geological Setting of Type Material:
In active fumaroles
Associated Minerals at Type Locality:

Synonyms of FlinteiteHide

Other Language Names for FlinteiteHide

Dutch:Flinteiet
German:Flinteit

Common AssociatesHide

Associated Minerals Based on Photo Data:
1 photo of Flinteite associated with HaliteNaCl

Related Minerals - Strunz-mindat GroupingHide

3.A0.MellizinkaliteK3Zn2Cl7Tric. 1 : P1
3.A0.OskarssoniteAlF3Trig. 3 : R3
3.A0.SanguiteKCuCl3Mon. 2/m : P21/b
3.A0.Waimirite-(Y)YF3Orth. mmm (2/m 2/m 2/m) : Pnma

RadioactivityHide

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.

Interactive Simulator:

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:

DistanceDose rateRisk
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 InformationHide

Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for FlinteiteHide

References for FlinteiteHide

Localities for FlinteiteHide

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.

Locality ListHide

- 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). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

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