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Demartinite

A valid IMA mineral species
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About DemartiniteHide

06386790017271949419440.jpg
Francesco Demartin
Formula:
K2[SiF6]
Colour:
Colorless
Specific Gravity:
2.85
Crystal System:
Hexagonal
Name:
After Francesco Demartin (born 1953), professor of General and Inorganic Chemistry and Stechiometry at the University of Milan, Italy. He has made significant contributions to the chemistry of metallic clusters in organometallic compounds and to the crystal structure of Alpine rare-earth minerals and uranium minerals.
Dimorph of:
This page provides mineralogical data about Demartinite.


Unique IdentifiersHide

Mindat ID:
30908
Long-form identifier:
mindat:1:1:30908:6

IMA Classification of DemartiniteHide

Approved
IMA Formula:
K2SiF6
Approval year:
2006
First published:
2007

Classification of DemartiniteHide

3.CH.20

3 : HALIDES
C : Complex halides
H : Silicofluorides
11.5.2.3

11 : HALIDE COMPLEXES
5 : AmBX6

Mineral SymbolsHide

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

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

Physical Properties of DemartiniteHide

Transparency:
Transparent
Colour:
Colorless
Streak:
White
Density:
2.85 g/cm3 (Measured)    2.87 g/cm3 (Calculated)

Optical Data of DemartiniteHide

Type:
Uniaxial (-)
RI values:
nω = 1.350(5) nε = 1.340(5)
Max. Birefringence:
δ = 0.010
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. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Moderate
Pleochroism:
Non-pleochroic

Chemistry of DemartiniteHide

Mindat Formula:
K2[SiF6]
Element Weights:
Element% weight
F51.750 %
K35.500 %
Si12.750 %

Calculated from ideal end-member formula.

Crystallography of DemartiniteHide

Crystal System:
Hexagonal
Class (H-M):
6mm - Dihexagonal Pyramidal
Space Group:
P63mc
Cell Parameters:
a = 5.6461(8) Å, c = 9.2322(18) Å
Ratio:
a:c = 1 : 1.635
Unit Cell V:
254.88 ų (Calculated from Unit Cell)
Z:
2
Morphology:
Hexagonal pyramidal crystals. The observed forms are the pedion {001} and the hexagonal pyramid {112}.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006157DemartiniteGramaccioli C M, Campostrini I (2007) Demartinite, a new polymorph of K2SiF6 from La Fossa Crater, Vulcano, Aeolian Islands, Italy The Canadian Mineralogist 45 1275-12802007La Fossa Crater, Vulcano Island, Aeolian Archipelago, Sicily, Italy0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
4.90 Å(25)
4.62 Å(75)
4.32 Å(43)
2.358 Å(22)
2.301 Å(100)
2.155 Å(54)
1.909 Å(14)
1.403 Å(13)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45b : [Other oxidized fumarolic minerals]

Type Occurrence of DemartiniteHide

General Appearance of Type Material:
Colorless hexagonal pyramidal crystals up to 0.3 mm across.
Place of Conservation of Type Material:
State University of Milan, Italy, number 2006-1.
Geological Setting of Type Material:
From a fumarole, on a fragment of altered pyroclastic breccia.
Associated Minerals at Type Locality:

Synonyms of DemartiniteHide

Other Language Names for DemartiniteHide

Common AssociatesHide

Associations Based on Photo Data:
3 photos of Demartinite associated with HieratiteK2[SiF6]
1 photo of Demartinite associated with KnasibfiteK3Na4[SiF6]3[BF4]
1 photo of Demartinite associated with Native SulphurS8

Related Minerals - Strunz-mindat GroupingHide

3.CH.05MalladriteNa2[SiF6]Trig. 32 : P321
3.CH.10Bararite(NH4)2[SiF6]Trig. 3m(32/m)
3.CH.15HieratiteK2[SiF6]Iso. m3m(4/m32/m) : Fm3m
3.CH.15Cryptohalite(NH4)2[SiF6]Iso. m3m(4/m32/m) : Fm3m
3.CH.25KnasibfiteK3Na4[SiF6]3[BF4]Orth. mm2 : Imm2
3.CH.30HeklaiteKNaSiF6Orth. mmm(2/m2/m2/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) 35.4999% 11,005 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

Notes:
Not hygroscopic.
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 DemartiniteHide

References for DemartiniteHide

Localities for DemartiniteHide

Showing 2 localities.

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.
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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.
Italy (TL)
 
  • Sicily
    • Metropolitan City of Messina
      • Eolie Islands (Aeolian Islands)
        • Lipari
          • Vulcano Island
Gramaccioli et al. (2007)
Russia
 
  • Kamchatka Krai
    • Milkovsky District
      • Tolbachik Volcanic field
        • Plosky Tolbachik Volcano
Zelenski et al. (2020)
 
and/or  
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