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Sanguite

A valid IMA mineral species
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About SanguiteHide

Formula:
KCuCl3
Colour:
Bright red
Lustre:
Vitreous
Hardness:
3
Specific Gravity:
2.86
Crystal System:
Monoclinic
Name:
The mineral is named from the Latin sanguis (blood), alluding to its color.
(NH4)CdCl3 structure type.

The structure is based on almost planar and discrete [Cu2+2Cl6] dimers. There are also KCl9 polyhedra that share faces to form interrupted layers; the layers are linked to each other by the common edges of the K-bearing polyhedra.


Unique IdentifiersHide

Mindat ID:
43869
Long-form identifier:
mindat:1:1:43869:8

Similar NamesHide

PanguiteA valid IMA mineral species(Ti,Al,Sc,Mg,Zr,Ca)1.8O3
SanguineA variety of HematiteFe2O3

IMA Classification of SanguiteHide

Approved
IMA Formula:
KCu2+Cl3
Approval year:
2013
First published:
2015

Classification of SanguiteHide

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

Physical Properties of SanguiteHide

Vitreous
Transparency:
Transparent
Colour:
Bright red
Comment:
Slightly altered samples are dark red to brownish red.
Streak:
Reddish orange
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
Perfect on (010); another distinct cleavage observed under the microscope is probably on (102), based on angles measured on cleaved
pieces and by analogy with the synthetic crystals.
Fracture:
Step-Like
Density:
2.86(1) g/cm3 (Measured)    2.88 g/cm3 (Calculated)

Optical Data of SanguiteHide

Type:
Biaxial (-)
RI values:
nα = 1.653(3) nβ = 1.780(6) nγ = 1.900(8)
2V:
Measured: 85° (5), Calculated: 82°
Max. Birefringence:
δ = 0.247
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
Dispersion:
Very strong, r > v
Optical Extinction:
Y = b; Z ∧ a = 48°.
Pleochroism:
Strong
Comments:
X = yellowish grey to colorless; Y = grey to pinkish grey; Z = brownish red.
Comments:
Absorption: Z > Y > X.

Chemistry of SanguiteHide

Mindat Formula:
KCuCl3
Element Weights:
Element% weight
Cl50.889 %
Cu30.404 %
K18.707 %

Calculated from ideal end-member formula.

Crystallography of SanguiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/b
Setting:
P21/c
Cell Parameters:
a = 4.0281(2) Å, b = 13.7906(5) Å, c = 8.7335(4) Å
γ = 97.137(4)°
Ratio:
a:b:c = 0.292 : 1 : 0.633
Unit Cell V:
481.38 ų
Z:
4
Morphology:
Prismatic crystals up to 1 mm long and up to 0.2 mm thick, groups, crusts. Crystal forms are {011}, {100}, and {010}.
Twinning:
Areas with polysynthetic twinning have been observed in some crystals under the microscope. On the section coplanar to (010); the twin lamellae are wedge-shaped and elongated along [100].

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0019972SanguiteWillett R D, Dwiggins C, Kruth R F, Rundle R E (1963) Crystal strucutres of KCuCl3 and NH4CuCl3 Journal of Chemical Physics 38 2429-24361963synthetic0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
7.36 Å(78)
6.92 Å(100)
3.684 Å(69)
3.146 Å(64)
3.068 Å(63)
2.857 Å(73)
2.709 Å(82)
2.574 Å(56)
Comments:
From Type Description.

Geological EnvironmentHide

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

Type Occurrence of SanguiteHide

General Appearance of Type Material:
Prismatic crystals up to 1 mm long and up to 0.2 mm thick, typically combined in groups, dense clusters, or crusts up to several dozens of cm2 in area.
Place of Conservation of Type Material:
Type material is deposited in the collections of the collections of the Fersman Mineralogical Museum of the Russian Academy of Sciences, Moscow, Russia, registration number 4363/1.
Geological Setting of Type Material:
Volcanic fumarole.
Associated Minerals at Type Locality:

Synonyms of SanguiteHide

Other Language Names for SanguiteHide

Dutch:Sanguiet
German:Sanguit

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Sanguite associated with RomanorloviteK8Cu6Cl17(OH)3

Related Minerals - Strunz-mindat GroupingHide

3.A0.FlinteiteK2ZnCl4Orth. mm2 : Pna21
3.A0.MellizinkaliteK3Zn2Cl7Tric. 1 : P1
3.A0.OskarssoniteAlF3Trig. 3 : R3
3.A0.Waimirite-(Y)YF3Orth. 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) 18.7070% 5,799 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 SanguiteHide

References for SanguiteHide

Localities for SanguiteHide

Showing 1 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.
Russia (TL)
 
  • Kamchatka Krai
    • Milkovsky District
      • Tolbachik Volcanic field
        • Great Fissure eruption (Main Fracture)
          • Northern Breakthrough (North Breach)
            • Second scoria cone
Pekov et al. (2015)
 
and/or  
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