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Kapellasite

A valid IMA mineral species
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About KapellasiteHide

Formula:
Cu3Zn(OH)6Cl2
Colour:
Green-blue
Lustre:
Adamantine
Hardness:
4
Specific Gravity:
3.55
Crystal System:
Trigonal
Member of:
Name:
Named after Christo Kapellas (1938-2004), collector and mineral dealer of Kamariza, Lavrion, Greece. He was one of the foremost experts on the Lavrion minerals.
Dimorph of:
Isostructural with:
A metastable polymorph of herbertsmithite. Has been confused with botallackite ("Zn-bearing botallackite"; Wendel et al., 1999); both are visually very similar.
Also known as a synthetic compound (phase IIα of Feitknecht and Maget, 1949).

The Mg analogue of kapellasite is called haydeeite.



Unique IdentifiersHide

Mindat ID:
27446
Long-form identifier:
mindat:1:1:27446:1

IMA Classification of KapellasiteHide

Classification of KapellasiteHide

3.DA.10c

3 : HALIDES
D : Oxyhalides, hydroxyhalides and related double halides
A : With Cu, etc., without Pb

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

Physical Properties of KapellasiteHide

Adamantine
Transparency:
Transparent
Colour:
Green-blue
Streak:
Light green-blue
Hardness:
Hardness:
VHN25=200(30) kg/mm2 - Vickers
Tenacity:
Brittle
Cleavage:
Distinct/Good
Parallel to {0001}
Fracture:
Irregular/Uneven
Density:
3.55(10) g/cm3 (Measured)    3.62 g/cm3 (Calculated)
Comment:
Measured by flotation in Clerici solution. Calculated from the empirical formula.

Optical Data of KapellasiteHide

Type:
Uniaxial (-)
RI values:
nω = 1.80(1) nε = 1.76(1)
Max. Birefringence:
δ = 0.040
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:
Strong
Comments:
E = pale green and O = green-blue.
Comments:
Some crystals show biaxial behavior with 2V up to 20 degrees.

Chemistry of KapellasiteHide

Mindat Formula:
Cu3Zn(OH)6Cl2
Element Weights:
Element% weight
Cu44.441 %
O22.379 %
Cl16.529 %
Zn15.241 %
H1.410 %

Calculated from ideal end-member formula.

Crystallography of KapellasiteHide

Crystal System:
Trigonal
Class (H-M):
3m(32/m) - Hexagonal Scalenohedral
Space Group:
P3m1
Cell Parameters:
a = 6.300 Å, c = 5.733 Å
Ratio:
a:c = 1 : 0.91
Unit Cell V:
197.06 ų
Z:
1
Morphology:
Most crystals exhibit a bladed or needle-like irregular habit and are typically strongly distorted with elongation perpendicular to [0001]. Crystallographic forms are {0001} and {1010}.
Twinning:
None observed

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0014577KapellasiteKrause W, Bernhardt H J, Braithwaite R S W, Kolitsch U, Pritchard R (2006) Kapellasite, Cu3Zn(OH)6Cl2, a new mineral from Lavrion, Greece, and its crystal structure Mineralogical Magazine 70 329-3402006Lavrion, Greece0293
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
47a : [Near-surface hydration of prior minerals]
47g : [Halogen-bearing surface weathering minerals]

Type Occurrence of KapellasiteHide

General Appearance of Type Material:
Crusts and small aggregates up to 0.5 mm, composed of bladed or needle-like indistinct crystals up to 0.2 mm long.
Place of Conservation of Type Material:
Mineralogical Institute, University of Bochum, Germany, catalogue number IMA-2005-009.
Geological Setting of Type Material:
Formed underground in a mine, from weathering of copper- and zinc-containing ore, in the presence of chloride ions.
Associated Minerals at Type Locality:

Synonyms of KapellasiteHide

Other Language Names for KapellasiteHide

Relationship of Kapellasite to other SpeciesHide

Member of:
Other Members of Atacamite Group:
AtacamiteCu2(OH)3ClOrth. mmm(2/m2/m2/m) : Pnma
BotallackiteCu2(OH)3ClMon. 2/m : P21/m
ClinoatacamiteCu2(OH)3ClMon. 2/m
GillarditeCu3Ni(OH)6Cl2Trig. 3m(32/m) : R3m
HaydeeiteCu3Mg(OH)6Cl2Trig. 3m(32/m) : P3m1
HerbertsmithiteCu3Zn(OH)6Cl2Trig. 3m(32/m) : R3m
HibbingiteFe2+2(OH)3ClOrth. mmm(2/m2/m2/m) : Pnma
IyoiteMnCuCl(OH)3Mon. 2/m : P21/m
KempiteMn2+2(OH)3ClOrth. mmm(2/m2/m2/m) : Pnma
KuliginiteFe3Mg(OH)6Cl2Trig. 3 : R3
LeverettiteCu3Co(OH)6Cl2Trig. 3 : R3
MisakiiteCu3Mn(OH)6Cl2Trig. 3m(32/m) : P3m1
ParatacamiteCu3(Cu,Zn)(OH)6Cl2Trig. 3 : R3
Paratacamite-(Mg)Cu3(Mg,Cu)(OH)6Cl2Trig. 3 : R3
Paratacamite-(Ni)Cu3(Ni,Cu)(OH)6Cl2Trig. 3 : R3
TondiiteCu3Mg(OH)6Cl2Trig. 3m(32/m) : R3m
'Unnamed (Cu-Zn Chloride Hydroxide)'CuZnCl(OH)3Mon. 2/m : P21/m

Common AssociatesHide

Associations Based on Photo Data:
14 photos of Kapellasite associated with GypsumCaSO4 · 2H2O
10 photos of Kapellasite associated with HemimorphiteZn4Si2O7(OH)2 · H2O
4 photos of Kapellasite associated with CumengeitePb21Cu20Cl42(OH)40 · 6H2O
3 photos of Kapellasite associated with ParatacamiteCu3(Cu,Zn)(OH)6Cl2
2 photos of Kapellasite associated with LaurionitePbCl(OH)
2 photos of Kapellasite associated with WoodruffiteZn2+x/2(Mn4+1-xMn3+x)O2 · yH2O
1 photo of Kapellasite associated with GordaiteNaZn4(SO4)(OH)6Cl · 6H2O
1 photo of Kapellasite associated with 'Unnamed (Gordaite-related Ca-Zn Sulphate Chloride Hydrate)'Ca[Zn8(SO4)2(OH)12Cl2](H2O)9
1 photo of Kapellasite associated with PseudoboleitePb31Cu24Cl62(OH)48
1 photo of Kapellasite associated with HydrozinciteZn5(CO3)2(OH)6

Related Minerals - Strunz-mindat GroupingHide

3.DA.ParahibbingiteFe2(OH)3ClTrig. 3m(32/m) : R3m
3.DA.CentennialiteCaCu3Cl2(OH)6 · nH2O (n ~ 0.7)Trig. 3m(32/m) : P3m1
3.DA.BounahasiteCu+Cu2+2(OH)3Cl2Mon. 2/m
3.DA.MuonionalustaiteNi3(OH)4Cl2 · 4H2OMon. 2/m : B2/m
3.DA.05MelanothalliteCu2Cl2OOrth. mmm(2/m2/m2/m) : Fddd
3.DA.10cHaydeeiteCu3Mg(OH)6Cl2Trig. 3m(32/m) : P3m1
3.DA.10bClinoatacamiteCu2(OH)3ClMon. 2/m
3.DA.10cParatacamiteCu3(Cu,Zn)(OH)6Cl2Trig. 3 : R3
3.DA.10cLeverettiteCu3Co(OH)6Cl2Trig. 3 : R3
3.DA.10aHibbingiteFe2+2(OH)3ClOrth. mmm(2/m2/m2/m) : Pnma
3.DA.10cParatacamite-(Ni)Cu3(Ni,Cu)(OH)6Cl2Trig. 3 : R3
3.DA.10aKempiteMn2+2(OH)3ClOrth. mmm(2/m2/m2/m) : Pnma
3.DA.10cTondiiteCu3Mg(OH)6Cl2Trig. 3m(32/m) : R3m
3.DA.10aAtacamiteCu2(OH)3ClOrth. mmm(2/m2/m2/m) : Pnma
3.DA.10bBelloiteCu(OH)ClMon. 2/m : P21/b
3.DA.10cMisakiiteCu3Mn(OH)6Cl2Trig. 3m(32/m) : P3m1
3.DA.10bIyoiteMnCuCl(OH)3Mon. 2/m : P21/m
3.DA.10cKuliginiteFe3Mg(OH)6Cl2Trig. 3 : R3
3.DA.10cGillarditeCu3Ni(OH)6Cl2Trig. 3m(32/m) : R3m
3.DA.10b'Unnamed (Cu-Zn Chloride Hydroxide)'CuZnCl(OH)3Mon. 2/m : P21/m
3.DA.10bBotallackiteCu2(OH)3ClMon. 2/m : P21/m
3.DA.10cHerbertsmithiteCu3Zn(OH)6Cl2Trig. 3m(32/m) : R3m
3.DA.15ClaringbulliteCu4ClF(OH)6Hex. 6/mmm(6/m2/m2/m) : P63/mmc
3.DA.15BarlowiteCu4BrF(OH)6Hex. 6/mmm(6/m2/m2/m) : P63/mmc
3.DA.20SimonkolleiteZn5Cl2(OH)8 · H2OTrig. 3m(32/m) : P3m1
3.DA.25ButtgenbachiteCu19(NO3)2(OH)32Cl4 · 2H2OHex. 6/mmm(6/m2/m2/m) : P63/mmc
3.DA.25ConnelliteCu19(SO4)(OH)32Cl4 · 3H2OHex. 6m2 : P62c
3.DA.30AbhuriteSn21Cl16(OH)14O6Trig. 32 : R32
3.DA.35PonomareviteK4Cu4Cl10OMon. 2/m : B2/b
3.DA.40CalumetiteCaCu4(OH)8Cl2 · 3.5H2OOrth. mmm(2/m2/m2/m) : Cmcm
3.DA.40AnthonyiteCu(OH,Cl)2 · 3H2OMon. 2/m
3.DA.45KhaidarkaniteCu4Al3(OH)14F3 · 2H2OMon. 2/m : B2/m
3.DA.50BobkingiteCu5Cl2(OH)8 · 2H2OMon. 2/m : B2/m
3.DA.55AvdoniniteK2Cu5(OH)4Cl8 · H2OMon. 2/m : P21/b
3.DA.60DroninoiteNi6Fe3+2(OH)16Cl2 · 4H2OTrig. 3m(32/m) : R3m
3.DA.70ChrysothalliteK6Cu6Tl3+Cl17(OH)4 · H2OTet. 4/mmm(4/m2/m2/m) : I4/mmm
3.DA.70DioskouriiteCaCu4Cl6(OH)4 · 4H2OMon. 2/m : P21/b
3.DA.75FeodosiyiteCu11Mg2Cl18(OH)8 · 16H2OMon. 2/m : P21/b
3.DA.80RomanorloviteK8Cu6Cl17(OH)3Tet. 4/mmm(4/m2/m2/m) : I4/mmm

Fluorescence of KapellasiteHide

Not fluorescent in LW or SW UV.

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 KapellasiteHide

References for KapellasiteHide

Localities for KapellasiteHide

Showing 6 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.
France
 
  • Provence-Alpes-Côte d'Azur
    • Var
      • Toulon
        • Le Pradet
Favreau et al. (2024)
Favreau (n.d.) +2 other references
Germany
 
  • Lower Saxony
    • Goslar District
      • Langelsheim
        • Astfeld
Krause et al. (2006)
Greece (TL)
 
  • Attica
    • East Attica
      • Lavreotiki
        • Sounion
          • Cato Sounio mines
Krause et al. (2006)
Italy
 
  • Sardinia
    • South Sardinia Province
      • Nuxis
        • Monte Tamara mining area
Lecca et al. (2022)
Spain
 
  • Andalusia
    • Almería
      • Pechina
        • Baños de Alhamilla
Rewitzer et al. (2020)
 
and/or  
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