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Sabelliite

A valid IMA mineral species
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About SabelliiteHide

Formula:
(Cu,Zn)2Zn(AsO4,SbO4)(OH)3
Type material formula:
Cu2.19Zn0.96(As0.80Sb0.16Si0.05)Σ=1.01O4.31(OH)2.69.
Formula of Spanish material (Vrtiška et al., 2017): (Cu1.83Zn0.14Ni0.03)Σ2.00Zn1.00[(As
O4)0.72(SbO4)0.19(SiO4)0.05(PO4)0.01]Σ0.97(OH)3.15.
Colour:
Emerald-green, grass-green
Lustre:
Adamantine
Hardness:
Specific Gravity:
4.65 (Calculated)
Crystal System:
Trigonal
Name:
To honor Dr. Cesare Sabelli (b. 1934), Consiglio Nazionale della Ricerche, Florence, Italy, who has worked with the copper-bearing alteration minerals of Sardinia, Italy.
The reported crystal structure (Olmi et al., 1995b) and the presence of "SbO4" groups appear questionable (U. Kolitsch, unpublished results; see also U. Kolitsch, P. G. Slade, E. R. T. Tiekink and A. Pring (1999): The structure of antimonian dussertite and the role of antimony in oxysalt minerals. Mineral. Mag. 63, 17-26.).

Chemically similar to theisite.


Unique IdentifiersHide

Mindat ID:
3493
Long-form identifier:
mindat:1:1:3493:3

Similar NamesHide

IMA Classification of SabelliiteHide

Approved
IMA Formula:
Cu2+2Zn2+As5+O4(OH)3
Approval year:
1994
First published:
1995

Classification of SabelliiteHide

8.BE.65

8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
E : With only medium-sized cations, (OH, etc.):RO4 > 2:1

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

Physical Properties of SabelliiteHide

Adamantine
Transparency:
Transparent
Colour:
Emerald-green, grass-green
Streak:
Light green
Hardness:
4½ on Mohs scale
Hardness:
VHN15=322 - 469 kg/mm2 - Vickers
Tenacity:
Brittle
Cleavage:
None Observed
Density:
4.65 g/cm3 (Calculated)
Comment:
Could not be measured due to lack of material.

Optical Data of SabelliiteHide

Type:
Uniaxial (-)
RI values:
nω = 1.802 nε = 1.797
Max. Birefringence:
δ = 0.005
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:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized uniaxial interference figure - the conoscopic (convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis centred and vertical. The coloured rings are isochromatics, computed with the same physics as the Michel-Lévy bar above; the dark cross is the isogyre.

For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.

Chemistry of SabelliiteHide

Mindat Formula:
(Cu,Zn)2Zn(AsO4,SbO4)(OH)3

Type material formula:
Cu2.19Zn0.96(As0.80Sb0.16Si0.05)Σ=1.01O4.31(OH)2.69.
Formula of Spanish material (Vrtiška et al., 2017): (Cu1.83Zn0.14Ni0.03)Σ2.00Zn1.00[(As
O4)0.72(SbO4)0.19(SiO4)0.05(PO4)0.01]Σ0.97(OH)3.15.
Element Weights:
Element% weight
Cu33.234 %
O29.287 %
As19.592 %
Zn17.097 %
H0.791 %

Calculated from ideal end-member formula.

Crystallography of SabelliiteHide

Crystal System:
Trigonal
Class (H-M):
3 - Rhombohedral
Space Group:
P3
Cell Parameters:
a = 8.197(2) Å, c = 7.312(1) Å
Ratio:
a:c = 1 : 0.892
Unit Cell V:
425.48 ų (Calculated from Unit Cell)
Z:
3
Morphology:
Tabular on {001}, with a characteristic coin-like circular outline.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006608SabelliiteOlmi F, Sabelli C, Trosti-Ferroni R (1995) The crystal structure of sabelliite European Journal of Mineralogy 7 1331-133719950293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
2.522 Å(100)
1.550 Å(100)
1.805 Å(92)
2.166 Å(88)
1.513 Å(85)
4.11 Å(55)
3.66 Å(52)

Geological EnvironmentHide

Paragenetic Mode(s):

Type Occurrence of SabelliiteHide

General Appearance of Type Material:
Green crystals that are both tabular {001} and cylindrical; resembling small coins. The diameter of intergrown crystals rarely exceeds 400 µm; isolated single crystals are up to 200 µm in diameter and 15 µm in thickness. It is often overgrown on foliated aggregates of theisite, and is probably the last mineral to form.
Place of Conservation of Type Material:
Museum of Natural History, University of Florence, Florence, Italy, 2053/RI.
Geological Setting of Type Material:
Hydrothermal vein-like bodies of fluorite, sulphides, and sulphosalts.
Associated Minerals at Type Locality:

Synonyms of SabelliiteHide

Other Language Names for SabelliiteHide

Common AssociatesHide

Associations Based on Photo Data:
6 photos of Sabelliite associated with AzuriteCu3(CO3)2(OH)2
2 photos of Sabelliite associated with TheisiteCu5Zn5(AsO4,SbO4)2(OH)14
2 photos of Sabelliite associated with ZálesíiteCaCu6(AsO4)2(AsO3OH)(OH)6 · 3H2O
1 photo of Sabelliite associated with ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
1 photo of Sabelliite associated with FluoriteCaF2
1 photo of Sabelliite associated with QuartzSiO2
1 photo of Sabelliite associated with ConichalciteCaCu(AsO4)(OH)
1 photo of Sabelliite associated with Allanite-(Ce)(CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH)

Related Minerals - Strunz-mindat GroupingHide

8.BE.05AugeliteAl2(PO4)(OH)3Mon. 2/m : B2/m
8.BE.10GrattarolaiteFe3+3(PO4)O3Trig. 3m : R3m
8.BE.15CornetiteCu3(PO4)(OH)3Orth. mmm(2/m2/m2/m) : Pbca
8.BE.20ClinoclaseCu3(AsO4)(OH)3Mon. 2/m : P21/b
8.BE.25GilmariteCu3(AsO4)(OH)3Tric. 1 : P1
8.BE.25ArhbariteCu2Mg(AsO4)(OH)3Tric. 1 : P1
8.BE.30FlinkiteMn2+2Mn3+(AsO4)(OH)4Orth. mmm(2/m2/m2/m) : Pnma
8.BE.30ArganditeMn7(VO4)2(OH)8Mon. 2/m : P21/m
8.BE.30RaadeiteMg7(PO4)2(OH)8Mon. 2/m
8.BE.30AllactiteMn2+7(AsO4)2(OH)8Mon. 2/m : P21/b
8.BE.35'Mineral E (of Dunn, et. al., 1982)'Orth. mmm(2/m2/m2/m)
8.BE.35Chlorophoenicite(Mn,Mg)3Zn2(AsO4)(OH,O)6Mon. 2/m : B2/m
8.BE.35Magnesiochlorophoenicite(Mg,Mn)3Zn2(AsO4)(OH,O)6Mon. 2/m : B2/m
8.BE.40Gerdtremmelite(Zn,Fe)(Al,Fe)2(AsO4)(OH)5Tric.
8.BE.45DixeniteCuMn2+14Fe2+(SiO4)2(As5+O4)(As3+O3)5(OH)6Trig. 3 : R3
8.BE.45McgoverniteMn19Zn3(AsO4)3(AsO3)(SiO4)3(OH)21Trig. 3m : R3c
8.BE.45Hematolite(Mn,Mg,Al,Fe3+)15(As5+O4)2(As3+O3)(OH)23Trig. 3 : R3
8.BE.45Turtmannite(Mn,Mg)22.5Mg3-3x((V5+,As5+)O4)3(As3+O3)x(SiO4)3O5-5x(OH)20+xTrig.
8.BE.45CarlfrancisiteMn2+3(Mn2+,Mg,Fe3+,Al)42[As3+O3]2(As5+O4)4[(Si,As5+)O4]6[(As5+,Si)O4]2(OH)42Trig. 3m : R3c
8.BE.45Arakiite(Zn,Mn2+)(Mn2+,Mg)12(Fe3+,Al)2(As5+O4)2(As3+O3)(OH)23Mon. m : Bb
8.BE.45KraissliteZn3(Mn,Mg)25(Fe3+,Al)(As3+O3)2[(Si,As5+)O4]10(OH)16Orth. 222 : C2221
8.BE.50SynadelphiteMn2+9(As5+O4)2(As3+O3)(OH)9 · 2H2OOrth. mmm(2/m2/m2/m) : Pnma
8.BE.55Holdenite(Mn2+,Mg)6Zn3(AsO4)2(SiO4)(OH)8Orth. mmm(2/m2/m2/m) : Ccca
8.BE.60KoliciteMn2+7Zn4(AsO4)2(SiO4)2(OH)8Orth. mmm(2/m2/m2/m) : Cmca
8.BE.70JarosewichiteMn2+3Mn3+(AsO4)(OH)6Orth. 222
8.BE.75TheisiteCu5Zn5(AsO4,SbO4)2(OH)14Orth.
8.BE.80CoparsiteCu4(AsO4,VO4)O2ClOrth. mmm(2/m2/m2/m) : Pbcm
8.BE.85WaterhouseiteMn2+7(PO4)2(OH)8Mon. 2/m : P21/b
8.BE.90VasilseverginiteCu9O4(AsO4)2(SO4)2Mon. 2/m

Fluorescence of SabelliiteHide

Not fluorescent.

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 SabelliiteHide

References for SabelliiteHide

Localities for SabelliiteHide

Showing 9 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.
Austria
 
  • Tyrol
    • Schwaz District
      • Schrofen area
E Lackner collection
Hungary
 
  • Veszprém County
    • Balatonfüred District
      • Balatonfüred
HOM Collection
Italy
 
  • Friuli Venezia Giulia
    • Udine Province
      • Forni Avoltri
Bortolozzi et al. (2015) +1 other reference
  • Lombardy
    • Lecco Province
      • Valsassina
        • Introbio
Vergani (2019) +1 other reference
  • Sardinia
    • South Sardinia Province
      • Domusnovas
Olmi et al. (1995)
      • Narcao
Lecca et al. (2024)
Spain
 
  • Andalusia
    • Almería
      • Tíjola
Calvo Rebollar et al. (2022)
  • Asturias
    • Cabrales
      • Prado
        • Ortiguero
          • Hoyos de Alda
Vrtiška et al. (2017) +2 other references
Switzerland
 
  • Valais
    • Sierre
      • Anniviers
        • Saint-Luc
Ansermet (2012)
 
and/or  
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