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Asisite

A valid IMA mineral species
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About AsisiteHide

Formula:
Pb7SiO9Cl2
Colour:
Yellow to yellow-green, red
Lustre:
Adamantine
Hardness:
Specific Gravity:
8.041 (Calculated)
Crystal System:
Tetragonal
Name:
Named after the Asis farm where the Kombat mine is located.
The Si analogue of janchevite.

Note: Asisite from the Kombat mine has been sold as either "lorettoite" or "chubutite".


Unique IdentifiersHide

Mindat ID:
391
Long-form identifier:
mindat:1:1:391:5

Similar NamesHide

Arisite
Arisite-(Ce)A valid IMA mineral speciesNaCe2(CO3)2[F2x(CO3)1-x]F
Arisite-(La)A valid IMA mineral speciesNaLa2(CO3)2[F2x(CO3)1-x]F

IMA Classification of AsisiteHide

Classification of AsisiteHide

3.DB.40

3 : HALIDES
D : Oxyhalides, hydroxyhalides and related double halides
B : With Pb, Cu, etc.
10.2.7.1

10 : OXYHALIDES AND HYDROXYHALIDES
2 : A(O,OH)Xq
17.3.9

17 : Silicates Containing other Anions
3 : Silicates with chloride (including aluminosilicates)

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

Physical Properties of AsisiteHide

Adamantine
Transparency:
Transparent
Colour:
Yellow to yellow-green, red
Streak:
Light yellow to white
Hardness:
3½ on Mohs scale
Hardness:
VHN50=146 - 186 kg/mm2 - Vickers
Cleavage:
Perfect
{001}
Density:
8.041 g/cm3 (Calculated)

Optical Data of AsisiteHide

Type:
Uniaxial (-)
RI values:
nω = 2.39 nε = 2.32
Max. Birefringence:
δ = 0.070
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
Anisotropism:
Not noticeable in air, only weakly so in oil, rotation tints of gray
Bireflectance:
Not perceptible, except at grain boundaries
Reflectivity:
WavelengthR1 (%)R2 (%)
400nm20.2% 20.7%
450nm17.9% 18.9%
500nm16.9% 17.9%
550nm16.2% 17.15%
600nm15.7% 16.7%
650nm15.35% 16.3%
700nm15.1% 16.1%


Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 20.7%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Gray
Internal Reflections:
Abundant uncolored reflections in plane-polarized light, brilliant pale greenish yellow between crossed polars
Pleochroism:
Non-pleochroic

Chemistry of AsisiteHide

Mindat Formula:
Pb7SiO9Cl2
Element Weights:
Element% weight
Pb85.651 %
O8.503 %
Cl4.187 %
Si1.659 %

Calculated from ideal end-member formula.

Crystallography of AsisiteHide

Crystal System:
Tetragonal
Class (H-M):
4/mmm(4/m2/m2/m) - Ditetragonal Dipyramidal
Space Group:
I4/mmm
Cell Parameters:
a = 3.897(2) Å, c = 22.81(2) Å
Ratio:
a:c = 1 : 5.853
Unit Cell V:
346.41 ų (Calculated from Unit Cell)
Z:
1
Morphology:
Tabular on {001}.
Comment:
Only subcell (but strongly dominant); real cell has tetragonal cell parameters ~14 and ~23 A (Welch, 2004)

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0014572AsisiteWelch M D (2004) Pb-Si ordering in sheet-oxychloride minerals: the super-structure of asisite, nominally Pb7SiO8Cl2 Mineralogical Magazine 68 247-2542004Kombat mine, Namibia0293
0001166AsisiteRouse R C, Peacor D R, Dunn P J, Criddle A J, Stanley C J, Innes J (1988) Asisite, a silicon-bearing lead oxychloride from the Kombat mine, South West Africa (Namibia) American Mineralogist 73 643-65019880293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
2.957 Å(100)
2.752 Å(60)
1.627 Å(60)
1.602 Å(50)
3.46 Å(40)
1.984 Å(40)
1.747 Å(40)
Comments:
Kombat mine, Namiba. Data from the type description.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47h : [Near-surface oxidized, dehydrated minerals]

Type Occurrence of AsisiteHide

General Appearance of Type Material:
Yellow to greenish-yellow, 0.5 mm, platy crystals.
Place of Conservation of Type Material:
Geological Survey of Canada, Ottawa, Ontario, Canada, number GSC no. 64565.
British Museum of Natural History, London, UK, number 1986,304.
Geological Setting of Type Material:
Manganese silicate lens.
Associated Minerals at Type Locality:

Synonyms of AsisiteHide

Other Language Names for AsisiteHide

Dutch:Asisiet
French:Asisite
German:Asisit
Italian:Asisite
Norwegian:Asisitt
Russian:Асисит
Spanish:Asisita

Common AssociatesHide

Associations Based on Photo Data:
15 photos of Asisite associated with HausmanniteMn2+Mn3+2O4
2 photos of Asisite associated with SahlinitePb14(AsO4)2O9Cl4
2 photos of Asisite associated with BaryteBaSO4
1 photo of Asisite associated with CahniteCa2[B(OH)4](AsO4)
1 photo of Asisite associated with Hereroite[Pb32(O,◻)21](AsO4)2[(Si,As,V,Mo)O4]2Cl10
1 photo of Asisite associated with Vladkrivovichevite[Pb32O18][Pb4Mn2O]Cl14(BO3)8 · 2H2O
1 photo of Asisite associated with KombatitePb14(VO4)2O9Cl4
1 photo of Asisite associated with BarysilitePb8Mn2+[Si2O7]3

Related Minerals - Strunz-mindat GroupingHide

3.DB.RickturneritePb7O4[Mg(OH)4](OH)Cl3Orth. mmm(2/m2/m2/m) : Pnma
3.DB.05DiaboleitePb2CuCl2(OH)4Tet. 4mm : P4mm
3.DB.10PseudoboleitePb31Cu24Cl62(OH)48Tet. 4/mmm(4/m2/m2/m) : I4/mmm
3.DB.15BoleiteKPb26Ag9Cu24(OH)48Cl62Iso. m3m(4/m32/m) : Pm3m
3.DB.20CumengeitePb21Cu20Cl42(OH)40 · 6H2OTet. 4/mmm(4/m2/m2/m) : I4/mmm
3.DB.25BideauxitePb2AgCl3(F,OH)2Iso. m3m(4/m32/m) : Fd3m
3.DB.30ChloroxiphitePb3CuO2Cl2(OH)2Mon. 2/m : P21/m
3.DB.35HematophanitePb4Fe3O8(OH,Cl)Tet. 4mm : P4mm
3.DB.40ParkinsonitePb7MoO9Cl2Tet.
3.DB.40JanchevitePb9V5+(O10.250.75)Cl2.5Tric. 1 : P1
3.DB.45EddaviditeCu12Pb2O15Br2Iso. m3m(4/m32/m) : Fm3m
3.DB.45MurdochiteCu12Pb2O15Cl2Iso. m3m(4/m32/m) : Fm3m
3.DB.50YedlinitePb6Cr3+Cl6(O,OH,H2O)8Trig. 3 : R3
3.DB.55SiidraitePb2Cu(OH)2I3Orth. mmm(2/m2/m2/m) : Fddd

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 AsisiteHide

References for AsisiteHide

Localities for AsisiteHide

Showing 4 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.
Greece
 
  • Attica
    • East Attica
      • Lavreotiki
        • Lavreotiki Municipal Unit
SEM-EDS
Namibia (TL)
 
  • Otjozondjupa Region
    • Otavi Constituency
      • Kombat
Rouse et al. (1988)
Poland
 
  • Lower Silesian Voivodeship
    • Kłodzko County
      • Gmina Bystrzyca Kłodzka
Ł. Kruszewski PXRD & pXRF data (paper in preparation)
Spain
 
  • Murcia
    • Mazarrón
Georges FAVREAU collection + EDX ...
 
and/or  
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