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Cerchiaraite-(Al)

A valid IMA mineral species
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About Cerchiaraite-(Al)Hide

Formula:
Ba4Al4O3(OH)3(Si4O12)[Si2O3(OH)4]Cl
Colour:
Blue to bluish-green
Lustre:
Vitreous
Hardness:
4½
Specific Gravity:
3.69
Crystal System:
Tetragonal
Name:
in allusion to relation with "cerchiaraite" (now cerchiaraite-(Mn))
The Al analogue of cerchiaraite-(Mn) (ex-cerchiaraite) and cerchiaraite-(Fe). Chemically related to meierite.

The structure details (1) corner-sharing silicate tetrahedra, forming 4-membered rings; (2) the rings share corners with an edge-sharing chain of AlO6 octahedra || c; (3) the rings alternate with Cl sites alternates along c; (4) large channels in the framework host Ba around their peripheries, statistically distributed Si2O3(OH)4 dimers, and Cl atoms.


Unique IdentifiersHide

Mindat ID:
42782
Long-form identifier:
mindat:1:1:42782:3

Similar NamesHide

Cerchiaraite-(Fe)A valid IMA mineral speciesBa4Fe43+O3(OH)3(Si4O12)[Si2O3(OH)4]Cl
Cerchiaraite-(Mn)A valid IMA mineral speciesBa4Mn43+(Si4O12)O2(OH)4Cl2[Si2O3(OH)4]
CherchiaraiteA synonym of Cerchiaraite Group

IMA Classification of Cerchiaraite-(Al)Hide

Approved
IMA Formula:
Ba4Al4(Si4O12)O2(OH)4Cl2[Si2O3(OH)4]
Approval year:
2012

Classification of Cerchiaraite-(Al)Hide

9.CF.25

9 : SILICATES (Germanates)
C : Cyclosilicates
F : [Si4O12]8- 4-membered single rings, with insular complex anions

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

Physical Properties of Cerchiaraite-(Al)Hide

Vitreous
Transparency:
Transparent
Colour:
Blue to bluish-green
Streak:
Pale blue-green
Hardness:
4½ on Mohs scale
Comment:
ca. 4.5
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Irregular/Uneven
Density:
3.69(3) g/cm3 (Measured)    3.643 g/cm3 (Calculated)

Optical Data of Cerchiaraite-(Al)Hide

Type:
Uniaxial (-)
RI values:
nω = 1.695(2) nε = 1.677(2)
Max. Birefringence:
δ = 0.018
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.
Pleochroism:
Strong
Comments:
colorless (O), blue (E), O < E

Chemistry of Cerchiaraite-(Al)Hide

Mindat Formula:
Ba4Al4O3(OH)3(Si4O12)[Si2O3(OH)4]Cl
Element Weights:
Element% weight
Ba43.313 %
O31.539 %
Si13.287 %
Al8.510 %
Cl2.795 %
H0.556 %

Calculated from ideal end-member formula.
Ba
O
Si
Al
Cl
H
Common Impurities:
Fe(III),Mg,Fe(II),(Mn(II))

Crystallography of Cerchiaraite-(Al)Hide

Crystal System:
Tetragonal
Class (H-M):
4/mmm(4/m2/m2/m) - Ditetragonal Dipyramidal
Space Group:
I4/mmm
Cell Parameters:
a = 14.317(4) Å, c = 6.0037(18) Å
Ratio:
a:c = 1 : 0.419
Unit Cell V:
1230.6 ų

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
10.15 Å(39)
4.407 Å(39)
3.316 Å(74)
3.009 Å(100)
2.580 Å(93)
2.029 Å(43)
1.880 Å(68)
1.403 Å(54)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)
Geological Setting:
Esquire #7 and #8 claims

Type Occurrence of Cerchiaraite-(Al)Hide

General Appearance of Type Material:
subparallel aggregates of irregular prisms, generally less than 1 mm across
Place of Conservation of Type Material:
Natural History Museum of Los Angeles County, Los Angeles, California, USA, catalogue numbers 63519, 63517 and 63518
Geological Setting of Type Material:
quartz-sanbomite vein assemblages resulting fromfluid interaction along the margin of the vein; associated minerals concert Esquire # 1 claim
Associated Minerals at Type Locality:

Synonyms of Cerchiaraite-(Al)Hide

Other Language Names for Cerchiaraite-(Al)Hide

Relationship of Cerchiaraite-(Al) to other SpeciesHide

Other Members of Cerchiaraite Group:
Cerchiaraite-(Fe)Ba4Fe3+4O3(OH)3(Si4O12)[Si2O3(OH)4]Cl Tet. 4/mmm(4/m2/m2/m) : I4/mmm
Cerchiaraite-(Mn)Ba4Mn3+4(Si4O12)O2(OH)4Cl2[Si2O3(OH)4]Tet. 4/mmm(4/m2/m2/m) : I4/mmm

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Cerchiaraite-(Al) associated with SanborniteBaSi2O5
1 photo of Cerchiaraite-(Al) associated with TitantaramelliteBa4(Ti,Fe3+,Fe2+,Mg)4(B2Si8O27)O2Clx
1 photo of Cerchiaraite-(Al) associated with QuartzSiO2

Related Minerals - Strunz-mindat GroupingHide

9.CF.BobmeyeritePb4(Al3Cu)(Si4O12)(S0.5Si0.5O4)(OH)7Cl(H2O)3Orth. mmm(2/m2/m2/m) : Pnnm
9.CF.05AshburtonitePb4Cu4(Si4O12)(HCO3)4(OH)3Cl · H2OTet.
9.CF.10Kainosite-(Y)Ca2Y2(SiO3)4(CO3) · H2OOrth. mmm(2/m2/m2/m)
9.CF.15ClinophosinaiteNa12(Ca,Sr)4(Si4O12)(PO4)4Mon. 2/m : P2/b
9.CF.15Phosinaite-(Ce)Na13Ca2(Ce,La,Th,Nd,Pr)(Si4O12)(PO4)4Orth. 222 : P21212
9.CF.20StrakhoviteNaBa3Mn2+2Mn3+2Si6O19(OH)3Orth. mmm(2/m2/m2/m)
9.CF.25Cerchiaraite-(Fe)Ba4Fe3+4O3(OH)3(Si4O12)[Si2O3(OH)4]Cl Tet. 4/mmm(4/m2/m2/m) : I4/mmm
9.CF.25Cerchiaraite-(Mn)Ba4Mn3+4(Si4O12)O2(OH)4Cl2[Si2O3(OH)4]Tet. 4/mmm(4/m2/m2/m) : I4/mmm

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 Cerchiaraite-(Al)Hide

References for Cerchiaraite-(Al)Hide

Localities for Cerchiaraite-(Al)Hide

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.
Canada
 
  • Yukon
    • Watson Lake mining district
      • Itsi Mountain
        • Wilson Lake
McNeil et al. (2013) +1 other reference
Sweden
 
  • Örebro County
    • Askersund
      • Zinkgruvan
Cámara et al. (2021)
USA (TL)
 
  • California
    • Fresno County
      • Big Creek-Rush Creek Mining District
        • Big Creek
Williams et al. (2012) +1 other reference
Williams et al. (2012) +2 other references
        • Rush Creek
Walstrom (n.d.) +3 other references
Walstrom (n.d.)
 
and/or  
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