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Orschallite

A valid IMA mineral species
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About OrschalliteHide

Formula:
Ca3(SO3)2(SO4) · 12H2O
Colour:
Colorless
Lustre:
Vitreous
Hardness:
4
Specific Gravity:
1.90
Crystal System:
Trigonal
Name:
The name is in honour of Mr. P. Orschall, Cologne, Germany, who discovered this sulfite mineral and was also the first to find the new sulfite mineral hannebachite at the same locality (Weidenthaler, Tillmanns & Hentschel, 1993).
This page provides mineralogical data about Orschallite.


Unique IdentifiersHide

Mindat ID:
3022
Long-form identifier:
mindat:1:1:3022:5

IMA Classification of OrschalliteHide

Approved
IMA Formula:
Ca3(S4+O3)2S6+O4(H2O)12
Approval year:
1990
First published:
1993

Classification of OrschalliteHide

4.JE.15

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
E : Sulfites
34.8.7.1

34 : SELENITES, TELLURITES AND SULFITES
8 : Compound Selenites, Tellurites and Sulfites

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

Physical Properties of OrschalliteHide

Vitreous
Transparency:
Transparent
Colour:
Colorless
Streak:
White
Hardness:
Density:
1.90(3) g/cm3 (Measured)    1.87 g/cm3 (Calculated)

Optical Data of OrschalliteHide

Type:
Uniaxial (+)
RI values:
nω = 1.4941(4) nε = 1.4960(4)
Max. Birefringence:
δ = 0.002
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 (negative)
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 OrschalliteHide

Mindat Formula:
Ca3(SO3)2(SO4) · 12H2O
Element Weights:
Element% weight
O59.396 %
Ca20.289 %
S16.233 %
H4.082 %

Calculated from ideal end-member formula.
O
Ca
S
H

Crystallography of OrschalliteHide

Crystal System:
Trigonal
Class (H-M):
3m(32/m) - Hexagonal Scalenohedral
Space Group:
R3c
Setting:
R3c
Cell Parameters:
a = 11.35 Å, c = 28.32 Å
Ratio:
a:c = 1 : 2.495
Unit Cell V:
3,159.48 ų (Calculated from Unit Cell)
Z:
6
Morphology:
Pseudo-cubic crystals.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0014633OrschalliteWeidenthaler C, Tillmanns E, Hentschel G (1993) Orschallite, Ca3(SO3)2SO4*12H2O, a new calcium-sulfite-sulfate-hydrate mineral Mineralogy and Petrology 48 167-1771993Hannebacher Ley, Hannebach, Eifel, Germany0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
8.11 Å(80)
5.73 Å(100)
3.63 Å(60)
3.28 Å(40)
2.69 Å(80)
2.11 Å(40)
Comments:
Hannebacher Ley, Rhineland-Palatinate, Germany. The data are from the type description.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45a : [Sulfates, arsenates, selenates, antimonates]
47b : [Sulfates and sulfites]
Stage 10b: Anthropogenic minerals<10 Ka
56 : Slag and smelter minerals (see also #51 and #55)

Type Occurrence of OrschalliteHide

General Appearance of Type Material:
Colorless, transparent pseudo-cubic crystals to 0.3 mm.
Place of Conservation of Type Material:
University of Vienna, Austria.
Geological Setting of Type Material:
Submarine pillow basalts.
Associated Minerals at Type Locality:

Synonyms of OrschalliteHide

Other Language Names for OrschalliteHide

Common AssociatesHide

Associations Based on Photo Data:
6 photos of Orschallite associated with DolomiteCaMg(CO3)2
6 photos of Orschallite associated with PicropharmacoliteCa4Mg(AsO4)2(HAsO4)2 · 11H2O
1 photo of Orschallite associated with Native BismuthBi

Related Minerals - Strunz-mindat GroupingHide

4.JE.XAlbertiniiteFe2+(SO3) · 3H2OMon. 2/m
4.JE.MikenewiteMn2+(S4+O3) · 3H2OMon. 2/m
4.JE.Vanpeltite(Mo2O5)(S4+O3) · 4H2OMon. 2/m
4.JE.05FleisstaliteFeSO3 · 3H2OOrth. mmm(2/m2/m2/m) : Pnma
4.JE.05GravegliaiteMn2+SO3 · 3H2OOrth. mmm(2/m2/m2/m) : Pnma
4.JE.10HannebachiteCaSO3 · H2OOrth. mmm(2/m2/m2/m)
4.JE.20ScotlanditePbSO3Mon. 2/m : P21/m
4.JE.25Kollerite(NH4)2Fe3+(SO3)2(OH) · H2OOrth. mmm(2/m2/m2/m) : Cmcm

Other InformationHide

IR Spectrum:
The infrared pattern has absorption bands for H2O (3300 and 1630 cm-1), for SO3 (945 and 630-650 cm-1), and for SO4 (1100 cm-1).
Thermal Behaviour:
TGA of synthetic material showed endothermic dehydration at 120°C to anhydrite with a weight loss of 34.5%.
Notes:
Rapidly volatilizes under an electron microprobe beam.
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 OrschalliteHide

References for OrschalliteHide

Localities for OrschalliteHide

Showing 5 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
 
  • Ontario
    • Timiskaming District
      • Cobalt-Gowganda region
        • Cobalt area
          • Coleman Township
Reiner Mielke 2015
Reiner Mielke 2016
France
 
  • Occitanie
    • Aveyron
      • Rodez
        • Sévérac-d'Aveyron
Eytier J.R. & Ch. et al. (2004)
Germany (TL)
 
  • Rhineland-Palatinate
    • Ahrweiler
      • Brohltal
        • Spessart
          • Hannebach
Weidenthaler et al. (1993) +1 other reference
USA
 
  • Utah
    • Grand County
      • Thompsons Mining District
        • Yellow Cat Mesa
Kasatkin et al. (2014) +1 other reference
 
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