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Alfredstelznerite

A valid IMA mineral species
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Alfred Wilhelm Stelzner
Formula:
Ca4(H2O)4[B4O4(OH)6]4(H2O)15
Colour:
Colorless
Lustre:
Vitreous, Silky
Hardness:
2
Specific Gravity:
1.77
Crystal System:
Orthorhombic
Name:
Named for Alfred Wilhelm Stelzner [December 20, 1840 Dresden, Germany - February 25, 1895 Wiesbaden, Hesse, Germany]. Professor of mineralogy at the Bergakademie Freiberg.
This page provides mineralogical data about Alfredstelznerite.


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Unique IdentifiersHide

Mindat ID:
35790
Long-form identifier:
mindat:1:1:35790:4

IMA Classification of AlfredstelzneriteHide

Approved
IMA Formula:
Ca4B16O16(OH)24·19H2O
Approval year:
2007
First published:
2010

Classification of AlfredstelzneriteHide

6.D0.

6 : BORATES
D : Tetraborates
0 :
26.4.6.

26 : HYDRATED BORATES CONTAINING HYDROXYL OR HALOGEN
4 : Tetraborates

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

Physical Properties of AlfredstelzneriteHide

Vitreous, Silky
Transparency:
Transparent
Colour:
Colorless
Comment:
Aggregates are white.
Streak:
White
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
Parallel to {010}.
Fracture:
Irregular/Uneven
Density:
1.77(1) g/cm3 (Measured)    1.775 g/cm3 (Calculated)

Optical Data of AlfredstelzneriteHide

Type:
Biaxial (+)
RI values:
nα = 1.476(3) nβ = 1.478(3) nγ = 1.494(3)
2V:
Calculated: 39°
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:
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 biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
None observed.
Optical Extinction:
X = b, Y = c, Z = a.
Pleochroism:
Not Visible

Chemistry of AlfredstelzneriteHide

Mindat Formula:
Ca4(H2O)4[B4O4(OH)6]4(H2O)15
Element Weights:
Element% weight
O70.459 %
B12.911 %
Ca11.966 %
H4.665 %

Calculated from ideal end-member formula.

Crystallography of AlfredstelzneriteHide

Crystal System:
Orthorhombic
Class (H-M):
mm2 - Pyramidal
Space Group:
Pca21
Cell Parameters:
a = 12.161 Å, b = 40.477 Å, c = 10.1843 Å
Ratio:
a:b:c = 0.3 : 1 : 0.252
Unit Cell V:
5,013.13 ų (Calculated from Unit Cell)
Morphology:
Radial aggregates; sometimes parallel aggregates. Elongate along [001].

Type material: The forms observed are {010} dominant, {hk0}, {100}, {hkl}, and {hkl}.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006321AlfredstelzneriteCooper M A, Hawthorne F C, Galliski M A, Marquez-Zavalia M F (2010) The crystal structure of alfredstelznerite, Ca4(H2O)4[B4O4(OH)6]4(H2O)15, a complex hydroxy-hydrated calcium borate mineral The Canadian Mineralogist 48 129-1382010Santa Rosa mine, Sijes, Salta, Argentina0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
10.501 Å(100)
5.226 Å(70)
3.837 Å(70)
3.118 Å(70 broad)
4.623 Å(60 broad)
2.612 Å(60)
2.538 Å(60)
Comments:
Santa Rosa Mine, Argentina. Data from the type description.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
25 : Evaporites (prebiotic)

Type Occurrence of AlfredstelzneriteHide

General Appearance of Type Material:
White radial aggregates. The crystals are up to 5 mm long and 30 mm wide.
Place of Conservation of Type Material:
Facultad de Ciencias Exactas Físicas y Naturales, Universidad Nacional de Córdoba, Argentina, number MS003266.
Geological Setting of Type Material:
Sedimentary-evaporitic borate-bearing clays. Found immediately after the rainy season.

Synonyms of AlfredstelzneriteHide

Other Language Names for AlfredstelzneriteHide

Fluorescence of AlfredstelzneriteHide

Not fluorescent.

Other InformationHide

Notes:
Dissolves slowly in warm water. Soluble in HCl, and the solution colors a flame yellowish green, as is typical of boron-bearing minerals.
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 AlfredstelzneriteHide

References for AlfredstelzneriteHide

Localities for AlfredstelzneriteHide

Showing 1 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.
Argentina (TL)
 
  • Jujuy Province
    • Susques Department
      • Sijes
Galliski et al. (2010)
 
and/or  
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