Alfredstelznerite
A valid IMA mineral species
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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.
Unique Identifiers
Mindat ID:
35790
Long-form identifier:
mindat:1:1:35790:4
IMA Classification of Alfredstelznerite
Classification of Alfredstelznerite
6.D0.
6 : BORATES
D : Tetraborates
0 :
6 : BORATES
D : Tetraborates
0 :
26.4.6.
26 : HYDRATED BORATES CONTAINING HYDROXYL OR HALOGEN
4 : Tetraborates
26 : HYDRATED BORATES CONTAINING HYDROXYL OR HALOGEN
4 : Tetraborates
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Asz | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Alfredstelznerite
Vitreous, Silky
Transparency:
Transparent
Colour:
Colorless
Comment:
Aggregates are white.
Streak:
White
Hardness:
2 on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
Parallel to {010}.
Parallel to {010}.
Fracture:
Irregular/Uneven
Density:
1.77(1) g/cm3 (Measured) 1.775 g/cm3 (Calculated)
Optical Data of Alfredstelznerite
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.
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.
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).
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.
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 Alfredstelznerite
Mindat Formula:
Ca4(H2O)4[B4O4(OH)6]4(H2O)15
Element Weights:
Elements listed:
Crystallography of Alfredstelznerite
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}.
Type material: The forms observed are {010} dominant, {hk0}, {100}, {hkl}, and {hkl}.
Crystal Structure
Load
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Show
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Polyhedra Off | Si Polyhedra | All Polyhedra
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CIF File Best | x | y | z | a | b | c
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Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0006321 | Alfredstelznerite | Cooper 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 48 129-138 | 2010 | Santa Rosa mine, Sijes, Salta, Argentina | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 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 Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Near-surface Processes | |
| 25 : Evaporites (prebiotic) |
Type Occurrence of Alfredstelznerite
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 Alfredstelznerite
Other Language Names for Alfredstelznerite
Fluorescence of Alfredstelznerite
Not fluorescent.
Other Information
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 Alfredstelznerite
mindat.org URL:
https://www.mindat.org/min-35790.html
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Please feel free to link to this page.
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References for Alfredstelznerite
Reference List:
Galliski, M. A., Cooper, M. A., Marquez-Zavalia, M. F., Hawthorne, F. C. (2010) Alfredstelznerite: A new species of calcium borate hydrate from the Santa Rosa mine, Salta, northwestern Argentina. The Canadian Mineralogist, 48 (1) 123-128 doi:10.3749/canmin.48.1.123
Localities for Alfredstelznerite
Showing 1 localities.
Locality List
- 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).
All localities listed without proper references should be considered as questionable.
Argentina (TL) | |
| Galliski et al. (2010) |
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