Anorthominasragrite
A valid IMA mineral species
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About Anorthominasragrite
Formula:
(V4+O)(SO4) · 5H2O
Colour:
Bluish green
Lustre:
Vitreous
Hardness:
1
Specific Gravity:
2.12 (Calculated)
Crystal System:
Triclinic
Member of:
Name:
Named for being the triclinic (anortho is Greek for "not right angle") polymorph of minasragrite.
Polymorph of:
This page provides mineralogical data about Anorthominasragrite.
Unique Identifiers
Mindat ID:
25587
Long-form identifier:
mindat:1:1:25587:3
IMA Classification of Anorthominasragrite
Approved
IMA Formula:
V4+O(S6+O4)·5H2O
Approval year:
2001
First published:
2003
Type description reference:
Cooper, M. A., Hawthorne, F. C., Grice, J. D., Haynes, P. (2003) Anorthominasragrite, V4+O(SO4)(H2O)5, a new mineral species from the Temple Mountain, Emery County, Utah, U.S.A.: description, crystal structure and hydrogen bonding. The Canadian Mineralogist, 41 (4) 959-979 doi:10.2113/gscanmin.41.4.959
Classification of Anorthominasragrite
7.DB.20
7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
D : Sulfates (selenates, etc.) with additional anions, with H2O
B : With only medium-sized cations; insular octahedra and finite units
7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
D : Sulfates (selenates, etc.) with additional anions, with H2O
B : With only medium-sized cations; insular octahedra and finite units
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 |
|---|---|---|
| Amrg | 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 Anorthominasragrite
Vitreous
Colour:
Bluish green
Streak:
Pale blue
Hardness:
1 on Mohs scale
Cleavage:
None Observed
Density:
2.12 g/cm3 (Calculated)
Optical Data of Anorthominasragrite
Type:
Biaxial (+)
RI values:
nα = 1.548(2) nβ = 1.555(2) nγ = 1.574(2)
2V:
Measured: 86° (1)
Max. Birefringence:
δ = 0.026
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:
Low (positive)
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.
Optical Extinction:
X ∧ c ≈ 18° (in β obtuse), Y ≈ a, Z ∧ b ≈ 19° (in γ obtuse).
Pleochroism:
Non-pleochroic
Chemistry of Anorthominasragrite
Mindat Formula:
(V4+O)(SO4) · 5H2O
Element Weights:
Elements listed:
Crystallography of Anorthominasragrite
Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 7.548 Å, b = 7.805 Å, c = 7.821 Å
α = 79.03°, β = 71.94°, γ = 65.31°
α = 79.03°, β = 71.94°, γ = 65.31°
Ratio:
a:b:c = 0.967 : 1 : 1.002
Unit Cell V:
397.02 ų (Calculated from Unit Cell)
Crystal Structure
Load
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Show
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
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Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Display Options
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
View
CIF File Best | x | y | z | a | b | c
CIF File Best | x | y | z | a | b | c
Rotation
Stop | Start
Stop | Start
Labels
Console Off | On | Grey | Yellow
Console Off | On | Grey | Yellow
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) |
|---|---|---|---|---|---|---|---|
| 0005878 | Anorthominasragrite | Cooper M A, Hawthorne F C, Grice J D, Haynes P (2003) Anorthominasragrite, VO(SO4)(H2O)5, a new mineral species from Temple Mountain, Emery County, Utah, U.S.A.: Description, crystal structure and hydrogen bonding The Canadian Mineralogist 41 959-979 | ![]() | 2003 | Temple Mountain, Emery County, Utah, USA | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 6.617 Å | (100) |
| 7.053 Å | (80) |
| 4.116 Å | (80) |
| 3.712 Å | (80) |
| 3.206 Å | (70) |
| 2.934 Å | (50) |
| 5.314 Å | (30) |
Reference:
Cooper, M. A., Hawthorne, F. C., Grice, J. D., Haynes, P. (2003) Anorthominasragrite, V4+O(SO4)(H2O)5, a new mineral species from the Temple Mountain, Emery County, Utah, U.S.A.: description, crystal structure and hydrogen bonding. The Canadian Mineralogist, 41 (4) 959-979 doi:10.2113/gscanmin.41.4.959
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 47b : [Sulfates and sulfites] | |
| 47e : [Vanadates, chromates, manganates] | |
| Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere | <0.6 |
| 53 : Other minerals with taphonomic origins | <0.4 |
Type Occurrence of Anorthominasragrite
General Appearance of Type Material:
Microcrystalline crusts and efflorescences.
Place of Conservation of Type Material:
Canadian Museum of Nature, Ottawa, Canada, catalogue number CMNMC 83924.
Geological Setting of Type Material:
In cracks of coal-clad silicified wood, embedded in a Triassic conglomerate.
Associated Minerals at Type Locality:
Reference:
Cooper, M. A., Hawthorne, F. C., Grice, J. D., Haynes, P. (2003) Anorthominasragrite, V4+O(SO4)(H2O)5, a new mineral species from the Temple Mountain, Emery County, Utah, U.S.A.: description, crystal structure and hydrogen bonding. The Canadian Mineralogist, 41 (4) 959-979 doi:10.2113/gscanmin.41.4.959
Synonyms of Anorthominasragrite
Other Language Names for Anorthominasragrite
Dutch:Anorthominasragriet
French:Anorthominasragrite
German:Anorthominasragrit
Norwegian:Anortominasragritt
Russian:Анортоминасрагрит
Simplified Chinese:三斜钒矾
Traditional Chinese:三斜釩礬
Relationship of Anorthominasragrite to other Species
Member of:
Other Members of Minasragrite Group:
| Minasragrite | (V4+O)(SO4) · 5H2O | Mon. 2/m : P21/b |
| Orthominasragrite | (V4+O)(SO4) · 5H2O | Orth. mm2 : Pmn21 |
Common Associates
Associations Based on Photo Data:
| 5 photos of Anorthominasragrite associated with Pyrite | FeS2 |
| 5 photos of Anorthominasragrite associated with 'Asphaltite' | |
| 4 photos of Anorthominasragrite associated with Orthominasragrite | (V4+O)(SO4) · 5H2O |
| 4 photos of Anorthominasragrite associated with Rozenite | FeSO4 · 4H2O |
| 4 photos of Anorthominasragrite associated with 'Sandstone' | |
| 2 photos of Anorthominasragrite associated with Bobjonesite | (V4+O)(SO4) · 3H2O |
| 1 photo of Anorthominasragrite associated with Szomolnokite | FeSO4 · H2O |
| 1 photo of Anorthominasragrite associated with Stanleyite | (V4+O)(SO4) · 6H2O |
| 1 photo of Anorthominasragrite associated with 'Petrified Wood' | |
| 1 photo of Anorthominasragrite associated with Oldsite-(K) | K2Fe2+[(UO2)(SO4)2]2(H2O)8 |
Related Minerals - Strunz-mindat Grouping
| 7.DB.05 | Svyazhinite | (Mg,Mn2+,Ca)(Al,Fe3+)(SO4)2F · 14H2O |
| 7.DB.05 | Aubertite | CuAl(SO4)2Cl · 14H2O |
| 7.DB.05 | Magnesioaubertite | (Mg,Cu)Al(SO4)2Cl · 14H2O |
| 7.DB.10 | Rostite | Al(SO4)(OH) · 5H2O |
| 7.DB.10 | Khademite | Al(SO4)F · 5H2O |
| 7.DB.15 | Jurbanite | Al(SO4)(OH) · 5H2O |
| 7.DB.20 | Minasragrite | (V4+O)(SO4) · 5H2O |
| 7.DB.20 | Orthominasragrite | (V4+O)(SO4) · 5H2O |
| 7.DB.25 | Bobjonesite | (V4+O)(SO4) · 3H2O |
| 7.DB.27 | Karpovite | Tl2VO(SO4)2(H2O) |
| 7.DB.30 | Metahohmannite | Fe3+2(SO4)2O · 4H2O |
| 7.DB.30 | Hohmannite | Fe3+2(SO4)2O · 8H2O |
| 7.DB.30 | Amarantite | Fe3+2(SO4)2O · 7H2O |
| 7.DB.35 | Calciocopiapite | CaFe3+4(SO4)6(OH)2 · 20H2O |
| 7.DB.35 | Zincocopiapite | ZnFe3+4(SO4)6(OH)2 · 18H2O |
| 7.DB.35 | Aluminocopiapite | Al2/3Fe3+4(SO4)6(OH)2 · 20H2O |
| 7.DB.35 | Copiapite | Fe2+Fe3+4(SO4)6(OH)2 · 20H2O |
| 7.DB.35 | Cuprocopiapite | Cu2+Fe3+4(SO4)6(OH)2 · 20H2O |
| 7.DB.35 | Magnesiocopiapite | MgFe3+4(SO4)6(OH)2 · 20H2O |
| 7.DB.35 | Ferricopiapite | Fe3+0.67Fe3+4(SO4)6(OH)2 · 20H2O |
Fluorescence of Anorthominasragrite
none
Other Information
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 Anorthominasragrite
mindat.org URL:
https://www.mindat.org/min-25587.html
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References for Anorthominasragrite
Reference List:
Cooper, M. A., Hawthorne, F. C., Grice, J. D., Haynes, P. (2003) Anorthominasragrite, V4+O(SO4)(H2O)5, a new mineral species from the Temple Mountain, Emery County, Utah, U.S.A.: description, crystal structure and hydrogen bonding. The Canadian Mineralogist, 41 (4) 959-979 doi:10.2113/gscanmin.41.4.959
Localities for Anorthominasragrite
Showing 3 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.
USA (TL) | |
| Cooper et al. (2003) +1 other reference |
| Collected by and in the collection of ... | |
| Patrick Haynes |
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North Mesa 10 Mine, North Mesa Mine Group, Temple Mountain Mining District, Emery County, Utah, USA