Arsenoveszelyite
A valid IMA mineral species - pending publication
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About Arsenoveszelyite
Formula:
Cu2Zn(AsO4)(OH)3 · 2H2O
Colour:
cyan to emerald green
Lustre:
Vitreous
Hardness:
3 - 4
Specific Gravity:
3.61 (Calculated)
Crystal System:
Monoclinic
Name:
Named for being the The arsenic analogue of veszelyite.
The As analogue of veszelyite. Chemically related to, i.a., goldhillite, sabelliite, theisite, veselovskýite, and somewhat to zincolivenite.
Unique Identifiers
Mindat ID:
55948
Long-form identifier:
mindat:1:1:55948:7
IMA Classification of Arsenoveszelyite
Approved, Pending publication
IMA Formula:
Cu2+2Zn2+(As5+O4)(OH)3·2H2O
Approval year:
2021
Approval history:
IMA no. 2021-076a
Type description reference:
Classification of Arsenoveszelyite
8.DE.
8 : PHOSPHATES, ARSENATES, VANADATES
D : Phosphates, etc. with additional anions, with H2O
E : With only medium-sized cations, (OH, etc.):RO4 = 3:1
8 : PHOSPHATES, ARSENATES, VANADATES
D : Phosphates, etc. with additional anions, with H2O
E : With only medium-sized cations, (OH, etc.):RO4 = 3:1
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 |
|---|---|---|
| Avsz | 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 Arsenoveszelyite
Vitreous
Transparency:
Transparent
Colour:
Cyan to emerald green
Streak:
Light green
Hardness:
3 - 4 on Mohs scale
Hardness:
VHN10=265.5 kg/mm2 - Vickers
Tenacity:
Brittle
Cleavage:
Distinct/Good
good cleavage on {001} and {110}
good cleavage on {001} and {110}
Parting:
none
Fracture:
Irregular/Uneven
Density:
3.61 g/cm3 (Calculated)
Optical Data of Arsenoveszelyite
Type:
Biaxial (+)
RI values:
nα = 1.655(10) nβ = 1.665(5) nγ = 1.690(10)
2V:
Measured: 40°
Max. Birefringence:
δ = 0.035
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:
Very High (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.
Orientation:
Y = b
Pleochroism:
Weak
Comments:
with X = cyan, Y = cyan, and Z = indigo.
Chemistry of Arsenoveszelyite
Mindat Formula:
Cu2Zn(AsO4)(OH)3 · 2H2O
Element Weights:
Crystallography of Arsenoveszelyite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/c
Setting:
P21/c
Cell Parameters:
a = 7.5852(4) Å, b = 10.3877(5) Å, c = 9.8714(5) Å
β = 102.984(5)°
β = 102.984(5)°
Ratio:
a:b:c = 0.73 : 1 : 0.95
Unit Cell V:
757.91 ų (Calculated from Unit Cell)
Z:
4
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 7.129 Å | (95) |
| 4.391 Å | (40) |
| 3.698 Å | (100) |
| 3.521 Å | (45) |
| 3.000 Å | (50) |
| 2.811 Å | (35) |
| 2.511 Å | (40) |
| 2.388 Å | (20) |
Type Occurrence of Arsenoveszelyite
General Appearance of Type Material:
radiating aggregates or as individual lamellar crystals
Place of Conservation of Type Material:
(1) mineralogical collections of the Geological Museum of China, No. 15, Yangrou Hutong Xisi, Beijing 100083, People’s Republic of China, catalogue number M16126 (holotype), and (2) the Crystal Structure Laboratory, China University of Geosciences, Beijing 100083, People’s Republic of China, catalogue number DC-3 (cotype)
Geological Setting of Type Material:
supergene mineral from a sediment-hosted Zn–Pb–Cu deposit
Associated Minerals at Type Locality:
Synonyms of Arsenoveszelyite
Other Language Names for Arsenoveszelyite
Common Associates
Associations Based on Photo Data:
| 5 photos of Arsenoveszelyite associated with Hemimorphite | Zn4Si2O7(OH)2 · H2O |
| 1 photo of Arsenoveszelyite associated with Cuprozheshengite | Pb4CuZn2(AsO4)2(PO4)2(OH)2 |
| 1 photo of Arsenoveszelyite associated with Cuprodongchuanite | Pb4CuZn2(PO4)4(OH)2 |
| 1 photo of Arsenoveszelyite associated with Veszelyite | (Cu,Zn)2Zn(PO4)(OH)3 · 2H2O |
| 1 photo of Arsenoveszelyite associated with Azurite | Cu3(CO3)2(OH)2 |
Related Minerals - Strunz-mindat Grouping
| 8.DE. | Kipushite | (Cu,Zn)5Zn(PO4)2(OH)6 · H2O |
| 8.DE. | Goldhillite | Cu5Zn(AsO4)2(OH)6 · H2O |
| 8.DE.05 | Senegalite | Al2(PO4)(OH)(OH)2 · H2O |
| 8.DE.10 | Fluellite | Al2(PO4)F2(OH) · 7H2O |
| 8.DE.15 | Bulachite | Al6(AsO4)3(OH)9(H2O)4 · 2H2O |
| 8.DE.20 | Zapatalite | Cu3Al4(PO4)3(OH)9 · 4H2O |
| 8.DE.25 | Ceruleite | Cu2Al7(AsO4)4(OH)13 · 11.5H2O |
| 8.DE.30 | Veszelyite | (Cu,Zn)2Zn(PO4)(OH)3 · 2H2O |
| 8.DE.35 | Philipsburgite | Cu5Zn(AsO4)(PO4)(OH)6 · H2O |
| 8.DE.40 | Juanitaite | (Cu,Ca,Fe)10Bi(AsO4)4(OH)11 · 2H2O |
| 8.DE.45 | Iangreyite | Ca2Al7(PO4)2(PO3OH)2(OH,F)15 · 8H2O |
Other Information
Magnetism:
Non-Magnetic
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 Arsenoveszelyite
mindat.org URL:
https://www.mindat.org/min-55948.html
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Please feel free to link to this page.
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References for Arsenoveszelyite
Localities for Arsenoveszelyite
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.
China (TL) | |
| Miyawaki et al. (2022) +2 other references |
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The
Sanguozhuang, Shizhuang Village, Tangdan Town, Dongchuan District, Kunming, Yunnan, China