Parwelite
A valid IMA mineral species
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About Parwelite
Formula:
Mn10Sb2As2Si2O24
Colour:
Yellow-brown, tan
Lustre:
Greasy
Hardness:
5½
Specific Gravity:
4.62
Crystal System:
Monoclinic
Name:
In honour of Dr. Alexander Parwel (June 15, 1906, Valga - 23 December 1978, Stockholm, Sweden), Swedish chemist, Swedish National History Museum, Stockholm, Sweden, who has performed many analyses of Långban minerals, including this one.
This page provides mineralogical data about Parwelite.
Unique Identifiers
Mindat ID:
3129
Long-form identifier:
mindat:1:1:3129:1
IMA Classification of Parwelite
Approved
IMA Formula:
Mn2+10Sb5+2As5+2Si2O24
Approval year:
1966
First published:
1968
Classification of Parwelite
8.BD.15
8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
D : With only medium-sized cations, (OH, etc.):RO4= 2:1
8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
D : With only medium-sized cations, (OH, etc.):RO4= 2:1
44.3.3.1
44 : ANTIMONATES
3 : Miscellaneous
44 : ANTIMONATES
3 : Miscellaneous
17.7.18
17 : Silicates Containing other Anions
7 : Silicates with vanadate, arsenate or antimonate
17 : Silicates Containing other Anions
7 : Silicates with vanadate, arsenate or antimonate
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 |
|---|---|---|
| Pwe | 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 Parwelite
Greasy
Transparency:
Transparent
Colour:
Yellow-brown, tan
Hardness:
5½ on Mohs scale
Tenacity:
Brittle
Cleavage:
Imperfect/Fair
Fair to poor on {010}
Fair to poor on {010}
Fracture:
Sub-Conchoidal
Density:
4.62 g/cm3 (Measured) 4.64 g/cm3 (Calculated)
Optical Data of Parwelite
Type:
Biaxial (+)
RI values:
nα = 1.85(1) nβ = 1.85(1) nγ = 1.88(1)
2V:
Measured: 27° (3)
Max. Birefringence:
δ = 0.030
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.
Dispersion:
r > v strong
Chemistry of Parwelite
Mindat Formula:
Mn10Sb2As2Si2O24
Element Weights:
Common Impurities:
Fe,Pb,Ca
Crystallography of Parwelite
Crystal System:
Monoclinic
Class (H-M):
m - Domatic
Space Group:
Bb
Cell Parameters:
a = 10.048(2) Å, b = 19.418(5) Å, c = 9.735(5) Å
β = 95.83(1)°
β = 95.83(1)°
Ratio:
a:b:c = 0.517 : 1 : 0.501
Unit Cell V:
1,889.59 ų (Calculated from Unit Cell)
Z:
8
Crystal Structure
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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) |
|---|---|---|---|---|---|---|---|
| 0012688 | Parwelite | Marsh R E, Schomaker V (1979) Some incorrect space groups in Inorganic Chemistry, Volume 16 Inorganic Chemistry 18 2331-2336 | 1979 | Langban, Sweden | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 2.734 Å | (100) |
| 2.915 Å | (95) |
| 4.84 Å | (50) |
| 3.411 Å | (50) |
| 2.422 Å | (40) |
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| High-? alteration and/or metamorphism | |
| 32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits |
Type Occurrence of Parwelite
General Appearance of Type Material:
Crystals rounded, stubby prismatic, to 1 cm.
Place of Conservation of Type Material:
Swedish Museum of Natural History, Stockholm, Sweden, NRMS 26758; National Museum of Natural History, Washington, D.C., USA, 120065.
Geological Setting of Type Material:
High temperature skarn.
Associated Minerals at Type Locality:
Synonyms of Parwelite
Other Language Names for Parwelite
Relationship of Parwelite to other Species
Structurally related to group(s):
Common Associates
Associations Based on Photo Data:
| 1 photo of Parwelite associated with Långbanite | Mn2+4Mn3+9Sb5+O16(SiO4)2 |
| 1 photo of Parwelite associated with Calcite | CaCO3 |
Related Minerals - Strunz-mindat Grouping
| 8.BD. | Antipovite | Cu5O2(PO4)2 |
| 8.BD.05 | Reichenbachite | Cu5(PO4)2(OH)4 |
| 8.BD.05 | Cornwallite | Cu5(AsO4)2(OH)4 |
| 8.BD.05 | Pseudomalachite | Cu5(PO4)2(OH)4 |
| 8.BD.10 | Gatehouseite | Mn2+5(PO4)2(OH)4 |
| 8.BD.10 | Arsenoclasite | Mn2+5(AsO4)2(OH)4 |
| 8.BD.20 | Reppiaite | Mn2+5(VO4)2(OH)4 |
| 8.BD.25 | Ludjibaite | Cu5(PO4)2(OH)4 |
| 8.BD.30 | Cornubite | Cu5(AsO4)2(OH)4 |
Other Information
Notes:
It is insoluble in cold 1:1 HCl solution
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 Parwelite
mindat.org URL:
https://www.mindat.org/min-3129.html
Please feel free to link to this page.
Please feel free to link to this page.
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References for Parwelite
Reference List:
Moore, Paul Brian., Araki, Takaharu. (1977) Parwelite, MnII10SbV2AsV2Si2O24, a complex anion-deficient fluorite derivative structure. Inorganic Chemistry, 16 (8) 1839-1847 doi:10.1021/ic50174a003
Marsh, Richard E., Schomaker, Verner (1979) Some incorrect space groups in Inorganic Chemistry, Volume 16. Inorganic Chemistry, 18 (8) 2331-2336 doi:10.1021/ic50198a064
Bevan, D. J. M., Martin, R. L. (2008) The role of the coordination defect: A new structural description of four fluorite-related sesquioxide minerals, bixbyite (Mn2O3), braunite (Mn7SiO12), braunite II (CaMn14SiO24), parwelite (Mn10Sb2As2Si2O24), and their structural relationships. Journal of Solid State Chemistry, 181. 2250-2259 doi:10.1016/j.jssc.2008.04.046
Localities for Parwelite
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.
Sweden (TL) | |
| Moore (1969) +1 other reference |
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symbol to view information about a locality.
The
Långban Mine, Långban Ore District, Filipstad, Värmland County, Sweden