Pseudolyonsite
A valid IMA mineral species
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About Pseudolyonsite
Formula:
Cu3(VO4)2
Colour:
Dark red with a brownish tint to black
Lustre:
Adamantine, Sub-Metallic
Hardness:
2 - 3
Specific Gravity:
4.749 (Calculated)
Crystal System:
Monoclinic
Name:
For the relation to lyonsite to which it is visually similar.
Dimorph of:
Unique Identifiers
Mindat ID:
40571
Long-form identifier:
mindat:1:1:40571:5
GUID
(UUID V4):
(UUID V4):
7d69fbde-55e2-4550-b8ff-b801da71650f
IMA Classification of Pseudolyonsite
Classification of Pseudolyonsite
8.AB.35
8 : PHOSPHATES, ARSENATES, VANADATES
A : Phosphates, etc. without additional anions, without H2O
B : With medium-sized cations
8 : PHOSPHATES, ARSENATES, VANADATES
A : Phosphates, etc. without additional anions, without H2O
B : With medium-sized cations
38.3.8.4
38 : ANHYDROUS NORMAL PHOSPHATES, ARSENATES, AND VANADATES
3 : (AB)3(XO4)2
38 : ANHYDROUS NORMAL PHOSPHATES, ARSENATES, AND VANADATES
3 : (AB)3(XO4)2
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 |
---|---|---|
Plyo | 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 Pseudolyonsite
Adamantine, Sub-Metallic
Transparency:
Translucent, Opaque
Colour:
Dark red with a brownish tint to black
Streak:
Reddish-brown
Hardness:
2 - 3 on Mohs scale
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Conchoidal
Comment:
Long thin needles are flexible.
Density:
4.749 g/cm3 (Calculated)
Optical Data of Pseudolyonsite
Anisotropism:
Distinct
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
400nm | 19% | 21.75% |
420nm | 18.55% | 21.1% |
440nm | 17.9% | 20.55% |
460nm | 17.25% | 19.95% |
470nm | 17.05% | 19.6% |
480nm | 16.9% | 19.3% |
500nm | 16.6% | 18.9% |
520nm | 16.35% | 18.5% |
540nm | 16.15% | 18.25% |
546nm | 16.1% | 18.15% |
560nm | 16% | 17.95% |
580nm | 15.9% | 17.75% |
589nm | 15.85% | 17.7% |
600nm | 15.8% | 17.6% |
620nm | 15.7% | 17.45% |
640nm | 15.6% | 17.4% |
650nm | 15.55% | 17.4% |
660nm | 15.5% | 17.4% |
680nm | 15.5% | 17.4% |
700nm | 15.5% | 17.4% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 21.75%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Grey with a weak bluish tint.
Internal Reflections:
Ubiquitous, red to orange.
Pleochroism:
Non-pleochroic
Chemistry of Pseudolyonsite
Mindat Formula:
Cu3(VO4)2
Elements listed:
Crystallography of Pseudolyonsite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/b
Setting:
P1 21/c 1
Cell Parameters:
a = 6.2695(4) Å, b = 8.0195(3) Å, c = 6.3620(3) Å
β = 111.96(1)°
β = 111.96(1)°
Ratio:
a:b:c = 0.782 : 1 : 0.793
Unit Cell V:
296.66 ų
Z:
2
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) |
---|---|---|---|---|---|---|---|
0018365 | Pseudolyonsite | Zelenski M E, Zubkova N V, Pekov I V, Boldyreva M M, Pushcharovsky D Y, Nekrasov A N (2011) Pseudolyonsite, Cu3(VO4)2, a new mineral species from the Tolbachik volcano, Kamchatka Peninsula, Russia European Journal of Mineralogy 23 475-481 | 2011 | Tolbachik volcano, Kamchatka Peninsula, Russia | 0 | 293 | |
0018360 | Pseudolyonsite | Shannon R D, Calvo C (1972) Crystal structure of a new form of Cu3V2O8 Canadian Journal of Chemistry 50 3944-3949 | 1972 | synthetic | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
4.70 Å | (60) |
3.30 Å | (79) |
3.22 Å | (87) |
3.18 Å | (34) |
2.894 Å | (74) |
2.761 Å | (100) |
2.479 Å | (59) |
2.419 Å | (67) |
Geological Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Stage 7: Great Oxidation Event | <2.4 |
45b : [Other oxidized fumarolic minerals] | |
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere | <0.6 |
53 : Other minerals with taphonomic origins | <0.4 |
Type Occurrence of Pseudolyonsite
General Appearance of Type Material:
Needles that are 5–20 µm across and up to 0.5 mm in the length, which sometimes produce parallel intergrowths, sprays or openwork clusters up to 2 mm.
Place of Conservation of Type Material:
A.E. Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia (# 3879/1).
Geological Setting of Type Material:
Fumarole. Likely deposited at a temperature ranging from 200 to 300 °C.
Associated Minerals at Type Locality:
Synonyms of Pseudolyonsite
Common Associates
Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat Grouping
8.AB. | Rodolicoite | Fe3+PO4 |
8.AB. | Johanngeorgenstadtite | Ni2+4.5(AsO4)3 |
8.AB. | Borisenkoite | Cu3[(V,As)O4]2 |
8.AB. | Niasite | Ni2+4.5(AsO4)3 |
8.AB. | Olsenite | KFe4(PO4)3 |
8.AB. | Karwowskiite | Ca9Mg(Fe2+0.5◻0.5)(PO4)7 |
8.AB.05 | Farringtonite | Mg3(PO4)2 |
8.AB.10 | Ferrisicklerite | Li1-x(Fe3+xFe2+1-x)PO4 |
8.AB.10 | Heterosite | (Fe3+,Mn3+)PO4 |
8.AB.10 | Lithiophilite | LiMn2+PO4 |
8.AB.10 | Natrophilite | NaMn2+PO4 |
8.AB.10 | Purpurite | Mn3+(PO4) |
8.AB.10 | Sicklerite | Li1-x(Mn3+xMn2+1-x)PO4 |
8.AB.10 | Simferite | LiMg(PO4) |
8.AB.10 | Triphylite | LiFe2+PO4 |
8.AB.10 | Karenwebberite | NaFe2+PO4 |
8.AB.15 | Sarcopside | Fe2+3(PO4)2 |
8.AB.15 | Chopinite | Mg3(PO4)2 |
8.AB.15 | Zavalíaite | Mn2+3(PO4)2 |
8.AB.20 | Beusite | Mn2+Mn2+2 (PO4)2 |
8.AB.20 | Graftonite | Fe2+Fe2+2(PO4)2 |
8.AB.20 | Graftonite-(Ca) | CaFe2+2(PO4)2 |
8.AB.20 | Graftonite-(Mn) | MnFe2+2(PO4)2 |
8.AB.20 | Beusite-(Ca) | CaMn2+2(PO4)2 |
8.AB.25 | Xanthiosite | Ni3(AsO4)2 |
8.AB.30 | Lammerite | Cu3(AsO4)2 |
8.AB.30 | Paralammerite | Cu3(AsO4)2 |
8.AB.35 | Mcbirneyite | Cu3(VO4)2 |
8.AB.35 | Stranskiite | Zn2Cu(AsO4)2 |
8.AB.40 | Lyonsite | Cu3Fe4(VO4)6 |
8.AB.40 | Michalskiite | Fe3+1.33Cu2+2(MgFe3+)2(VO4)6 |
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 Pseudolyonsite
mindat.org URL:
https://www.mindat.org/min-40571.html
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References for Pseudolyonsite
Reference List:
Zelenski, Michael E., Zubkova, Natalia V., Pekov, Igor V., Boldyreva, Maya M., Yu. Pushcharovsky, Dmitry, Nekrasov, Aleksey N. (2011) Pseudolyonsite, Cu3(VO4)2, a new mineral species from the Tolbachik volcano, Kamchatka Peninsula, Russia. European Journal of Mineralogy, 23 (3) 475-481 doi:10.1127/0935-1221/2011/0023-2101
Localities for Pseudolyonsite
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).
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.
All localities listed without proper references should be considered as questionable.
Russia (TL) | |
| Zelenski et al. (2011) |
| In the collection of Brent Thorne. +1 other reference |
Quick NavTopAbout PseudolyonsiteUnique IdentifiersIMA Classification Classification Mineral SymbolsPhysical Properties Optical Data Chemistry Crystallography Crystal StructureX-Ray Powder DiffractionGeological EnvironmentType Occurrence SynonymsCommon AssociatesStrunz-MindatOther InformationInternet Links References Localities Locality List
Yadovitaya fumarole, Second scoria cone, Northern Breakthrough, Great Fissure eruption, Tolbachik Volcanic field, Milkovsky District, Kamchatka Krai, Russia