Paraershovite
A valid IMA mineral species
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About Paraershovite
Formula:
Na3K3Fe3+2Si8O20(OH)4 · 4H2O
Colour:
yellow with orange or pinkish shades
Lustre:
Vitreous
Specific Gravity:
2.60
Crystal System:
Triclinic
Name:
The name paraershovite [from the Greek para (close by) and ershovite] recognizes the close structural and chemical relations between the new mineral and its closest analogue
Type Locality:
Unique Identifiers
Mindat ID:
39560
Long-form identifier:
mindat:1:1:39560:3
GUID
(UUID V4):
(UUID V4):
f8867e42-344b-4dff-b483-6ed3b26204b9
IMA Classification of Paraershovite
Classification of Paraershovite
9.DF.15
9 : SILICATES (Germanates)
D : Inosilicates
F : Inosilicates with 2-periodic multiple chains
9 : SILICATES (Germanates)
D : Inosilicates
F : Inosilicates with 2-periodic multiple chains
66.6.3.2
66 : INOSILICATES Double-Width,Unbranched Chains,(W=2)
6 : Double-Width Unbranched Chains, W=2 with P=2 non-amphibole configuration
66 : INOSILICATES Double-Width,Unbranched Chains,(W=2)
6 : Double-Width Unbranched Chains, W=2 with P=2 non-amphibole configuration
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 |
---|---|---|
Psh | 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 Paraershovite
Vitreous
Transparency:
Transparent, Translucent
Colour:
yellow with orange or pinkish shades
Streak:
White
Tenacity:
Brittle
Cleavage:
Perfect
{100}
{100}
Fracture:
Splintery, Step-Like
Density:
2.60(3) g/cm3 (Measured) 2.584 g/cm3 (Calculated)
Optical Data of Paraershovite
Type:
Biaxial (+)
RI values:
nα = 1.569(2) nβ = 1.583(2) nγ = 1.602(2)
2V:
Measured: 80° (3), Calculated: 82°
Max Birefringence:
δ = 0.033
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
and does not take into account mineral colouration.
Surface Relief:
Moderate
Dispersion:
dispersion r > v (weak)
Pleochroism:
Non-pleochroic
Chemistry of Paraershovite
Mindat Formula:
Na3K3Fe3+2Si8O20(OH)4 · 4H2O
Crystallography of Paraershovite
Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 10.1978(5) Å, b = 12.0155(6) Å, c = 5.2263(3) Å
α = 103.439(1)°, β = 96.020(1)°, γ = 91.683(1)°
α = 103.439(1)°, β = 96.020(1)°, γ = 91.683(1)°
Ratio:
a:b:c = 0.849 : 1 : 0.435
Unit Cell V:
618.46 ų (Calculated from Unit Cell)
Z:
1
Crystal Structure
Load
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
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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) |
---|---|---|---|---|---|---|---|
0006330 | Paraershovite | Khomyakov A P, Camara F, Sokolova E, Abdu Y, Hawthorne F C (2010) Paraershovite, Na3K3Fe3+2(Si4O10OH)2(OH)2(H2O)4, a new mineral species from the Khibina Alkaline massif, Kola Peninsula, Russia: Description and crystal structure The Canadian Mineralogist 48 279-290 | 2010 | the Khibina Alkaline massif, Kola Peninsula, Russia | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
11.778 Å | (100) |
4.390 Å | (70) |
4.109 Å | (60) |
3.390 Å | (50) |
3.012 Å | (70) |
2.730 Å | (60) |
2.606 Å | (70) |
Geological Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Stage 4b: Highly evolved igneous rocks | >3.0 |
35 : Ultra-alkali and agpaitic igneous rocks |
Type Occurrence of Paraershovite
General Appearance of Type Material:
equant (100) platy and [001] elongate prismatic crystals up to 0.5–1 mm and aggregates up to 2–3 mm, sporadically scattered
in the pegmatite matrix.
in the pegmatite matrix.
Place of Conservation of Type Material:
Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia (catalogue number 3793).
Geological Setting of Type Material:
hyperagpaitic pegmatite occurring in ijolite–urtite.
Associated Minerals at Type Locality:
Synonyms of Paraershovite
Related Minerals - Strunz-mindat Grouping
9.DF. | Bohseite | Ca4Be3+xAl1-xSi9O25-x(OH)3+x |
9.DF.05 | Chesterite | (Mg,Fe)17Si20O54(OH)6 |
9.DF.05 | Clinojimthompsonite | (Mg,Fe)5Si6O16(OH)2 |
9.DF.05 | Jimthompsonite | (Mg,Fe)5Si6O16(OH)2 |
9.DF.15 | Ershovite | Na4K3(Fe,Mn,Ti)2Si8O22(OH)4 · 4H2O |
9.DF.20 | Tvedalite | (Ca,Mn)4Be3Si6O17(OH)4 · 3H2O |
9.DF.25 | Bavenite | Ca4Be2Al2Si9O26(OH)2 |
9.DF.30 | Bigcreekite | BaSi2O5 · 4H2O |
Fluorescence of Paraershovite
none
Other Information
Notes:
Paraershovite readily decomposes at room temperature in a ceramic container with 50% HCl and HNO3 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 Paraershovite
mindat.org URL:
https://www.mindat.org/min-39560.html
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References for Paraershovite
Reference List:
Khomyakov, A. P., Camara, F., Sokolova, E., Abdu, Y., Hawthorne, F. C. (2010) Paraershovite, Na3K3Fe3+2(Si4O10OH)2(OH)2(H2O)4, a new mineral species from the Khibina Alkaline massif, Kola Peninsula, Russia: Description and crystal structure. The Canadian Mineralogist, 48 (2) 279-290 doi:10.3749/canmin.48.2.279
Localities for Paraershovite
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) | |
| Khomyakov et al. (2010) |
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Yukspor Mt, Khibiny Massif, Murmansk Oblast, Russia