Parakeldyshite
A valid IMA mineral species
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About Parakeldyshite
Formula:
Na2ZrSi2O7
Colour:
White, pale blue
Lustre:
Vitreous
Hardness:
5½ - 6
Specific Gravity:
3.37 - 3.39
Crystal System:
Triclinic
Name:
Named for its chemical relationship to keldyshite.
This page provides mineralogical data about Parakeldyshite.
Unique Identifiers
Mindat ID:
3094
Long-form identifier:
mindat:1:1:3094:2
GUID
(UUID V4):
(UUID V4):
3a05b080-b06f-4448-bcdc-edf3b65b2d6e
IMA Classification of Parakeldyshite
Approved
First published:
1977
Classification of Parakeldyshite
9.BC.10
9 : SILICATES (Germanates)
B : Sorosilicates
C : Si2O7 groups, without non-tetrahedral anions; cations in octahedral [6] and greater coordination
9 : SILICATES (Germanates)
B : Sorosilicates
C : Si2O7 groups, without non-tetrahedral anions; cations in octahedral [6] and greater coordination
55.2.2.3
55 : SOROSILICATES Si2O7 Groups,Generally with no Additional Anions
2 : Si2O7 Groups, Generally with no Additional Anions with cations in [6] coordination
55 : SOROSILICATES Si2O7 Groups,Generally with no Additional Anions
2 : Si2O7 Groups, Generally with no Additional Anions with cations in [6] coordination
14.10.4
14 : Silicates not Containing Aluminum
10 : Silicates of Zr or Hf
14 : Silicates not Containing Aluminum
10 : Silicates of Zr or Hf
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 |
---|---|---|
Pkel | 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 Parakeldyshite
Vitreous
Colour:
White, pale blue
Hardness:
5½ - 6 on Mohs scale
Cleavage:
Perfect
Three cleavages result in a pseudo-rhombohedral shape: {001} perfect, {110} and {110} somewhat less perfect. The acute angles between these planes are all between 76° and 82°. Also a good cleavage parallel to {011}.
Three cleavages result in a pseudo-rhombohedral shape: {001} perfect, {110} and {110} somewhat less perfect. The acute angles between these planes are all between 76° and 82°. Also a good cleavage parallel to {011}.
Density:
3.37 - 3.39 g/cm3 (Measured) 3.40 g/cm3 (Calculated)
Optical Data of Parakeldyshite
Type:
Biaxial (-)
RI values:
nα = 1.670 nβ = 1.692 - 1.697 nγ = 1.713 - 1.718
2V:
Measured: 83° to 84°, Calculated: 88°
Max Birefringence:
δ = 0.043 - 0.048
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:
High
Dispersion:
r > v strong
Optical Extinction:
Y ≈ c; X ≈ b; Z ≈ a.
Chemistry of Parakeldyshite
Mindat Formula:
Na2ZrSi2O7
Elements listed:
Common Impurities:
Ti,Hf,Al,Fe,Mg,Ca,K,H2O
Crystallography of Parakeldyshite
Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 5.419(1) Å, b = 6.607(2) Å, c = 8.806(2) Å
α = 71.50(2)°, β = 87.15(3)°, γ = 85.63(2)°
α = 71.50(2)°, β = 87.15(3)°, γ = 85.63(2)°
Ratio:
a:b:c = 0.82 : 1 : 1.333
Unit Cell V:
298.01 ų (Calculated from Unit Cell)
Z:
2
Twinning:
Polysynthetic on {100}, with several other sets intersecting.
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) |
---|---|---|---|---|---|---|---|
0018674 | Parakeldyshite | Pekov I V, Zubkova N V, Pushcharovsky D Y, Kolitsch U, Tillmanns E (2007) Refined crystal structure of parakeldyshite and genetic crystal chemistry of zirconium minerals with [Si2O7] diorthogroups Crystallography Reports 52 1066-1071 | 2007 | Alluaiv Mountain (Lovozero), Kola Peninsula, Russia | 0 | 293 | |
0014056 | Parakeldyshite | Voronkov A A, Shumyatskaya N G, Pyatenko Y A (1970) Crystal structure of a new natural modification of Na2Zr[Si2O7] Journal of Structural Chemistry 11 866-867 | 1970 | synthetic | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.963 Å | (10) |
2.913 Å | (9) |
4.234 Å | (7) |
2.703 Å | (7) |
6.00 Å | (6) |
2.718 Å | (6) |
2.905 Å | (5) |
Comments:
Bratthagen, Norway. Data from Raade and Mladeck (1977).
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 Parakeldyshite
Co-Type Localities:
General Appearance of Type Material:
Grains to 5 mm and aggregates.
Place of Conservation of Type Material:
Geology Museum, Kola Branch, Academy of Sciences, Apatity, 3270, 4457; Mining Institute, St. Petersburg, 1079/1{2, vis4361; Vernadsky Geological Museum, Moscow, 517151; A.E. Fersman Mineralogical Museum, Academy of Sciences, Moscow, Russia, 78461, 78462
Associated Minerals at Type Locality:
Reference:
Sizova R G, Kuz'min E A, Ilyukhin V V (1975) Deciphering the continuous Patterson function of the Na,Zr-diorthosilicate Na2ZrSi2O7 (parakeldyshite) by the vector subsystem method. Konstitutsiya i Svoistva Mineralov 9, 10-12
Synonyms of Parakeldyshite
Other Language Names for Parakeldyshite
Common Associates
Associated Minerals Based on Photo Data:
18 photos of Parakeldyshite associated with Keldyshite | (Na,H)2ZrSi2O7 |
8 photos of Parakeldyshite associated with Aegirine | NaFe3+Si2O6 |
8 photos of Parakeldyshite associated with Kentbrooksite | (Na,REE)15(Ca,REE)6(Mn2+,Fe2+)3Zr3Nb[Si25O74]F2 · 2H2O |
5 photos of Parakeldyshite associated with Sodalite | Na4(Si3Al3)O12Cl |
4 photos of Parakeldyshite associated with Albite | Na(AlSi3O8) |
2 photos of Parakeldyshite associated with Nepheline | Na3K(Al4Si4O16) |
1 photo of Parakeldyshite associated with Lorenzenite | Na2Ti2(Si2O6)O3 |
1 photo of Parakeldyshite associated with Loparite-(Ce) | (Na,REE)2Ti2O6 |
1 photo of Parakeldyshite associated with Catapleiite | Na2Zr(Si3O9) · 2H2O |
1 photo of Parakeldyshite associated with Eudialyte | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 |
Related Minerals - Strunz-mindat Grouping
9.BC. | Kozłowskiite | Ca4Fe2+2Sn3(Si2O7)2(Si2O6OH)2 |
9.BC. | Anorthoyttrialite-(Y) | Y4(SiO4)(Si3O10) |
9.BC.05 | Gittinsite | CaZrSi2O7 |
9.BC.05 | Keiviite-(Y) | Y2Si2O7 |
9.BC.05 | Keiviite-(Yb) | Yb2Si2O7 |
9.BC.05 | Thortveitite | Sc2Si2O7 |
9.BC.05 | Yttrialite-(Y) | (Y,Th)2Si2O7 |
9.BC.10 | Keldyshite | (Na,H)2ZrSi2O7 |
9.BC.10 | Khibinskite | K2ZrSi2O7 |
9.BC.15 | Rankinite | Ca3Si2O7 |
9.BC.20 | Barysilite | Pb8Mn2+[Si2O7]3 |
9.BC.25 | Edgarbaileyite | [Hg2]2+3[Si2O7] |
9.BC.30 | Kristiansenite | Ca4Sc2Sn2(Si2O7)2(Si2O6OH)2 |
9.BC.30 | Silesiaite | Ca4Fe3+2Sn2(Si2O7)2(Si2O6OH)2 |
9.BC.35 | Percleveite-(Ce) | Ce2Si2O7 |
9.BC.35 | Percleveite-(La) | La2Si2O7 |
9.BC.40 | Scottyite | BaCu2Si2O7 |
Fluorescence of Parakeldyshite
Fluoresces deep cream under SW UV and a very weak cream under LW UV.
Other Information
Special Storage/
Display Requirements:
Display Requirements:
Alters readily to a snow-white coating.
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 Parakeldyshite
mindat.org URL:
https://www.mindat.org/min-3094.html
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References for Parakeldyshite
Localities for Parakeldyshite
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.
Canada | |
| 166-175. +2 other references |
Germany | |
| Skrzyńska et al. (2023) |
Norway | |
| Raade et al. (1977) |
Russia | |
| Pavel.M. Kartashov (n.d.) |
Yakovenchuk et al. (2019) | |
Arzamastsev et al. (2008) | |
| Pekov (1998) |
| Pekov (1998) |
| Pekov (2003) |
Pavel.M. Kartashov (n.d.) | |
Pakhomovsky et al. (2014) | |
Petrovsky et al. (2012) | |
Pekov (1998) | |
South Africa | |
| Kamenetsky et al. (2014) |
| R. Liferovich - L. Horváth p.c. (2004) |
USA | |
| Prof. W. Stoll (pers. comm. 2004) +8 other references |
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Bratthagen 1, Lågendalen, Hedrum, Larvik, Vestfold, Norway