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Tsaregorodtsevite
A valid IMA mineral species
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About Tsaregorodtsevite
Formula:
(N(CH3)4)(AlSi5O12)
Colour:
Colourless to white
Lustre:
Vitreous
Hardness:
6
Specific Gravity:
2.04
Crystal System:
Orthorhombic
Member of:
Name:
Named after Sergei Vasil'evich Tsaregorodtsev (Сергей Васильевич Царегородцев) (1953-1986), Russian mineral collector of the Urals.
Sodalite Group. The mineral contains (as the only one known) the tetramethylammonium ion, [N(CH3)4]+.
Unique Identifiers
Mindat ID:
4034
Long-form identifier:
mindat:1:1:4034:7
IMA Classification of Tsaregorodtsevite
Approved
IMA Formula:
(N(CH3)4)1+Si4(SiAl)O12
Approval year:
1991
First published:
1993
Classification of Tsaregorodtsevite
9.FB.10
9 : SILICATES (Germanates)
F : Tektosilicates without zeolitic H2O
B : Tektosilicates with additional anions
9 : SILICATES (Germanates)
F : Tektosilicates without zeolitic H2O
B : Tektosilicates with additional anions
76.2.3.8
76 : TECTOSILICATES Al-Si Framework
2 : Al-Si Framework Feldspathoids and related species
76 : TECTOSILICATES Al-Si Framework
2 : Al-Si Framework Feldspathoids and related species
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 |
|---|---|---|
| Tsa | 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 Tsaregorodtsevite
Vitreous
Transparency:
Transparent
Colour:
Colourless to white
Streak:
White
Hardness:
6 on Mohs scale
Hardness:
VHN120=796 - 893 kg/mm2 - Vickers
Tenacity:
Brittle
Fracture:
Conchoidal
Density:
2.04(5) g/cm3 (Measured) 2.01 g/cm3 (Calculated)
Optical Data of Tsaregorodtsevite
Type:
Biaxial (-)
RI values:
nα = 1.529(2) nγ = 1.531(2)
2V:
Measured: 76° (5)
Max. Birefringence:
δ = 0.002
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:
None to Very Low
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:
none
Chemistry of Tsaregorodtsevite
Mindat Formula:
(N(CH3)4)(AlSi5O12)
Element Weights:
Crystallography of Tsaregorodtsevite
Crystal System:
Orthorhombic
Class (H-M):
222 - Disphenoidal
Space Group:
I222
Cell Parameters:
a = 8.984(3) Å, b = 8.937(2) Å, c = 8.927(2) Å
Ratio:
a:b:c = 1.005 : 1 : 0.999
Unit Cell V:
716.75 ų (Calculated from Unit Cell)
Z:
2
Twinning:
Commonly sector twinned, as seen in thin section.
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) |
|---|---|---|---|---|---|---|---|
| 0020490 | Tsaregorodtsevite | Sokolova E V, Rybakov V B, Pautov L A (1991) The crystal structure of a new natural tetramethylammonium aluminosilicate [N(CH3)4][Si2(Si0.5Al0.5)O6]2 Soviet Physics Doklady 36 267-269 | 1991 | Northern Ural Mountains, Mankhambo region, Russia | 0 | 293 | |
| 0012488 | Tsaregorodtsevite | Sokolova E V, Rybakov V B, Pautov L A, Pushcharovsky D Yu (1993) Structural changes in tsaregorodtsevite Doklady Akademii Nauk SSSR 332 309-312 | 1993 | 0 | 293 | ||
| 0012489 | Tsaregorodtsevite | Sokolova E V, Rybakov V B, Pautov L A, Pushcharovsky D Yu (1993) Structural changes in tsaregorodtsevite Doklady Akademii Nauk SSSR 332 309-312 | 1993 | 0 | 1143 | ||
| 0012490 | Tsaregorodtsevite | Sokolova E V, Rybakov V B, Pautov L A, Pushcharovsky D Yu (1993) Structural changes in tsaregorodtsevite Doklady Akademii Nauk SSSR 332 309-312 | 1993 | 0 | 1243 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Loading XRD data...
Data courtesy of RRUFF project at University of Arizona, used with permission.
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 3.66 Å | (100) |
| 4.46 Å | (82) |
| 6.33 Å | (60) |
| 2.586 Å | (15) |
| 4.50 Å | (12b) |
| 3.16 Å | (12) |
| 2.832 Å | (10) |
Comments:
very close to ammonian sodalite
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 5: Initiation of plate tectonics | <3.5-2.5 |
| 40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | |
| Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere | <0.6 |
| 53 : Other minerals with taphonomic origins | <0.4 |
Type Occurrence of Tsaregorodtsevite
General Appearance of Type Material:
Pseudocubic crystals, to 1 cm
Place of Conservation of Type Material:
Mining Institute, St. Petersburg, 2054/1; Il'menskii Preserve Museum, Miass, 3303, 3374, 5121; Vernadsky Geological Museum, Moscow, 59719, 59859; A.E. Fersman Mineralogical Museum, Academy of Sciences, Moscow, Russia, 87949; National Museum, Sofint5a, Bulgaria; National Museum, Prague, Czech Republic.
Synonyms of Tsaregorodtsevite
Other Language Names for Tsaregorodtsevite
Relationship of Tsaregorodtsevite to other Species
Member of:
Other Members of Sodalite Group:
| Bolotinaite | (Na7◻)(Al6Si6O24)F · 4H2O | Iso. 43m : I43m |
| Haüyne | Na3Ca(Si3Al3)O12(SO4) | Iso. 43m : P43n |
| Lazurite | Na7Ca(Al6Si6O24)(SO4)(S3) · H2O | Iso. 43m : P43n |
| Nosean | Na8(Al6Si6O24)(SO4) · H2O | Iso. 43m : P43n |
| Sapozhnikovite | Na8(Al6Si6O24)(HS)2 | Iso. 43m : P43n |
| Slyudyankaite | Na28Ca4(Si24Al24O96)(SO4)6(S6)1/3(CO2) · 2H2O | Tric. 1 : P1 |
| Sodalite | Na4(Si3Al3)O12Cl | Iso. 43m : P43n |
| Vladimirivanovite | Na6Ca2(Al6Si6O24)(SO4,S3,S2,Cl)2 · H2O | Orth. mmm(2/m2/m2/m) |
Common Associates
Associations Based on Photo Data:
| 3 photos of Tsaregorodtsevite associated with Quartz | SiO2 |
| 1 photo of Tsaregorodtsevite associated with 'Muscovite-chlorite schist' | |
| 1 photo of Tsaregorodtsevite associated with Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
| 1 photo of Tsaregorodtsevite associated with Anatase | TiO2 |
Related Minerals - Strunz-mindat Grouping
| 9.FB. | Perchukite-(Y) | PbYAsSi2O8 |
| 9.FB. | Åsgruvanite-(Ce) | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| 9.FB. | Steudelite | Na3(K17Ca7)Ca4(Al24Si24O96)(SO3)6F6 · 4H2O |
| 9.FB. | Wenlanzhangite-(Y) | Y2V3+2V4+2(SiO4)2O4(OH)4 |
| 9.FB. | Slyudyankaite | Na28Ca4(Si24Al24O96)(SO4)6(S6)1/3(CO2) · 2H2O |
| 9.FB. | Bolotinaite | (Na7◻)(Al6Si6O24)F · 4H2O |
| 9.FB. | Sapozhnikovite | Na8(Al6Si6O24)(HS)2 |
| 9.FB. | Betzite | Na6Ca2(Al6Si6O24)Cl4 |
| 9.FB.05 | Quadridavyne | (Na,K)6Ca2(Al6Si6O24)Cl4 |
| 9.FB.05 | Sulfhydrylbystrite | Na5K2Ca[Al6Si6O24](S5)2(SH) |
| 9.FB.05 | Marinellite | (Na,K)42Ca6(Al6Si6O24)6(SO4)8Cl2 · 3H2O |
| 9.FB.05 | Afghanite | (Na,K)22Ca10(Si24Al24O96)(SO4)6Cl6 |
| 9.FB.05 | Bystrite | (Na,K)7Ca(Al6Si6O24)(S5)Cl |
| 9.FB.05 | Franzinite | (Na,K)6Ca2(Al6Si6O24)(SO4)2 · 0.5H2O |
| 9.FB.05 | Kyanoxalite | Na7(Al6-xSi6+xO24)(C2O4)0.5+x · 5H2O (0 < x < 0.5) |
| 9.FB.05 | Vishnevite | (Na,K)8(Al6Si6O24)(SO4,CO3) · 2H2O |
| 9.FB.05 | Farneseite | (Na,Ca,K)56(Al6Si6O24)7(SO4)12 · 6H2O |
| 9.FB.05 | Alloriite | (Na,Ca,K)26Ca4(Al6Si6O24)4(SO4)6Cl6 |
| 9.FB.05 | Liottite | (Na,K)16Ca8(Al6Si6O24)3(SO4)5Cl4 |
| 9.FB.05 | Depmeierite | Na8(Al6Si6O24)(PO4,CO3)1-x · 3H2O (x<0.5) |
| 9.FB.05 | Biachellaite | (Na,Ca,K)8(Al6Si6O24)(SO4)2(OH)0.5 · H2O |
| 9.FB.05 | Cancrinite | (Na,Ca,◻)8(Al6Si6O24)(CO3,SO4)2 · 2H2O |
| 9.FB.05 | Cancrisilite | Na7(Al5Si7O24)(CO3) · 3H2O |
| 9.FB.05 | Fantappièite | [Na82.5Ca33K16.5](Si99Al99O396)(SO4)33 · 4H2O |
| 9.FB.05 | Carbobystrite | Na8(Al6Si6O24)(CO3) · 3.5H2O |
| 9.FB.05 | Microsommite | Na4K2Ca2(Al6Si6O24)(SO4)Cl2 |
| 9.FB.05 | Pitiglianoite | Na6K2(Al6Si6O24)(SO4) · 2H2O |
| 9.FB.05 | Tounkite | (Na,Ca,K)8(Si6Al6)O24(SO4)2Cl · 0.5H2O |
| 9.FB.05 | Balliranoite | (Na,K)6Ca2(Si6Al6O24)Cl2(CO3) |
| 9.FB.05 | Giuseppettite | (Na,K,Ca)7-8(Al6Si6O24)(SO4,Cl)1-2 |
| 9.FB.05 | Sacrofanite | (Na61K19Ca32)(Si84Al84O336)(SO4)26Cl2F6 · 2H2O |
| 9.FB.05 | Kircherite | Na5Ca2K(Al6Si6O24)(SO4)2 · 0.33H2O |
| 9.FB.05 | Hydroxycancrinite | Na8(Al6Si6O24)(OH)2 · 2H2O |
| 9.FB.05 | Davyne | (Na,K)6Ca2(Al6Si6O24)(Cl2,SO4)2 |
| 9.FB.10 | Haüyne | Na3Ca(Si3Al3)O12(SO4) |
| 9.FB.10 | Lazurite | Na7Ca(Al6Si6O24)(SO4)(S3) · H2O |
| 9.FB.10 | Danalite | Be3Fe2+4(SiO4)3S |
| 9.FB.10 | Helvine | Be3Mn2+4(SiO4)3S |
| 9.FB.10 | Kamaishilite | Ca2(Al2SiO6)(OH)2 |
| 9.FB.10 | Sodalite | Na4(Si3Al3)O12Cl |
| 9.FB.10 | Nosean | Na8(Al6Si6O24)(SO4) · H2O |
| 9.FB.10 | Genthelvite | Be3Zn4(SiO4)3S |
| 9.FB.10 | Bicchulite | Ca2(Al2SiO6)(OH)2 |
| 9.FB.10 | Vladimirivanovite | Na6Ca2(Al6Si6O24)(SO4,S3,S2,Cl)2 · H2O |
| 9.FB.10 | Tugtupite | (BeAlSi)Na4(SiO4)3Cl |
| 9.FB.15 | Marialite | Na4Al3Si9O24Cl |
| 9.FB.15 | Meionite | Ca4Al6Si6O24CO3 |
| 9.FB.15 | Silvialite | (Ca,Na)4(Al6Si6O24)(SO4,CO3) |
Other Information
Thermal Behaviour:
Evolves ammonia and eurotropine above 600°C, becoming pitch-black.
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 Tsaregorodtsevite
mindat.org URL:
https://www.mindat.org/min-4034.html
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References for Tsaregorodtsevite
Reference List:
Hassan, I., Grundy, H. D. (1984) The crystal structures of sodalite-group minerals. Acta Crystallographica Section B Structural Science, 40 (1) 6-13 doi:10.1107/s0108768184001683
Pautov, L. A., Karpenko, V. Y., Sokolova, E. V., Ignatenko, K. I. (1993) Tsaregorodtsevite N(CH3)4[Si2(Si0.5Al0.5)O6]2 — a new mineral. Zapiski Vserossijskogo Mineralogicheskogo Obshchestva, 122 (1) 128-135
Localities for Tsaregorodtsevite
Showing 3 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.
Poland | |
| Ł. Kruszewski (PXRD data) |
| Kruszewski (2012) |
Russia (TL) | |
| Pekov (1998) |
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The
Yaruta Mt, Man'-Khambo Mountains, Khanty-Mansi Autonomous Okrug, Russia