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Thomsonite-Sr

A valid IMA mineral species
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About Thomsonite-SrHide

03528690017271927359479.jpg
Thomas Thomson
Formula:
Na(Sr,Ca)2[Al5Si5O20] · 7H2O
Colour:
Colorless
Lustre:
Vitreous
Hardness:
5
Specific Gravity:
2.47
Crystal System:
Orthorhombic
Name:
Named as the Sr-dominant analogue of thomsonite-Ca.

The root name thomsonite is in honor of Thomas Thomson (12 April 1773 Crieff, Perthshire, Scotland - 2 July 1852 Kilmun, Argyleshire, Scotland), professor of chemistry at the University of Glasgow. Thomson was an indefatigable mineral chemist and contributed enormously to the number of accurate chemical analyses of minerals during his career as well as having discovered many new mineral species.
Zeolite Group.
The strontium analogue of Thomsonite-Ca.


Unique IdentifiersHide

Mindat ID:
28899
Long-form identifier:
mindat:1:1:28899:6

IMA Classification of Thomsonite-SrHide

Approved
IMA Formula:
NaSr2Al5Si5O20·6-7H2O
Approval year:
2000
First published:
2001

Classification of Thomsonite-SrHide

9.GA.10

9 : SILICATES (Germanates)
G : Tektosilicates with zeolitic H2O; zeolite family
A : Zeolites with T5O10 Units – The Fibrous Zeolites

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.

SymbolSourceReference for Standard
Thm-SrIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43
TmpKretz (1983)Kretz, R. (1983) Symbols of rock-forming minerals. American Mineralogist, 68, 277–279.
ThmWhitney & Evans (2010)Whitney, D.L. and Evans, B.W. (2010) Abbreviations for names of rock-forming minerals. American Mineralogist, 95, 185–187 doi:10.2138/am.2010.3371
ThmThe Canadian Mineralogist (2019)The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download

Physical Properties of Thomsonite-SrHide

Vitreous
Transparency:
Transparent
Colour:
Colorless
Streak:
White
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
[100] Perfect, [010] Good
Density:
2.47 g/cm3 (Measured)    2.62 g/cm3 (Calculated)

Optical Data of Thomsonite-SrHide

Type:
Biaxial (+)
RI values:
nα = 1.528 nβ = 1.532 nγ = 1.54
2V:
Measured: 62° , Calculated: 72°
Max. Birefringence:
δ = 0.012
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.

Surface Relief:
None to Very Low
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.
Dispersion:
weak, r > v
Optical Extinction:
X = a, Y = c, Z = b.
Pleochroism:
Non-pleochroic

Chemistry of Thomsonite-SrHide

Mindat Formula:
Na(Sr,Ca)2[Al5Si5O20] · 7H2O
Element Weights:
Element% weight
O46.972 %
Sr19.055 %
Si15.270 %
Al14.669 %
Na2.500 %
H1.534 %

Calculated from ideal end-member formula.
O
Sr
Si
Al
Na
H

Crystallography of Thomsonite-SrHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Cell Parameters:
a = 13.050 Å, b = 13.123 Å, c = 13.241 Å
Ratio:
a:b:c = 0.994 : 1 : 1.009
Unit Cell V:
2,267.59 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Forms: {100}, {010}, {0О1}, {110}.
Twinning:
None observed.
Comment:
Non-standard space-group setting Pcnn.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0012495Thomsonite-SrGurbanova O A, Rastsvetaeva R K, Pekov I V, Turchkova A G (2001) Crystal structure of strontium-rich thomsonite Doklady Akademii Nauk SSSR 376 387-3902001Khibiny alkaline massif, Kola peninsula, Russia0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Loading XRD data...
Data Set:
Data courtesy of RRUFF project at University of Arizona, used with permission.
Powder Diffraction Data:
d-spacingIntensity
2.691 Å(100)
2.86 Å(100)
2.96 Å(100)
3.49 Å(90)
3.19 Å(80)
4.66 Å(80)
6.63 Å(70)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
22 : Hydration and low-? subsurface aqueous alteration (see also #23)

Type Occurrence of Thomsonite-SrHide

General Appearance of Type Material:
Euhedral prismatic crystals up to 1.0 x 0.2 x 0.2 mm (Rasvumchorr) and zones up to 0.02 mm (Yuksporr).
Place of Conservation of Type Material:
A.E. Fersman Mineralogical Museum, Moscow, Russia.
Geological Setting of Type Material:
In veinlets cross-cutting natrolite of risschorrite pegmatite (Rasvumchorr). In a veinlet cross-cutting urtite, as zones in thomsonite-Ca (Yuksporr).
Associated Minerals at Type Locality:

Synonyms of Thomsonite-SrHide

Other Language Names for Thomsonite-SrHide

Simplified Chinese:锶杆沸石
Traditional Chinese:锶桿沸石

Relationship of Thomsonite-Sr to other SpeciesHide

Other Members of Thomsonite Subgroup:
Thomsonite-CaNaCa2[Al5Si5O20] · 6H2OOrth. mmm(2/m2/m2/m)

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Thomsonite-Sr associated with MesoliteNa2Ca2Si9Al6O30 · 8H2O
1 photo of Thomsonite-Sr associated with Thomsonite-CaNaCa2[Al5Si5O20] · 6H2O
1 photo of Thomsonite-Sr associated with Smectite GroupA0.3D2-3[T4O10]Z2 · nH2O
1 photo of Thomsonite-Sr associated with PrehniteCa2Al2Si3O10(OH)2

Related Minerals - Strunz-mindat GroupingHide

9.GA.05ScoleciteCaAl2Si3O10 · 3H2OMon. m : Bb
9.GA.05ParanatroliteNa2Al2Si3O10 · 3H2OMon. m : Bb
9.GA.05MesoliteNa2Ca2Si9Al6O30 · 8H2OOrth. mm2 : Fdd2
9.GA.05NatroliteNa2Al2Si3O10 · 2H2OOrth. mm2 : Fdd2
9.GA.05Gonnardite(Na,Ca)2(Si,Al)5O10 · 3H2OOrth.
9.GA.10Thomsonite-CaNaCa2[Al5Si5O20] · 6H2OOrth. mmm(2/m2/m2/m)
9.GA.15EdingtoniteBa[Al2Si3O10] · 4H2OOrth. 222 : P212121
9.GA.15KalborsiteK6Al4BSi6O20(OH)4ClTet. 42m : P421c
9.GA.15ArzamastseviteK6Al5Si6O20(OH)4ClTet. 42m : I42m

Other InformationHide

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 Thomsonite-SrHide

References for Thomsonite-SrHide

Localities for Thomsonite-SrHide

Showing 5 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- 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.
Japan
 
  • Niigata Prefecture
... +1 other reference
      • Ōmi
Miyajima (1999)
Myanmar
 
  • Kachin State
    • Mohnyin District
      • Hpakant Township (Hpakan; Phakant; Phakan)
Shi et al. (2012)
Russia (TL)
 
  • Murmansk Oblast
Pekov et al. (2001) +1 other reference
Pekov et al. (2001) +1 other reference
 
and/or  
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