Steacyite (original) (raw)
A valid IMA mineral species
About SteacyiteHide
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Formula:
K0.3(Na,Ca)2ThSi8O20
Colour:
Gray, dark brown, green, beige
Lustre:
Vitreous, Greasy, Dull
Crystal System:
Tetragonal
Name:
Named in 1982 by Guy Perrault and Jan T. Szymaňski in honor of Harold Robert Steacy [June 7, 1923 Ottawa, Ontario, Canada - April 7, 2012 Ottawa, Ontario, Canada], mineralogist, former Curator of the National Mineral Collection, Geological Survey of Canada, for his contributions to Canadian mineralogy.
This page provides mineralogical data about Steacyite.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:3754:5
e30a4d1b-af89-47ed-be55-4dc4d1a94991
IMA Classification of SteacyiteHide
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IMA Formula:
K0.3(Na,Ca)2ThSi8O20
Classification of SteacyiteHide
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9.CH.10
9 : SILICATES (Germanates)
C : Cyclosilicates
H : [Si4O12]8- 4-membered double rings
63.1.1.1
63 : CYCLOSILICATES Condensed Rings
1 : Condensed Rings (Steacyite group)
14.16.15
14 : Silicates not Containing Aluminum
16 : Silicates of U
Mineral SymbolsHide
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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.
Symbol | Source | Reference |
---|---|---|
Scy | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Stc | The 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 SteacyiteHide
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Transparency:
Translucent, Opaque
Colour:
Gray, dark brown, green, beige
Density:
2.95 g/cm3 (Measured) 3.32 g/cm3 (Calculated)
Comment:
Measured on porous material.
Optical Data of SteacyiteHide
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RI values:
_n_ω = 1.573 _n_ε = 1.572
δ = 0.001
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Chemistry of SteacyiteHide
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Mindat Formula:
K0.3(Na,Ca)2ThSi8O20
Common Impurities:
As,Mn,Pb,F,P
Crystallography of SteacyiteHide
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Crystal System:
Tetragonal
Class (H-M):
4/m m m _(_4/_m_2/_m_2/m ) - Ditetragonal Dipyramidal
Cell Parameters:
a = 7.58 Å, c = 14.76 Å
Unit Cell V:
848.06 ų (Calculated from Unit Cell)
Morphology:
Elongated along [001] and showing only the forms {100} and {001}.
Twinning:
Cruciform, by 90° rotation about [010].
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0018511 | Steacyite | Prichard P, Perrault G (1972) Structure cristalline de l'ekanite de St-Hilaire, P.Q. Acta Crystallographica B28 1994-1999 | 1972 | Mont St-Hilaire, Quebec, Canada | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.38 Å | (100) |
3.32 Å | (55) |
5.30 Å | (45) |
2.64 Å | (41) |
2.00 Å | (26) |
1.82 Å | (20) |
2.16 Å | (19) |
Geological EnvironmentHide
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Type Occurrence of SteacyiteHide
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General Appearance of Type Material:
Elongated crystals to 2 mm.
Place of Conservation of Type Material:
Ecole Polytechnique, Montreal, Quebec, Canada, number 12480.
Canadian Geological Survey, Ottawa, Ontario, Canada, number 61529.
Canadian Museum of Nature, Ottawa, Canada.
National Museum of Natural History, Washington, D.C., USA, number 149820.
The Natural History Museum, London, England, number 1970,168.
Geological Setting of Type Material:
In pegmatite veins in nepheline syenite.
Associated Minerals at Type Locality:
Synonyms of SteacyiteHide
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Other Language Names for SteacyiteHide
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Relationship of Steacyite to other SpeciesHide
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Other Members of this group:
Arapovite | (K1-x◻x)(Ca,Na)2U4+Si8O20 (x ~ 0.5) | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m c c |
---|---|---|
Iraqite-(La) | KCa2(La,Ce,Th)Si8O20 | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m c c |
Turkestanite | (K,◻)(Ca,Na)2ThSi8O20 · nH2O | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m c c |
Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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9.CH.05 | Hyalotekite | (Ba,Pb,K)4(Ca,Y)2(B,Be)2(Si,B)2Si8O28(F,Cl) | Tric. 1 : _P_1 |
---|---|---|---|
9.CH.05 | Kapitsaite-(Y) | (Ba,K,Pb)4(Y,Ca)2Si8(B,Si)4O28F | Tric. 1 : _P_1 |
9.CH.05 | Itsiite | Ba4Ca2[Si8B4O28]◻ | Tet. 42_m_ : I_42_m |
9.CH.05 | Khvorovite | (Pb,Ba,K)4Ca2[Si8B2(Si,B)2O28]F | Tric. |
9.CH.10 | Iraqite-(La) | KCa2(La,Ce,Th)Si8O20 | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m c c |
9.CH.10 | Turkestanite | (K,◻)(Ca,Na)2ThSi8O20 · nH2O | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m c c |
9.CH.10 | Arapovite | (K1-x◻x)(Ca,Na)2U4+Si8O20 (x ~ 0.5) | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m c c |
Other InformationHide
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Notes:
Radioactive. Emits α and β particles, but not γ radiation.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Steacyite in petrologyHide
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Internet Links for SteacyiteHide
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References for SteacyiteHide
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Reference List:
Szymański, J. T., Owens, D. R., Roberts, A. C., Ansell, H. G., Chao, G. Y. (1982) A mineralogical study and crystal structure determination of nonmetamict ekanite ThCa2Si8O20. The Canadian Mineralogist, 20 (1) 65-75
Localities for SteacyiteHide
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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.
Locality ListHide
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- 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.