Astrophyllite
About Astrophyllite
The mineral was first found in 1844 by the Norwegian mineralogist Paul Christian Weibye (1819-1865) and later described by him, in 1848, as a brown, micaceous mineral ("brauner Glimmer") from Låven (formerly Lamöskjär), Langesundsfjorden, Norway (Weibye 1848). Later Scheerer (1854) described it under the name astrophyllite. Brøgger (1890) described in detail the crystallographic and optical properties as well as its chemistry.
Visit gemdat.org for gemological information about Astrophyllite.Unique Identifiers
IMA Classification of Astrophyllite
Classification of Astrophyllite
9 : SILICATES (Germanates)
D : Inosilicates
C : Inosilicates with branched 2-periodic single chains; Si2O6 + 2SiO3 Si4O12
69 : INOSILICATES Chains with Side Branches or Loops
1 : Chains with Side Branches or Loops with (P=2, and N=4, 2 branches)
14 : Silicates not Containing Aluminum
9 : Silicates of Ti
Mineral Symbols
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
| Symbol | Source | Reference |
|---|---|---|
| Ast | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
| Ast | The Canadian Mineralogist (2019) | The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download |
| Ast | Warr (2020) | Warr, L.N. (2020) Recommended abbreviations for the names of clay minerals and associated phases. Clay Minerals, 55, 261–264 doi:10.1180/clm.2020.30 |
Physical Properties of Astrophyllite
Perfect on {001}
Poor on {100}
Optical Data of Astrophyllite
Based on recorded range of RI values above.
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.
Y= orange-yellow
Z= lemon-yellow
Chemistry of Astrophyllite
Chemical Analysis
| 1 | |
|---|---|
| Na2O | 2.68 % |
| K2O | 5.21 % |
| Rb2O | 1.05 % |
| Cs2O | 1.35 % |
| CaO | 1.00 % |
| SrO | 0.10 % |
| MgO | 1.11 % |
| MnO | 13.99 % |
| FeO | 18.45 % |
| ZnO | 0.49 % |
| Al2O3 | 1.01 % |
| Ce2O3 | 0.31 % |
| TiO2 | 9.20 % |
| SnO3 | 0.23 % |
| ZrO2 | 1.69 % |
| Nb2O5 | 2.81 % |
| SiO2 | 33.98 % |
| F | 1.38 % |
| H2O | 2.65 % |
| O=F | -0.58 % |
| Total: | 98.11 % |
Crystallography of Astrophyllite
α = 113.019°, β = 94.578°, γ = 103.120°
Crystal Structure
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
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| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0005802 | Astrophyllite | Piilonen P C, McDonald A M, Lalonde A E (2003) Insights into astrophyllite-group minerals II: Crystal chemistry The Canadian Mineralogist 41 27-54 | ![]() | 2003 | Seal Lake, Labrador, Canada | 0 | 293 |
| 0005803 | Astrophyllite | Piilonen P C, McDonald A M, Lalonde A E (2003) Insights into astrophyllite-group minerals II: Crystal chemistry The Canadian Mineralogist 41 27-54 | ![]() | 2003 | Langesundsfjord area, Oslo Rift Valley, Norway | 0 | 293 |
| 0005805 | Astrophyllite | Piilonen P C, McDonald A M, Lalonde A E (2003) Insights into astrophyllite-group minerals II: Crystal chemistry The Canadian Mineralogist 41 27-54 | ![]() | 2003 | Khibina massif, Kola Peninsula, Russia | 0 | 293 |
| 0005806 | Astrophyllite | Piilonen P C, McDonald A M, Lalonde A E (2003) Insights into astrophyllite-group minerals II: Crystal chemistry The Canadian Mineralogist 41 27-54 | ![]() | 2003 | Khibina massif, Kola Peninsula, Russia | 0 | 293 |
| 0005809 | Astrophyllite | Piilonen P C, McDonald A M, Lalonde A E (2003) Insights into astrophyllite-group minerals II: Crystal chemistry The Canadian Mineralogist 41 27-54 | ![]() | 2003 | granitic pegmatite at Mount Rosa, Pikes Peak, Colorado, USA | 0 | 293 |
| 0005818 | Astrophyllite | Piilonen P C, McDonald A M, Lalonde A E (2003) Insights into astrophyllite-group minerals II: Crystal chemistry The Canadian Mineralogist 41 27-54 | ![]() | 2003 | aplite/pegmatite at Mont Saint-Hilaire, Quebec, Canada | 0 | 293 |
| 0005819 | Astrophyllite | Piilonen P C, McDonald A M, Lalonde A E (2003) Insights into astrophyllite-group minerals II: Crystal chemistry The Canadian Mineralogist 41 27-54 | ![]() | 2003 | nepheline syenite pegmatite at Mont Saint-Hilaire, Quebec, Canada | 0 | 293 |
| 0007257 | Astrophyllite | Sokolova E, Camara F (2008) Re-investigation of the crystal structure of magnesium astrophyllite European Journal of Mineralogy 20 253-260 | 2008 | Mt. Yukspor, Khibina alkaline massif, Kola Peninsula, Russia | 0 | 293 | |
| 0009310 | Astrophyllite | Woodrow P J (1967) The crystal structure of astrophyllite Acta Crystallographica 22 673-678 | ![]() | 1967 | El Paso County, Colorado, USA | 0 | 293 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 10.6 Å | (100) |
| 3.51 Å | (80) |
| 2.77 Å | (60) |
| 2.64 Å | (60) |
| 2.57 Å | (60) |
| 9.82 Å | (30) |
| 1.76 Å | (30) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 4b: Highly evolved igneous rocks | >3.0 |
| 35 : Ultra-alkali and agpaitic igneous rocks |
Type Occurrence of Astrophyllite
Synonyms of Astrophyllite
Other Language Names for Astrophyllite
Relationship of Astrophyllite to other Species
| Bulgakite | Li2CaFe2+7Ti2[Si4O12]2O2(OH)4O(H2O)2 | Tric. 1 : P1 |
| Hydroastrophyllite | [H3O]+2CaFe2+7Ti2[Si4O12]2O2(OH)4O | Tric. |
| Nalivkinite | Li2NaFe2+7Ti2[Si4O12]2O2(OH)4F(H2O)2 | Tric. 1 : P1 |
| Niobophyllite | K2NaFe2+7(NbTi)[Si4O12]2O2(OH)4O | Tric. |
| Tarbagataite | (K◻)CaFe2+7Ti2[Si4O12]2O2(OH)4(OH) | Tric. 1 : P1 |
| Zircophyllite | K2NaFe2+7Zr2[Si4O12]2O2(OH)4F | Tric. |
Common Associates
| 118 photos of Astrophyllite associated with Aegirine | NaFe3+Si2O6 |
| 92 photos of Astrophyllite associated with Quartz | SiO2 |
| 42 photos of Astrophyllite associated with Microcline | K(AlSi3O8) |
| 38 photos of Astrophyllite associated with Albite | Na(AlSi3O8) |
| 36 photos of Astrophyllite associated with Feldspar Group | |
| 21 photos of Astrophyllite associated with Zircon | Zr(SiO4) |
| 18 photos of Astrophyllite associated with Ferro-katophorite | {Na}{CaNa}{Fe2+4Al}[(AlSi7)O22](OH)2 |
| 18 photos of Astrophyllite associated with Aenigmatite | Na4[Fe2+10Ti2]O4[Si12O36] |
| 17 photos of Astrophyllite associated with Leucophanite | NaCaBeSi2O6F |
| 16 photos of Astrophyllite associated with Eudialyte | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 |
Related Minerals - Strunz-mindat Grouping
| 9.DC. | Bulgakite | Li2CaFe2+7Ti2[Si4O12]2O2(OH)4O(H2O)2 |
| 9.DC.05 | Devitoite | Ba4Ba2Fe2+7Fe3+2[Si4O12]2[PO4]2[CO3]O2(OH)4◻2 |
| 9.DC.05 | Zircophyllite | K2NaFe2+7Zr2[Si4O12]2O2(OH)4F |
| 9.DC.05 | Nalivkinite | Li2NaFe2+7Ti2[Si4O12]2O2(OH)4F(H2O)2 |
| 9.DC.05 | Sveinbergeite | (H2O)2[Ca(H2O)](Fe2+6Fe3+)Ti2[Si4O12]2O2(OH)4[(OH)(H2O)] |
| 9.DC.05 | Niobophyllite | K2NaFe2+7(NbTi)[Si4O12]2O2(OH)4O |
| 9.DC.05 | Heyerdahlite | Na2NaMn2+7Ti2[Si4O12]2O2(OH)4F(H2O)2 |
| 9.DC.05 | Tarbagataite | (K◻)CaFe2+7Ti2[Si4O12]2O2(OH)4(OH) |
| 9.DC.05 | Hydroastrophyllite | [H3O]+2CaFe2+7Ti2[Si4O12]2O2(OH)4O |
| 9.DC.05 | Lobanovite | K2Na(Fe2+4Mg2Na)Ti2[Si4O12]2O2(OH)4◻ |
| 9.DC.05 | Niobokupletskite | K2NaMn2+7(NbTi)[Si4O12]2O2(OH)4O |
| 9.DC.05 | Kupletskite-(Cs) | Cs2NaMn2+7Ti2[Si4O12]2O2(OH)4F |
| 9.DC.05 | Kupletskite | K2NaMn2+7Ti2[Si4O12]2O2(OH)4F |
| 9.DC.05 | Laverovite | K2NaMn2+7Zr2[Si4O12]2O2(OH)4F |
Radioactivity
| Element | % Content | Activity (Bq/kg) | Radiation Type |
|---|---|---|---|
| Uranium (U) | 0.0000% | 0 | α, β, γ |
| Thorium (Th) | 0.0000% | 0 | α, β, γ |
| Potassium (K) | 5.9441% | 1,843 | β, γ |
For comparison:
- Banana: ~15 Bq per fruit
- Granite: 1,000–3,000 Bq/kg
- EU exemption limit: 10,000 Bq/kg
Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.
Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!
Activity: –
| Distance | Dose rate | Risk |
|---|---|---|
| 1 cm | ||
| 10 cm | ||
| 1 m |
The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).
D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield
Other Information
Internet Links for Astrophyllite
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References for Astrophyllite
Localities for Astrophyllite
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.






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Água de Pau Volcano, São Miguel, Azores, Portugal