Parsettensite
About Parsettensite
Compare also the chemically similar coombsite.
Unique Identifiers
IMA Classification of Parsettensite
Classification of Parsettensite
9 : SILICATES (Germanates)
E : Phyllosilicates
G : Double nets with 6-membered and larger rings
74 : PHYLLOSILICATES Modulated Layers
1 : Modulated Layers with joined islands
14 : Silicates not Containing Aluminum
17 : Silicates of Mn
Mineral Symbols
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
Symbol | Source | Reference |
---|---|---|
Psn | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Psn | 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 Parsettensite
[001] Perfect
Optical Data of Parsettensite
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.
Chemistry of Parsettensite
Previous, simplified formula: K1.2Mn8(Si,Al)12O26(OH)10.
Crystallography of Parsettensite
β = 135.60°
Crystal Structure
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0001653 | Parsettensite | Eggleton R A, Guggenheim S (1994) The use of electron optical methods to determine the crystal structure of a modulated phyllosilicate: Parsettensite American Mineralogist 79 426-437 | ![]() | 1994 | 0 | 293 |
X-Ray Powder Diffraction
d-spacing | Intensity |
---|---|
12.1 Å | (100) |
6.2 Å | (20) |
4.5 Å | (40) |
4.2 Å | (60) |
3.84 Å | (50) |
3.70 Å | (50) |
3.26 Å | (20) |
3.14 Å | (50) |
2.79 Å | (80) |
2.65 Å | (100) |
2.42 Å | (50) |
2.36 Å | (40) |
2.18 Å | (40) |
2.04 Å | (20) |
1.943 Å | (10) |
1.634 Å | (80) |
1.617 Å | (60) |
1.580 Å | (50) |
1.520 Å | (10) |
1.444 Å | (10) |
1.410 Å | (10) |
1.388 Å | (10) |
1.320 Å | (100) |
1.300 Å | (10) |
1.230 Å | (20) |
Geological Environment
Paragenetic Mode | Earliest Age (Ga) |
---|---|
High-𝑇 alteration and/or metamorphism | |
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits |
Type Occurrence of Parsettensite
The Natural History Museum, London, England.
Harvard University, Cambridge, Massachusetts, USA, 90497.
Synonyms of Parsettensite
Other Language Names for Parsettensite
Relationship of Parsettensite to other Species
Chalcodite | K(Fe3+,Mg,Fe2+)8(Si,Al)12(O,OH)27 | Tric. 1 : P1 |
Franklinphilite | (K,Na)4(Mn2+,Mg,Zn)48(Si,Al)72(O,OH)216 · 6H2O | Tric. |
Lennilenapeite | K6-7(Mg,Mn,Fe,Zn)48(Si,Al)72(O,OH)216 · 16H2O | Tric. |
Stilpnomelane | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O | Tric. 1 : P1 |
Common Associates
6 photos of Parsettensite associated with Albite | Na(AlSi3O8) |
5 photos of Parsettensite associated with Fluorapatite | Ca5(PO4)3F |
5 photos of Parsettensite associated with Neotocite | (Mn,Fe)SiO3 · H2O (?) |
4 photos of Parsettensite associated with Tinzenite | Ca2Mn2+4Al4[B2Si8O30](OH)2 |
4 photos of Parsettensite associated with Quartz | SiO2 |
2 photos of Parsettensite associated with Pyrite | FeS2 |
2 photos of Parsettensite associated with Rhodonite | CaMn3Mn[Si5O15] |
1 photo of Parsettensite associated with Braunite | Mn2+Mn3+6(SiO4)O8 |
1 photo of Parsettensite associated with Bikitaite | LiAlSi2O6 · H2O |
1 photo of Parsettensite associated with Lithiomarsturite | LiCaMn3Si5O14(OH) |
Related Minerals - Strunz-mindat Grouping
9.EG.05 | Cymrite | BaAl2Si2(O,OH)8 · H2O |
9.EG.10 | Naujakasite | (Na,K)6(Fe2+,Mn2+,Ca)(Al,Fe)4Si8O26 |
9.EG.10 | Manganonaujakasite | Na6(Mn2+,Fe2+)Al4Si8O26 |
9.EG.15 | Dmisteinbergite | Ca(Al2Si2O8) |
9.EG.20 | Kampfite | Ba12(Si11Al5)O31(CO3)8Cl5 |
9.EG.25 | Vertumnite | Ca4Al4Si4O6(OH)24 · 3H2O |
9.EG.25 | Strätlingite | Ca2Al2SiO7 · 8H2O |
9.EG.30 | Eggletonite | (Na,K,Ca)2(Mn,Fe)8(Si,Al)12O29(OH)7 · 11H2O |
9.EG.30 | Ganophyllite | (K,Na,Ca)2Mn8(Si,Al)12(O,OH)32 · 8H2O |
9.EG.30 | Tamaite | (Ca,K,Ba,Na)3-4Mn24(Si,Al)40(O,OH)112 · 21H2O |
9.EG.35 | Zussmanite | K(Fe,Mg,Mn)13(Si,Al)18O42(OH)14 |
9.EG.35 | Coombsite | KMn2+13(Si,Al)18O42(OH)14 |
9.EG.40 | Chalcodite | K(Fe3+,Mg,Fe2+)8(Si,Al)12(O,OH)27 |
9.EG.40 | Franklinphilite | (K,Na)4(Mn2+,Mg,Zn)48(Si,Al)72(O,OH)216 · 6H2O |
9.EG.40 | Lennilenapeite | K6-7(Mg,Mn,Fe,Zn)48(Si,Al)72(O,OH)216 · 16H2O |
9.EG.40 | Stilpnomelane | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
9.EG.45 | Latiumite | (Ca,K)4(Si,Al)5O11(SO4,CO3) |
9.EG.45 | Levantite | KCa3Al2(SiO4)(Si2O7)(PO4) |
9.EG.45 | Tuscanite | KCa6(Si,Al)10O22(SO4,CO3)2(OH) · H2O |
9.EG.50 | Jagoite | Pb18Fe3+4[Si4(Si,Fe3+)6][Pb4Si16(Si,Fe)4]O82Cl6 |
9.EG.50 | Friisite | Pb8Al3Si8O27Cl3 |
9.EG.55 | Wickenburgite | CaPb3Al2Si10O24(OH)6 |
9.EG.60 | Hyttsjöite | Pb18Ba2Ca5Mn2+2Fe3+2Si30O90Cl · 6H2O |
9.EG.65 | Armbrusterite | K5Na7Mn15[(Si9O22)4](OH)10 · 4H2O |
9.EG.70 | Roymillerite | Pb24Mg9(Si10O28)(CO3)10(BO3)(SiO4)(OH)13O5 |
9.EG.70 | Britvinite | [Pb7(OH)3F(BO3)2(CO3)][Mg4.5(OH)3(Si5O14)] |
9.EG.75 | Kayupovaite | Na2Mn10[(Si14Al2)O38(OH)8] · 7H2O |
9.EG.75 | UM1989-30-SiO:AlBaCaFeHKMgMn | (Ba,Ca)(Mn,Fe,Mg)22(Si,Al)32O76(OH)16 · 12H2O |
9.EG.75 | Bannisterite | (Ca,K,Na)(Mn2+,Fe2+)10(Si,Al)16O38(OH)8 · nH2O |
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) | 3.4242% | 1,062 | 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
Fluorescence of Parsettensite
Other Information
Internet Links for Parsettensite
Please feel free to link to this page.
References for Parsettensite
Localities for Parsettensite
Locality List




All localities listed without proper references should be considered as questionable.
China | |
| Jingfang Jin and Hui Jin (2000) |
| Pingyi Wan (2002) |
| Pingyi Wan (2002) |
| Pingyi Wan (2002) |
| Pingyi Wan (2002) |
Pingyi Wan (2002) | |
France | |
| De Ascenção Guedes et al. (2002) |
Indonesia | |
| Marcoux et al. (1993) +1 other reference |
Israel | |
| Krzątała et al. (2023) |
Italy | |
| Ricerche chimiche sulla tinzenite e parsettensite della miniera di Cassagna (Liguria) +1 other reference |
Cortesogno et al. (1979) | |
| Pipino (1984) |
| Dr. Uwe Kolitsch (EDS+XRD) |
| Piccoli (2002) +1 other reference |
| Martin et al. (1984) +3 other references |
| Piccoli et al. (2007) |
Japan | |
| Watanabe (1959) |
| Minerals Unlimited label from 1950s +1 other reference |
| Collection of NHM |
| Masutomi Museum specimen (Kyoto) +1 other reference |
Kazakhstan | |
| Brusnitsyn et al. (2021) |
New Zealand | |
| Sameshima et al. (1991) |
Romania | |
Hîrtopanu et al. (2003) +1 other reference | |
Russia | |
| Brusnitsyn et al. (2009) |
| Brusnitsyn (2006) |
| Brusnitsyn +3 other references |
| Sharygin et al. (2018) |
| Kassandrov et al. (2009) |
Kassandrov et al. (2009) | |
South Africa | |
| Pohl et al. (1991) |
Spain | |
| Jorge et al. (2005) |
Switzerland | |
| Geiger T. (1948) |
| Geiger T. (1948) |
Mandarino (2001) | |
| Schweiz.Min.Petr.Mitt. (1923) |
| Stalder et al. (1998) |
| Geiger T. (1948) +2 other references |
Geiger T. (1948) | |
Geiger T. (1948) +1 other reference | |
| Brugger et al. (1996) |
| Stalder et al. (1998) +1 other reference |
USA | |
| Mike Scott S105697 from Cureton FWZ ID ... |
| Muir Wood (1979) |
| Huebner +3 other references |
| Found Oct 2021 and optically studied. ... |
| Found in material from my 2019 ongoing ... +2 other references |
| White (1994) |
| Identical to parsettensite samples ... |
Smithsonian Institution Mineral ... |
Foote Lithium Co. Mine, Kings Mountain, Cleveland County, North Carolina, USA