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Unnamed (Mn3+-dominant analog of Sugilite)

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Formula:
KNa2(Mn3+,Fe3+,Al)2Li3Si12O30
Member of:
This page provides mineralogical data about Unnamed (Mn3+-dominant analog of Sugilite).


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Chemical Properties of Unnamed (Mn3+-dominant analog of Sugilite)Hide

Formula:
KNa2(Mn3+,Fe3+,Al)2Li3Si12O30
Idealised Formula:
KNa2Mn3+2Li3Si12O30

Chemical AnalysisHide

Oxide wt%:
 12
SiO272.48 %72.48 %
TiO20.08 %0.08 %
Al2O31.89 %1.89 %
Fe2O3*6.09 %6.09 %
MnO*7.04 % %
CaO0.00 %0.00 %
MgO0.00 %0.00 %
Na2O5.75 %5.75 %
K2O4.59 %4.59 %
BaO0.00 %0.00 %
Li2O**3 % %
H2O**1 % %
Mn2O3*** %7.83 %
Li2O# %4.2 %
Total:101.92 %102.91 %
Sample references:
IDLocalityReference
1Furumiya mine, Tobe-cho, Iyo district, Ehime Prefecture, Japananalysis #4 from Hirowatari, F. and Fukuoka, M. (1989) Some problems of the studies on the manganese minerals in Japan. Journal of the Mineralogical Society of Japan, 18, 347–365, https://doi.org/10.2465/gkk1952.18.347 *reported as **estimated
2  "  "re-calculation of analysis #4 from Hirowatari, F. and Fukuoka, M. (1989) based on Si=12 apfu normalization; Frank Mazdab re-normalization. *reported as ***calculated from measured Mn by charge balance #calculated from stoichiometry

Relationship of Unnamed (Mn3+-dominant analog of Sugilite) to other SpeciesHide

Member of:
Other Members of this group:
Agakhanovite-(Y)(YCa)□2KBe3Si12O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
AlmaruditeK(◻,Na)2(Mn,Fe,Mg)2[(Be,Al)3Si12]O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mmm
AluminosugiliteKNa2Al2Li3Si12O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
ArmeniteBaCa2Al6Si9O30 · 2H2OOrth. mmm (2/m 2/m 2/m) : Pnna
BerezanskiteKTi2Li3Si12O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
BrannockiteKSn2(Li3Si12)O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
ChayesiteK(Mg,Fe2+)4Fe3+[Si12O30]Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
DarapiositeKNa2Mn2(Li2ZnSi12)O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
DusmatoviteKK2Mn2(Zn2LiSi12)O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
EifeliteKNa3Mg4Si12O30Hex.
FriedrichbeckeiteK(◻Na)Mg2(Be2Mg)Si12O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
Klöchite(Fe2+Fe3+)◻2KZn3(Si12O30)Hex. 6/mmm (6/m 2/m 2/m) : P63/mmc
Merrihueite(K,Na)2(Fe2+,Mg)5Si12O30Hex.
MilariteK2Ca4Al2Be4Si24O60 · H2OHex. 6/mmm (6/m 2/m 2/m) : P6/mcc
OftedaliteKSc22Be3Si12O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
Osumilite(K,Na)(Fe2+,Mg)2(Al,Fe3+)3(Si,Al)12O30Hex.
Osumilite-(Mg)KMg2Al3(Al2Si10)O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
PoudretteiteKNa2B3Si12O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
RoedderiteKNaMg2(Mg3Si12)O30Hex. 6 m2 : P62c
ShibkoviteK2Ca2(Zn3Si12)O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
SogdianiteKZr2Li3Si12O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
SugiliteKNa2Fe3+2(Li3Si12)O30Hex.
TrattneriteFe3+2(Mg3Si12)O30Hex. 6/mmm (6/m 2/m 2/m) : P6/mcc
UM1990-73-SiO:KMnNaZn(K,Na)2Zn3Mn1.5Si12O30Hex.
YagiiteNaMg2(AlMg2Si12)O30Hex. 6/mmm (6/m 2/m 2/m)

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.

References for Unnamed (Mn3+-dominant analog of Sugilite)Hide

Reference List:
Sort by Year (asc) | by Year (desc) | by Author (A-Z) | by Author (Z-A)
Hirowatari, F. and Fukuoka, M. (1989) Some problems of the studies on the manganese minerals in Japan. Journal of the Mineralogical Society of Japan, 18, 347–365, https://doi.org/10.2465/gkk1952.18.347 (in Japanese)

Internet Links for Unnamed (Mn3+-dominant analog of Sugilite)Hide

Localities for Unnamed (Mn3+-dominant analog of Sugilite)Hide

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

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for 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 (eg from pseudomorphs.)

All localities listed without proper references should be considered as questionable.
Japan
 
  • Ehime Prefecture
    • Iyo district
      • Tobe-cho
Hirowatari, F. and Fukuoka, M. (1989) Some problems of the studies on the manganese minerals in Japan. Journal of the Mineralogical Society of Japan, 18, 347–365, https://doi.org/10.2465/gkk1952.18.347 (in Japanese)
 
矿物 and/or 产地  
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